Proceeding ประชุมวิชาการธรณี 2562

30
Figure 1. Potential risk areas of arsenic in water.

31 การประชุมวิชาการ “ธรณไี ทย 2562”, 16-17 กันยายน 2562 ณ โรงแรม เดอะ เบอรเ คลยี  ประตนู าํ้ กรุงเทพมหานคร

Tectonics and Paleogeography of Western Thailand

Prinya Putthapiban*, Dmitry Remizov**, Lin Chao*** Piyatida Saengthong,* Narongsak
Kaewdum* and Sirot Salyapongse*

*Geosience, Mahidol University Kanchanaburi, 199 Lum Sum, Sai Yok, Kanchanaburi 71150, Thailand.
** Dmitry N. Remizov, All-Russian Geological Institute (VSEGEI), St. Petersburg, RUSSIA.

*** Lin Chao, Structure and Metamorphic Petrology, School of Earth and Space Sciences, Peking University, China.

Abstract

Semi detailed field studies and research works via the Geoscience Students’ Senior
Research Projects and the students’ annual field investigation, which have been carried out
in the recent years, particularly in the areas of Kanchanaburi and Suphanburi, western
Thailand. In this paper, we present our new findings and propose the preliminary model on
the tectonics and paleogeography of this area. Marine Triassic rock units are wide-spread in
western Thailand. Their major rock types are thin bedded ribbon chert, mudstone & shale,
greywacke limestone and upper layered dolomite. Many fossils which clearly indicate their
depositional ages including radiolarian fossils in the chert beds, daonella and halobia fossils
in shale/mudstone and fine grained greywacke stratas. However, in several locations,
reworked fossils have been clearly observed. The evidences include : a) the fossils bearing
transported rock fragments were found as pebbles in many coarse grained clastic rocks, b)
severe corrosive edges of the older fossil fragments and frequently show preferred
orientation with placer depositional features, c) mixing of the older fossils and the younger
ones, etc. Furthermore, the relatively wide spread of Olistostrome deposits were clearly
observed at Ban Kaeng Riang Bon near Wat Tham Phra Tat, Sri Sawat district. The rocks are
very poorly sorted composing of highly angular and mainly carbonate rock fragments of
cobble sizes or larger. Some of these enclosed rock fragments are definitely Permian. The
most likely younger ones, Triassic dolomite (?) and matrix materials are still under
investigated and examined. This olistostrome unit was underlain by the fossiliferous
radiolarian ribbon chert and shale layers of Middle Triassic.

It is crystal clear that during the Triassic to at least the early stage of Jurassic, this
whole terrain must had been at least one kilometer or so below sea level. Our recent
findings on this paleo-continental shelf break and submarine fan features along the Kwae Yai
river bank Sri Sawat district, near Erawan National Park and other adjacent areas suggested
that the Triassic paleo-shoreline or landward side was facing the Eastward and
Southeastward, towards the eastern part and the southern peninsular including present day
Gulf of Thailand or beyond. The occurrence of olistostrome at Ban Kaeng Riang Bon and the
present of Marine Jurassic rock sequences at Thong Pha Phum district, Kanchanaburi and at

32

Mae Sot district, Tak provinces and their vicinity may indicate that the paleo-marine basin
had retreated westward toward the Myanmar-Thai border.

The occurences of a number of low angle eastward dipping sheared features in
various places and olistostrome are evidently favorable for accretionary wedge tectonic of
the region. The available geochronological data indicated that the area would have been
still very tectonically active throughout Cenozoic and the very early part of Quaternary.
Systematic works are being carried out for a better understanding of the geologic history and
geological reconstruction of the whole terrain.

Key words : Triassic radiolarian chert, greywacke, shelf break, submarine fan
environment, olistostrome, geological reconstruction

33 การประชุมวิชาการ “ธรณีไทย 2562”, 16-17 กันยายน 2562 ณ โรงแรม เดอะ เบอรเคลยี  ประตนู า้ํ กรงุ เทพมหานคร

The boundary between Palaeotethys (Inthanon Zone/Terrane) and
Gondwana (Sibumasu/Shan-Thai Terrane) northwest Thailand.

Udchachon, M1., Thassanapak, H2.., Burrett, C1.

1 Palaeontological Research and Education Centre, Mahasarakham University, Mahasarakham 44150, Thailand
2 Applied Palaeontology and Biostratigraphy Research Unit, Department of Biology, Faculty of Science, Mahasarakham

University, Mahasarakham 44150, Thailand

Abstract

New and previously published evidence from the area west of the Mae Yuam Fault in
NW Thailand (the Northern part of the West Thailand region or NWTR of the Sibumasu
Terrane) suggest that the Mae Yuam Fault constitutes the western boundary of both
Palaeotethyan, Permian faunas and the Inthanon Zone (as originally defined by Barr and
Macdonald) and is not placed further west as several recent authors have suggested (e.g.
Racki et al., in press). We suggest that the well-studied Siamodus-bearing, Upper Devonian
sections and fauna of the NWTR (e.g. Long, 1989; Long & Burrett, 1989; Koenigshof et al.,
2102; Dopieralska et al., 2012; Savage et al., 2007) do not suggest oceanic conditions as
suggested by Racki et al., (in press), but rather deep shelf.

Thin stratigraphic sections (c.50 m) of ‘lower’ to ‘middle’ Permian limestones in the
NWTR were deposited on a shallow marine shelf, were non-tropical and contain the
temperate-climate fusuline Monodiexodina (Ueno, 2003; Ingavat & Douglass, 1981).
Guadalupian (‘middle’ Permian) limestone with abundant calcareous algae, contains
abundant and diverse smaller foraminiferans, ostracodes and the conodonts Mesogondolella
siciliensis and M. dicerocarinata. These Permian limestones contrast strongly with coeval,
thick, (c.1000 m), Visean to Lopingian palaeo-tropical limestones and their diverse
coral/fusuline/algal faunas in the Inthanon Zone immediately to the west of the Mae Yuam
Fault in the Sop Pong area, within the Inthanon Zone/Terrane (e.g. Fontaine et al., 2009).

The petrography and geochemistry of Lower to Upper Triassic radiolarian cherts from
the NWTR and the Mae Yuam Fault zone suggest a hemipelagic continental margin
environment (e.g. Kamata et al., 2009; Saesaengseerung et al., 2006). Phosphatic nodules in
Carboniferous radiolarian cherts (Feng et al., 2005) and high phosphate content in some
Triassic cherts suggest an upwelling continental margin along the western margin of the
Inthanon Zone. The non-volcanic Palaeozoic to Late Triassic of the NWTR contrasts with the
mildly volcanic influenced Carboniferous to Middle Triassic of the northwestern part of the
Inthanon Zone to the east of the Mae Yuam Fault.

The popular model of allochthonous, tropical, Late Palaeozoic, seamount carbonates
in the northwest of the Inthanon Zone/Terrane (e.g. Ueno et al., 2008; Metcalfe, 2013; Barber

34

et al., 2011) is considered unlikely as outcrops of volcanics are rare and areally restricted and
the probably, conformably underlying, plant, bivalve and ammonoid-bearing, Carboniferous
marine sandstones (Ingavat-Helmcke, 1993) are of continental margin origin (Hara et al.,
2010). An alternative hypothesis is that the Inthanon Zone/Terrane rifted from Gondwana in
the Devonian and moved into tropical waters by the Carboniferous whereas Sibumasu was
glacially influenced in the Pennsylvanian and earliest Permian, rifted off Gondwana in the
Early Permian and was in temperate seas by the Middle Permian (Roadian). Docking of
Inthanon and the NWTR occurred in the Triassic with the deposition of the mainly siliciclastic
Mae Sariang Group in a probable foreland basin west of the Mae Yuam Fault (Srinak et al.,
2007; Tofke et al., 1993). These Triassic siliciclastics contain Cr-spinels interpreted as
representing the uplifted and eroded oceanic lithosphere that intervened between Inthanon
and Sibumasu (Hisada et al., 2005).

Keywords: terranes, Permian, Triassic, radiolarians, conodonts, foraminiferans, chert
geochemistry

35 การประชุมวชิ าการ “ธรณไี ทย 2562”, 16-17 กนั ยายน 2562 ณ โรงแรม เดอะ เบอรเคลีย ประตูนํ้า กรุงเทพมหานคร

THE CAVE OF YAI RUAK FROM KRABI CONFIRMS THE EXISTENCE
OF A SAVANNA CORRIDOR IN PENINSULAR THAILAND
DURING PLEISTOCENE GLACIALS

Kantapon Suraprasita,b,*, Sutee Jongautchariyakulc, Chotima Yameec, Cherdchan Pothichaiyac,
and Hervé Bocherensb,d

a Morphology of Earth Surface and Advanced Geohazards Research Unit (MESA RU), Department of Geology, Faculty of
Science, Chulalongkorn University, Bangkok, 10330, Thailand

b Department of Geosciences, Biogeology, University of Tübingen, Hölderlinstraße 12, 72074, Tübingen, Germany
c Department of Mineral Resources, Rama VI Road, Bangkok, 10400, Thailand

d Senckenberg Research Centre for Human Evolution and Paleoenvironment (S-HEP), University of Tübingen, Sigwartstraße
10, 72076, Tübingen, Germany

*presenting author, [email protected]; [email protected]

Abstract

The story of early human migration between mainland and island Southeast Asia is
one of the most debated topics in paleontological and archaeological communities today.
The hypothesis of a “savanna corridor” or a band of open vegetation (seasonal forests and
grasslands), stretching from mainland Southeast Asia to Java at several periods of lowering
sea level and exposed land bridges though the Pleistocene, has therefore been proposed for
explaining the facilitated route of early humans and associated large mammals in migrating
into islands of Southeast Asia. However, the existence of savanna grasslands in Peninsular
Thailand during the Pleistocene has never been demonstrated due to the scarcity of
available proxies. In 2017, the cave of Yai Ruak, Krabi Province was first excavated by Thai
paleontological teams from the Department of Mineral Resources and Chulalongkorn
University, together with locals. Some nearly complete mandibles, isolated teeth, and bones,
identified as belonging to four mammal taxa: Hystrix cf. brachyura, Crocuta crocuta ultima,
Rhinoceros sondaicus, and Rusa unicolor, were found from the infilling sediments within this
cave. A biochronological age is preliminarily attributed to a late Middle to Late Pleistocene
age for the fauna based on the presence of Crocuta crocuta ultima. We reconstructed the
Pleistocene vegetation and environments of the region, using a stable carbon isotope
analysis of mammalian tooth enamel recovered from this cave. The stable carbon isotope
results reveal that an open vegetation/forest-grassland mosaic was dominant in this region
during that time, unlike today, thus confirming the existence of the savanna corridor in
Peninsular Thailand. However, the connection of similar open vegetation types between
Peninsula Thailand and other Indonesian islands is still not demonstrated. Further
investigations into the Pleistocene mammal faunas in Thai-Malay Peninsula are thus helpful
to better identify such a corridor in relation to the early human migration route and to the
paleobiogeography of Southeast Asian large mammal species in the future.

Keywords: hyenid assemblage, stable carbon isotope, bioapatite, Sundaland,
Quaternary

36

The possible detection of more subsurface petrified wood deposits
via the 2D electrical resistivity survey and evaluation of the 2D

imaging technique at the petrified wood deposits at Ban Tak district,
Tak province, northern Thailand.

Patchawee Nualkhao*, Pattarakan Prapan*, Chatchai Vachiratienchai**, Supawit
Yawsangratt3***

* Geoscience Program, Mahidol University, Kanchanaburi Campus
** Curl-E Geophysics Co., Ltd**.

***Geotechnology, Dapartment of Mineral Resources

Abstract

An electrical resistivity survey, a non-destructive geophysical investigation method,
was chosen and carried out in Doi Soi Malai National Park area, Ban Tak District, Tak Province.
This park is considered both a natural ecosystem and part of a natural heritage as the
country’s largest petrified wood tree trunk was discovered there. The aim of this study is to
investigate and locate the shape, size and distribution of the subsurface gravel bed(s), the
layer in which the buried treasure of fossilized tree trunks are frequently found. The eight
geo-electrical sections of the Wenner-Schlumberger configuration derived from the electrical
resistivity survey have provided a broad view of the subsurface features. Inversion results of
the two-dimensional electrical images obtained from these surveys clearly display two
distinct layers. The lower and deeper layer at > 3 m depth is apparently more closely
related to the surrounding geological materials like sand and clay with lower resistivity values
of < 170 ohm-meters. In contrast, the upper layer at an average depth of 1-3 m, the gravel
bed in the basin in which higher resistivity values of > 170 ohm-meters were detected. This
later layer has a much higher potential of containing big petrified wood tree trunks.

Keywords: Electrical resistivity survey, Wenner-Schlumberger, configuration, petrified
woods, gravel bed

37 การประชมุ วชิ าการ “ธรณไี ทย 2562”, 16-17 กันยายน 2562 ณ โรงแรม เดอะ เบอรเ คลีย ประตูน้ํา กรงุ เทพมหานคร

Öú÷ìč íŤÖćøóĆçîćÖćøìŠĂÜđìę÷Ċ üđßĉÜíøèĊ×ĂÜĂčì÷ćîíøèĊ×ĂîĒÖîŠ ÿŠĂĎ ìč ÷ćîíøèĊēúÖ

ýčõöĉêø ÝîĆ ìąÙćö1 , ĒéîüĉßĆ÷ ÿć÷øÖĆ þć2 ĒúąøÜĆ ÿøøÙŤ ÿÜĉ Āđúĉý3

1 ÿĞćîĆÖÜćîìøĆó÷ćÖøíøèĊ đ×ê 2 ÖøöìøóĆ ÷ćÖøíøèĊ ê.ĔîđöČĂÜ Ă.đöČĂÜ Ý.×ĂîĒÖŠî 40000
2,3 ñšßĎ Šü÷ýćÿêøćÝćø÷Ť éø., ÿć×ć÷ìč íýćÿêøÖŤ ćøóĆçîćõĎöĉõćÙ öĀćüìĉ ÷ćú÷Ć øćßõĆäöĀćÿćøÙćö

Corresponding author, E-Mail : [email protected]

ïìÙĆé÷ĂŠ

Ăčì÷ćîíøèĊ×ĂîĒÖŠî đðŨîĂčì÷ćîíøèĊøąéĆïÝĆÜĀüĆéđöČęĂðŘ ó.ý. 2561 öĊóĚČîìęĊÙøĂïÙúčöĒĀúŠÜ
íøèĊüĉì÷ć 3 ïøĉđüè ĕéšĒÖŠ ïøĉđüèõĎöĉðøąđìýĒïïĀĉîðĎîĀøČĂÙćÿêŤ ïøĉđüèĒĀúŠÜàćÖéċÖéĞćïøøóŤĕéēîđÿćøŤ
đìČĂÖđ×ćõĎđüĊ÷Ü ĒúąïøĉđüèĀîĉ ÿü÷ÜćöĒðúÖêć àÜęċ öýĊ ĆÖ÷õćóĔîóçĆ îćđðîŨ ĒĀúŠÜìŠĂÜđì÷ęĊ üđßÜĉ íøèĊĒúąïøĉĀćø
ÝĆéÖćøĔĀšđðŨîĂčì÷ćîíøèĊøąéĆïēúÖĕéš ĒêŠÿõćóðŦÝÝčïĆî÷ĆÜ×ćéĒñîÖú÷čìíŤÖćøóĆçîćÖćøìŠĂÜđìęĊ÷üđßĉÜíøèĊìęĊ
đðîŨ øĎðíøøöàęċÜĂćÝÿŠÜñúêĂŠ ÖćøóçĆ îćĂčì÷ćîíøèĊìĊęĕöŠÿĂéÙúšĂÜÖĆïĒîüìćÜ×ĂÜĂčì÷ćîíøèĊðøąđìýĕì÷Ēúą
Ăčì÷ćîíøèĊøąéĆïēúÖ×ĂÜĂÜÙŤÖćø÷ĎđîÿēÖ ñĎšüĉÝĆ÷ĕéšýċÖþćÖú÷čìíŤÖćøóĆçîćÖćøìŠĂÜđìĊę÷üđßĉÜíøèĊ×ĂÜĂčì÷ćî
íøèĊ×ĂîĒÖŠîÿĎŠÖćøđðŨîĂčì÷ćîíøèĊøąéĆïēúÖ ēé÷ĔßšÖćøüĉÝĆ÷ĒïïñÿöñÿćîüĉíĊ (Mixed Method Research)
ĒïŠÜÖćøüĉÝĆ÷đðŨî 3 øą÷ą ÙČĂ øą÷ąìęĊ 1 ÖćøýċÖþćýĆÖ÷õćóìćÜÖćøìŠĂÜđìĊę÷üđßĉÜíøèĊ×ĂÜĂčì÷ćîíøèĊ
×ĂîĒÖŠî ĔßšĒïïÿĂïëćöÖĆïÖúŠčöêĆüĂ÷ŠćÜìĊęđðŨîîĆÖìŠĂÜđìęĊ÷ü ðøąßćßî ÙèąìĞćÜćîĂčì÷ćîíøèĊ×ĂîĒÖŠî
đÝšćĀîšćìĊęĂÜÙŤÖćøðÖÙøĂÜÿŠüîìšĂÜëęĉî ñšĎðøąÖĂïÖćø ĒúąîĆÖüĉßćÖćø ÝĞćîüî 320 Ùî øą÷ąìęĊ 2 đðŨîÖćø
üĉđÙøćąĀŤÿõćóĒüéúšĂöõć÷ĔîĒúąõć÷îĂÖ (SWOT Analysis) Ēúą TOWS Metrix ēé÷ĔßšÖćøðøąßčöøąéö
ÙüćöÙĉéđĀĘîÝćÖÙèąìĞćÜćîĂčì÷ćîíøèĊ×ĂîĒÖŠî ÝĞćîüî 45 Ùî Ēúąøą÷ąìęĊ 3 đðŨîÖćøÿøšćÜÖú÷čìíŤēé÷Ĕßš
ÖćøÿîìîćÖúöčŠ ÝćÖÙèąìćĞ ÜćîĂìč ÷ćîíøèĊ×ĂîĒÖîŠ ÝĞćîüî 15 Ùî ñúÖćøüÝĉ ÷Ć óïüćŠ

1. ĔîõćóøüöĂčì÷ćîíøèĊ×ĂîĒÖŠîöĊýĆÖ÷õćóìćÜÖćøìŠĂÜđìęĊ÷üđßĉÜíøèĊĔîøąéĆïöćÖ ēé÷ĔîéšćîÿęĉÜ
éċÜéĎéìĊęîŠćÿîĔÝöĊýĆÖ÷õćóĔîøąéĆïöćÖìĊęÿčé øĂÜúÜöć ÙČĂ éšćîÖĉÝÖøøöÖćøìŠĂÜđìęĊ÷üđßĉÜíøèĊ éšćîÖćøÿøšćÜ
öĎúÙŠćđóĉęöìćÜÖćøìŠĂÜđìęĊ÷ü ĒúąéšćîÿęĉÜĂĞćîü÷ÙüćöÿąéüÖ öĊýĆÖ÷õćóĔîøąéĆïöćÖ ĒúąéšćîÖćøÿČęĂ
ÙüćöĀöć÷đßĉÜíøèĊ éšćîÖćøđךćëċÜĒĀúŠÜìĂŠ ÜđìĊę÷üöýĊ ĆÖ÷õćóĔîøąéïĆ öćÖ êćöúĞćéĆï

2. ñúÖćøüĉđÙøćąĀŤÿõćóĒüéúšĂöõć÷ĔîĒúąõć÷îĂÖ×ĂÜÖćøìŠĂÜđìęĊ÷üđßĉÜíøèĊ×ĂÜĂčì÷ćîíøèĊ
×ĂîĒÖŠî óïüŠć Ăčì÷ćîíøèĊ×ĂîĒÖŠîöĊÙŠćÙąĒîîëŠüÜîĚĞćĀîĆÖÿĎÜÿčéìęĊðøąđéĘîÝčéĒ×ĘÜ (Strength) ÝčéĂŠĂî
(Weakness) ēĂÖćÿ (Opportunities) ĒúąĂčðÿøøÙ (Threat) đìŠćÖĆï 4.79, 4.28, 3.43 Ēúą 2.98
êćöúĞćéĆï ēé÷ÝčéĒ×ĘÜ ÙČĂ ÖćøđðŨîđöČĂÜìŠĂÜđìĊę÷üĕéēîđÿćøŤĒĀŠÜĒøÖ×ĂÜðøąđìýĕì÷ìĊęöĊßęČĂđÿĊ÷ÜøąéĆïÿćÖú öĊ
ÖćøïøĉĀćøÝĆéÖćøēé÷ĀîŠü÷ÜćîìšĂÜëĉęîìęĊöĊðøąÿĉìíĉõćó öĊÖĉÝÖøøöìŠĂÜđìĊę÷üÿĞćÙĆâĀöčîđüĊ÷îêúĂéðŘ đðŨî
đöČĂÜĒĀŠÜĀöĂúĞćĀöĂĒÙîìĊęēééđéŠî ĒúąđðŨîđöČĂÜýĎî÷ŤÖúćÜïøĉĀćøøćßÖćøõĎöĉõćÙ öĊÝčéĂŠĂî ÙČĂ ĒĀúŠÜ
ìŠĂÜđìęĊ÷üöĊÿõćóđÿęČĂöēìøöĒúąđÿęĊ÷ÜêŠĂÖćøëĎÖìĞćúć÷ ×ćéÖú÷čìíŤÖćøóĆçîćÖćøìŠĂÜđìĊę÷üđßĉÜíøèĊìĊę
đĀöćąÿö ßčößî÷ĆÜ×ćéÙüćöøĎšđךćĔÝđÖęĊ÷üÖĆïĂčì÷ćîíøèĊ ðŦâĀć×÷ąĒúąÿĉęÜĒüéúšĂö ĒúąðøąÿïðŦâĀćõĆ÷
ĒúšÜĂ÷ĎŠđÿöĂ éšćîēĂÖćÿ ÙČĂ ÿČęĂēàđßĊ÷úöĊđéĊ÷öĊĂĉìíĉóúêŠĂÖćøðøąßćÿĆöóĆîíŤÖćøìŠĂÜđìęĊ÷ü øĆåïćúÿîĆïÿîčî
îē÷ïć÷Ăčì÷ćîíøèĊ îē÷ïć÷ÖúčŠöÝĆÜĀüĆéøšĂ÷ĒÖŠîÿćøÿĉîíčŤđîšîÖćøìŠĂÜđìęĊ÷üđßĉÜíøèĊ øĆåïćúÿŠÜđÿøĉöîē÷ïć÷
óĆçîćđÿšîìćÜÙöîćÙöĒúąÖćø×îÿŠÜ ĒúąĒîüēîšöÖøąĒÿÖćøìŠĂÜđìĊę÷üĂ÷ŠćÜ÷ęĆÜ÷ČîđóĉęöÿĎÜ×Ěċî ĒúąðŦâĀć
ĂčðÿøøÙ ÙČĂ ðŦâĀćÙŠćîĉ÷öĒúąóùêĉÖøøöÖćøìĞćÜćîĒïïĒ÷ÖÿŠüî đìÙēîēú÷ĊđðúĊę÷îĒðúÜđøĘüđÖĉîĕð ÿõćó

38

đýøþåÖĉÝðøąđìýĂ÷ĎĔŠ îõćüąßąúĂêüĆ ðŦâĀćÖćøĀćêúćéÿîĉ ÙšćìšĂÜëęîĉ ĒúąÿõćüąÖćøđðúĊę÷îĒðúÜõöĎ Ăĉ ćÖćý
ìøĊę čîĒøÜöćÖ×ċĚî

3. Öú÷čìíŤÖćøóĆçîćÖćøìŠĂÜđìĊę÷üđßĉÜíøèĊ×ĂÜĂčì÷ćîíøèĊ×ĂîĒÖŠîÿĎŠÖćøđðŨîĂčì÷ćîíøèĊøąéĆïēúÖ
ðøąÖĂïéüš ÷ üĉÿĆ÷ìĆýîŤ ÙČĂ “Ăčì÷ćîíøèĊ×ĂîĒÖîŠ đðîŨ Ăčì÷ćîÖćøìŠĂÜđìĊę÷üĒúąđøĊ÷îøšĎĕéēîđÿćøŤøąéĆïēúÖ” 5
ðøąđéĘî÷čìíýćÿêøŤ 11 đðŜćðøąÿÜÙŤ 22 Öú÷čìíŤĀøČĂĒîüìćÜÖćøóĆçîć Ēúą 34 êĆüßĊĚüĆé ēé÷ðøąđéĘî
÷čìíýćÿêøŤ 5 ðøąÖćø ĕéšĒÖŠ (1) ĂîčøĆÖþŤĒúąðÖðŜĂÜĒĀúŠÜöøéÖìćÜíøèĊĂ÷ŠćÜöĊÿŠüîøŠüö (2) ïøĉĀćøÝĆéÖćø
Ăčì÷ćîíøèĊĒïïĂÜÙŤøüöÿŠĎđÙøČĂ׊ć÷øąéĆïēúÖ (3) ÷ÖÖøąéĆïÿŠĎđöČĂÜìŠĂÜđìęĊ÷üĕéēîđÿćøŤĒúąõĎöĉðŦââćøąéĆï
ēúÖ (4) ÿŠÜđÿøĉöÖćøýċÖþćĒúąÿČęĂÙüćöĀöć÷đóęČĂÖćøìŠĂÜđìęĊ÷üđßĉÜíøèĊéšü÷îüĆêÖøøö Ēúą (5) óĆçîć
đýøþåÖÝĉ ìĂš Üëęîĉ Ă÷ćŠ Ü÷ęĆÜ÷îČ

ÙćĞ ÿĞćÙâĆ : Öú÷ìč í,Ť ÖćøìĂŠ Üđì÷ęĊ üđßÜĉ íøè,Ċ ×ĂîĒÖŠî, Ăčì÷ćîíøèĊøąéïĆ ēúÖ

Keywords: Strategy, Geotourism, Khon Kaen, Global Geopark

39 การประชุมวิชาการ “ธรณีไทย 2562”, 16-17 กันยายน 2562 ณ โรงแรม เดอะ เบอรเ คลีย ประตูน้ํา กรงุ เทพมหานคร

ÖúöŠč ôüŗ àúĎ îĉ éĉ Ăć÷čߊüÜðúć÷×ĂÜđóĂøđŤ öĊ÷îêĂîÖúćÜ
ĔîĀöüéĀĉîđ×ć×üćÜĒúąđ×ć×ćé ÝĆÜĀüéĆ ÿøąïøč Ċ

ÿčíćøêĆ îŤ ÿĊøĂé1,2* Ēúą åćÿèĉ ÷Ċ Ť đÝøâĉ åĉêĉøêĆ î1Ť

1 õćÙüßĉ ćíøèüĊ ĉì÷ć Ùèąüìĉ ÷ćýćÿêøŤ Ýāč ćúÜÖøèŤöĀćüĉì÷ćúĆ÷ ÖøÜč đìóĄ 10330
2 ÖøöìøĆó÷ćÖøíøèĊ 75/10 ëîîóøąøćöìĊę 6 Ē×üÜìŠčÜóâćĕì đ×êøćßđìüĊ ÖøčÜđìóĄ 10400

*corresponding author: [email protected]

ïìÙéĆ ÷ĂŠ

ÖúŠöč Āîĉ ÿøąïčøĊđðŨîĀîüŠ ÷ĀĉîìÿęĊ ĞćÙĆâĔîߊüÜĂć÷čóćúĊēĂēàĂĉÖêĂîïî×ĂÜðøąđìýĕì÷ ÖøąÝć÷êĆüÖüšćÜ
ïøĉđüèÝĆÜĀüĆéÿøąïčøĊĒúąÝĆÜĀüĆéĔÖúšđÙĊ÷Ü ÖúčŠöĀĉîîĊĚðøąÖĂïéšü÷ 6 ĀöüéĀĉî đøĊ÷ÜúĞćéĆïÝćÖĂć÷čĒÖŠĕðĂŠĂî
ÙČĂ ĀöüéĀĉîõĎđó ĀöüéĀĉîđ×ć×üćÜ ĀöüéĀĉîĀîĂÜēðśÜ ĀöüéĀĉîðćÜĂēýÖ ĀöüéĀĉîđ×ć×ćé ĒúąĀöüéĀĉî
àĆïïĂî (Hinthong, 1981) ēé÷öĊÙüćöĀîćìĆĚÜĀöéðøąöćè 5,000 đöêø ĀöüéĀĉîĔîÖúŠčöĀĉîÿøąïčøĊìęĊÿîĔÝ
ýċÖþćüĉÝĆ÷öĊ 2 ĀöüéĀĉîÙČĂ ĀöüéĀĉîđ×ć×üćÜĒúąĀöüéĀĉîđ×ć×ćé ÝćÖøć÷Üćî×ĂÜ Hinthong (1981)
óïüŠćĀöüéĀĉîđ×ć×üćÜĂć÷čĒÖŠÖüŠćĀöüéĀĉîđ×ć×ćé ĀöüéĀĉîìĚĆÜÿĂÜîĊĚöĊĂÜÙŤðøąÖĂïÿŠüîĔĀâŠđðŨîĀĉî
ÙćøŤïĂđîê ÿõćóĒüéúšĂöÖćøÿąÿöêĆüĂ÷ĎŠĔîìąđúîĞĚćêČĚî ĒúąÝćÖøć÷ÜćîĀúć÷ÞïĆï÷Čî÷ĆîüŠćóïàćÖéċÖéĞć
ïøøóŤéĆßîĊôŗüàĎúĉîĉé÷čÙđóĂøŤđöĊ÷îđðŨîÿŠüîĔĀ⊠ĒêŠ÷ĆÜĕöŠöĊøć÷úąđĂĊ÷éÖćøĔĀšĂć÷č×ĂÜàćÖéċÖéĞćïøøóŤéĆßîĊôŗüàĎ
úĉîĉé îĂÖÝćÖîĊĚ Morley et al. (2013) ÖúŠćüüŠćöĊĒîüøĂ÷đúęČĂî÷šĂîĀúć÷ĒîüĔîóČĚîìęĊìĊęöĊÖćøÖøąÝć÷êĆü×ĂÜ
ÖúčöŠ Āîĉ ÿøąïčøĊ (øĎðìĊę 1) ÝćÖøć÷ÜćîîĚĊìĞćĔĀšđÖĉéךĂÿÜÿĆ÷ĔîđøČęĂÜ×ĂÜÖćøúĞćéĆïßĆĚîĀĉîìćÜÖć÷õćó×ĂÜÖúčŠöĀĉî
ÿøąïčøüĊ ćŠ ĂćÝÝąöÙĊ üćöàĞćĚ àĂš î×ĂÜÖćøúĞćéĆïßĚĆîĀĉîĒúąÙüćöĀîćìęĊĂćÝĀîćđÖĉîÙüćöđðŨîÝøĉÜ ĂĆîđîČęĂÜöćÝćÖ
øĂ÷đúęČĂî÷šĂîĔîóČĚîìĊę éĆÜîĚĆîÖćøúĞćéĆïßĚĆîĀĉî×ĂÜÖúčŠöĀĉîÿøąïčøĊ ÝċÜÝĞćđðŨîêšĂÜöĊÖćøýċÖþćøć÷úąđĂĊ÷éđóČęĂĀć
ÙüćöÿĆöóĆîíŤÖćøúĞćéĆïßĚĆîĀĉî ēé÷đøęĉöÝćÖĀöüéĀĉîđ×ć×üćÜĒúąđ×ć×ćéìęĊóïàćÖéċÖéĞćïøøóŤéĆßîĊôŗüàĎúĉîĉé
éüš ÷üíĉ ÖĊ ćøúĞćéĆïßîĚĆ Āîĉ ìćÜßĊüõćóĒúąĔßĂš ć÷čĀĉîđðŨîđÖèæŤĔîÖćøđìĊ÷ïÿöĆ óîĆ íŤ

ÖćøÿĞćøüÝÿõćóíøèĊüĉì÷ć×ĂÜĀĉîðĎîĔîóĚČîìęĊýċÖþć óïüŠćĀĉîðĎîēñúŠđðŨîđìČĂÖđ×ćĒúąêćöóĚČîøćï
ïćÜĒĀŠÜĀĉîðĎîđðŨîöüúĀîć×îćéĔĀâŠĕöŠöĊÖćøđøĊ÷ÜßĆĚî ïćÜĒĀŠÜóïÖćøđøĊ÷ÜßĚĆîĀîć×ĂÜĀĉîðĎîÿúĆïÖĆïßĆĚî
Āîĉ éîĉ éćî ĒúąïćÜïøđĉ üèóïÖøąđðćąĀîĉ đßĉøêŤ ĒìøÖĔîđîĂČĚ ĀĉîðĎîéüš ÷ đîČĂĚ Āîĉ ðĎîöĊÿĊđìćĂŠĂîëċÜđìćđ×öš óï
àćÖéÖċ éĞćïøøóĀŤ úćÖĀúć÷ßîéĉ ĒêđŠ îĂĚČ ĀĉîðîĎ ïćÜĒĀÜŠ ĕöŠóïàćÖéÖċ éĞćïøøóŤ đîĂęČ ÜÝćÖôŗüàúĎ îĉ éĉ đðîŨ àćÖ
éċÖéĞćïøøóŤéßĆ îìĊ éęĊ ĊĒúąÿĆÜđÖêđĀĘîÜŠć÷ĔîĀîĉ ðîĎ éÜĆ îĆîĚ êĆüĂ÷ćŠ ÜĀîĉ ðĎîĒúąàćÖéÖċ éćĞ ïøøóŤéßĆ îĊôüŗ àúĎ îĉ ĉé ÝċÜëĎÖ
đÖïĘ ÝćÖĀúć÷óĚČîììĊę ęĊóïÖćøÖøąÝć÷êĆü×ĂÜĀöüéĀĉîđ×ć×üćÜĒúąđ×ć×ćé ïøĉđüèÝĆÜĀüĆéÿøąïčøĊ (øĎðìęĊ 2) Ēúą
ëĎÖîĞćöćìĞćĒñŠîĀĉîïćÜ đóČęĂýċÖþćôŗüàĎúĉîĉéĒúąýĉúćüøøèîć×ĂÜĀĉîðĎî ÝćÖÖćøýċÖþćךĂöĎúĒñŠîĀĉîïćÜĔî
ïćÜÿŠüîÝćÖêĆüĂ÷ŠćÜìĊęđÖĘïöćìĚĆÜĀöé óïüŠćđîĚČĂĀĉîðĎîÿŠüîĔĀâŠđðŨîĕïēĂÙúćÿêĉÖĒüÙÿēêîĒúąĒóÙÿēêî
(Bioclastic wackestone and packstone) ÿĞćĀøĆïñúÖćøýċÖþćôŗüàĎúĉîĉéóïךĂöĎúìĊęîŠćÿîĔÝÙČĂ ÖúŠčöôŗüàĎúĉ
îĉéìęĊĕéšÝćÖĀĉîðĎîìęĊđÖĘïÝćÖĀöüéĀĉîđ×ć×üćÜĒúąđ×ć×ćéöĊÙüćöÙúšć÷ÙúċÜÖĆî ĒúąÿćöćøëÝĞćĒîÖĕéš 5 ÿÖčú
2 ßîĉéÙČĂ Sumatrina, Colania douvillei, Lepidolina, Verbeekina verbeeki ĒúąChusenella àęċÜÖúŠčö
ôüŗ àúĎ ĉîĉéîĚĊđðŨîàćÖéċÖéĞćïøøóéŤ ĆßîĊìĊęïÜŠ ïĂÖÿöĆ÷öĉđéĊ÷î (Midian) ĀøČĂ ĒÙððêŗ ćđîę÷Ċ î (Capitanian) ×ĂÜߊüÜ
ðúć÷÷čÙđóĂøŤđöĊ÷îêĂîÖúćÜ (late Middle Permian) ךĂöĎúĂć÷čîĊĚĒÿéÜĔĀšđĀĘîüŠćÖćøÿąÿöêĆü×ĂÜĀĉîðĎî
ĀöüéĀĉîđ×ć×üćÜĒúąđ×ć×ćéöĊߊüÜđüúćìĊęÙćïđÖĊę÷üÖĆîĀøČĂöĊߊüÜĂć÷čđéĊ÷üÖĆîÙČĂĂ÷ŠćÜîšĂ÷ĔîߊüÜðúć÷÷čÙ
đóĂøŤđöĊ÷îêĂîÖúćÜ ĀøČĂĒÿéÜëċÜÖćøÿąÿöêĆüìęĊêŠćÜÿëćîìęĊÖĆîĒêŠđÖĉéĔîߊüÜđüúćđéĊ÷üÖĆî

40
(Contemporaneous facies) éĆÜîĆĚîÝćÖøć÷ÜćîìęĊđÙ÷ÖúŠćüëċÜÖćøđøĊ÷ÜßĆĚîÝćÖĒÖŠĕðĂŠĂî×ĂÜĀöüéĀĉîêŠćÜė
ĔîÖúčöŠ Āîĉ ÿøąïčøĊ ÝċÜÝĞćđðŨîêšĂÜöĊÖćøìïìüîĒúąýċÖþćĔîøć÷úąđĂ÷Ċ éđóĉęö×ċîĚ

đĂÖÿćøĂšćÜĂÜĉ

Hinthong, C. 1981. Geology and Mineral Resources of Changwat Phra Nakhon Si Ayutthaya (ND 47-8), Scale
1:250,000. Department of Mineral Resources, Geological Survey Report, No.4, 1-105 (in Thai with
English summary).

Morley, C. K., Ampaiwan, P., Thanudamrong, S., Kuenphan, N., Warren J., 2013. Development of the Khao
Khwang Fold and Thrust Belt: Implications for the geodynamic setting of Thailand and Cambodia
during the Indosinian Orogeny. Journal of Asian Earth Sciences, 62, 705-719.

øĎðìęĊ 1 ĒîüÙéēÙšÜĒúąøĂ÷đúČęĂî÷šĂî ïøđĉ üèÝĆÜĀüéĆ ÿøąïøč ĒĊ úąÝÜĆ ĀüéĆ ĔÖúšđÙĊ÷Ü (Morley et al., 2013)

41 การประชมุ วิชาการ “ธรณไี ทย 2562”, 16-17 กันยายน 2562 ณ โรงแรม เดอะ เบอรเคลยี  ประตนู าํ้ กรงุ เทพมหานคร
øĎðìĊę 2 ĒñîìĊęíøèĊüĉì÷ćĒÿéÜÖćøÖøąÝć÷êĆü×ĂÜĀöüéĀĉîêŠćÜėĔîÖúčŠöĀĉîÿøąïčøĊ ÝčéýċÖþćĀĉîðĎîĒúąôŗüàĎúĉ
îéĉ ĔîĀöüéĀîĉ đ×ć×üćÜĒúąđ×ć×ćé (éĆéĒðúÜÝćÖ Ueno and Charoentitirat, 2011)

42

ÖúŠöč ĀĉîēÙøćßÙüøĕéøš ïĆ ÖćøĒÖšĕ×ĀøĂČ ÷ĆÜ?

îć÷đúĉýÿîĉ øÖĆ þćÿÖčúüÜýŤ

ïìÙéĆ ÷ŠĂ

ĀúĆÜÝćÖìĊę Ward and Bunnag ĕéšêĆĚÜßęČĂ “ÖúčŠöĀĉîēÙøćß” (Khorat Group) đöČęĂðŘ ó.ý. 2507 ĕéšöĊ
îĆÖüĉßćÖćøìĆĚÜĔîĒúąêŠćÜðøąđìýĕéšĔĀšÙüćöÿîĔÝöćýċÖþćđóęĉöđêĉööćÖöć÷ ìĆĚÜđóČęĂýċÖþćÖćøúĞćéĆïßĚĆîĀĉî Āć
ĒĀúŠÜìøĆó÷ćÖøíøèĊ đߊî îĞĚćïćéćú đÖúČĂĀĉî ēóĒìà ĒúąðŗēêøđúĊ÷ö ÿëćîõćóðŦÝÝčïĆîÖúŠčöĀĉîēÙøćß
ÿćöćøëĒïŠÜđðîŨ 9 ĀöüéĀîĉ ÝćÖúćŠ Üĕðïî éĆÜîĚĊ ÙČĂ ĀöüéĀĉîĀšü÷Āĉîúćé ĀöüéĀĉîîćĚĞ óĂÜ ĀöüéĀĉîõĎÖøąéċÜ
ĀöüéĀĉîóøąüĀĉ ćø ĀöüéĀîĉ đÿć×Ćü ĀöüéĀĉîõóĎ ćî ĀöüéĀĉîēÙÖÖøüé ĀöüéĀîĉ öĀćÿćøÙćö Ēúą ĀöüéĀĉî
õĎìĂÖ ÿõćóðŦâĀćóïüŠćßĆĚîĀĉîĒïïÞïĆïöĊÖćøđðúĊę÷îĕðöćÖÿöÙüøìĊęÝąêšĂÜĀćßĆĚîĀĉîĂšćÜĂĉÜđóęĉö×Ěċî đóęČĂĔĀš
đðîŨ ĒĀúŠÜýċÖþć×ĂÜĒêŠúąĀöüéĀĉî îĂÖÝćÖîĊ÷Ě ÜĆ öĊÖćøóĎéëċÜøĂ÷ßîĚĆ ĕöêŠ ĂŠ đîęĂČ ÜĔîÖúöčŠ ĀĉîēÙøćß ēé÷ýċÖþćÝćÖ
úąĂĂÜđøèēĎ ïøćè ĒúąÖćøüĆéĂć÷Ýč ćÖĒøŠđàĂøŤÙĂî ĀćÖóïøĂ÷ßĚĆîĕöŠêŠĂđîČęĂÜÝøĉÜÝąìĞćĔĀš×ĆéêŠĂöćêøåćîÖćø
êĚÜĆ ßČĂę ĀĉîêćöøąïïÿćÖú ÝċÜđĀîĘ ÿöÙüøìęĊÝąêĂš ÜöĊÖćøĒÖšĕ×ÖúčŠöĀĉîēÙøćß đóČęĂĔĀšÿĂéÙúšĂÜÖĆïÖêĉÖćîćîćßćêĉ
àċęÜÝąÿŠÜñúĔĀšÖćøñúĆÖéĆîĂčì÷ćîíøèĊ×ĂÜõćÙĂĊÿćøìĆĚÜ 3 ĒĀúŠÜìęĊÝĞćđðŨîêšĂÜĔßšÖćøúĞćéĆïßĚĆîĀĉî×ĂÜÖúčŠöĀĉî
ēÙøćßđóĂČę ĒÿéÜÿõćóíøèĊüĉì÷ć×ĂÜóČĚîìĕęĊ ðÿĎŠøąéĆï Unesco đðŨîĕðĂ÷ŠćÜöĊöćêøåćîÿćÖú

Key word: ÖúčŠöĀîĉ ēÙøćß ÖćøĒÖšĕ× öćêøåćîÿćÖú

43 การประชมุ วิชาการ “ธรณีไทย 2562”, 16-17 กนั ยายน 2562 ณ โรงแรม เดอะ เบอรเคลยี  ประตนู า้ํ กรงุ เทพมหานคร

ÖćøÖĞćĀîéĂć÷óč øąíćêčÝćÖĂåĉ ïøĉđüèüéĆ ðćś ĀöćÖĀîŠĂ êĞćïúÝĆîÝüšć ĂćĞ đõĂĒöÝŠ Ćî
ÝĆÜĀüéĆ đßĊ÷Üøć÷ éšü÷üíĉ Ċ Optically Stimulated Luminescence Dating

đÞúĉöóÜþŤ ēóú1ĚĊ *, ĒúąüĊøąßćêĉ üđĉ üÖüîĉ 2

1 ÿëćïîĆ đìÙēîēú÷ĊîĉüđÙú÷Ċ øĒŤ ĀÜŠ ßćêĉ (ĂÜÙŤÖćøöĀćßî)
2 ÖĂÜíøèüĊ ĉì÷ćÿęĉÜĒüéúšĂö ÖøöìøĆó÷ćÖøíøèĊ 75/10 ë.óøąøćö 6 øćßđìüĊ ÖøÜč đìóöĀćîÙø 10400

*Corresponding author: đÞúĉöóÜþŤ ēóúĊĚ
Email: [email protected]

ïìÙéĆ ÷ŠĂ

ÖćøÖĞćĀîéĂć÷čüĆêëčìćÜēïøćèÙéĊ ĒúąêąÖĂîéĉîéšü÷üĉíĊ Optically Stimulated Luminescence
(OSL) Dating ÿćöćøëîĞćĕðĔßšĔîÖćøĒðúÙüćöĀöć÷đøČęĂÜøćü×ĂÜðøąüĆêĉýćêøŤêŠćÜėìęĊđÖĉé×ĚĆîĔîĂéĊêĕéš Ēúą
îćĞ Ăć÷čêąÖĂîéîĉ ĕðĂíĉïć÷ߊüÜđüúćđĀêčÖćøèŤêŠćÜėìĊÿę öĆ óĆîóîĆ íŤÖïĆ ÖćøÿąÿöêĆü×ĂÜêąÖĂî đߊî ÖćøđúęČĂîêĆü
øĂ÷đúęČĂîöĊóúĆÜàċęÜìĞćĔĀšđÖĉéĒñŠîéĉîĕĀü đðŨîêšî đìÙîĉÙÖćøÖĞćĀîéĂć÷čîĚĊđðŨîüĉíĊìĊęđĀöćąÿĞćĀøĆïêĆüĂ÷ŠćÜìĊęöĊĒøŠ
ÙüĂêàŤđðŨîĂÜÙŤðøąÖĂïÝĞćîüîöćÖ ĒúąñŠćîÖøąïüîÖćøđñćĀøČĂÿĆöñĆÿÖĆïĒÿÜĒééđðŨîđüúćîćî ÙüćöøšĂî
ÝćÖÖćøđñćĀøČĂĒÿÜĒééöĊðøĉöćèöćÖđóĊ÷ÜóĂìĊęÝąúïÿĆââćîÖćøđøČĂÜĒÿÜìęĊÿąÿöĂ÷ŠĎÖŠĂîĀîšćîĊĚĔĀšĀöéĕð
êĆüĂ÷ŠćÜìĊęđĀöćąÿĞćĀøĆïÖćøÖĞćĀîéĂć÷čéšü÷üĉíĊîĊĚ ÙČĂ Ăĉå ÖøąđïČĚĂÜđñć đêćđñćēïøćè êąÖĂîìøć÷ìęĊÿąÿöêĆü
Ĕîìąđúìøć÷ đîĉîìøć÷ đðŨîêšî àęċÜêĆüĂ÷ŠćÜéĆÜÖúŠćüđöęČĂîĞćöćÖĞćĀîéĂć÷čéšü÷üĉíĊîĚĊÝąöĊÙüćöÙúćéđÙúęČĂîîšĂ÷
ÖćøýċÖþćÙøĆĚÜîĚĊđðŨîÖćøÖĞćĀîé×ĂÜĂĉåÝĞćîüî 3 êĆüĂ÷ŠćÜÝćÖåćî×ĂÜ 3 óøąíćêč ïøĉđüèüĆéðśćĀöćÖĀîŠĂ
êĞćïúÝĆîÝüšć ĂĞćđõĂĒöŠÝĆî ÝĆÜĀüĆéđßĊ÷Üøć÷ ñúÖćøýċÖþćóïüŠćóøąíćêčöĊĂć÷čðøąöćè 600-1,800 ðŘìęĊĒúšü
àÜęċ óøąíćêčđĀúŠćîĚĊĂćÝÝąëĎÖÿøšćÜ×ċĚîêĚĆÜĒêŠÖŠĂîĂćèćÝĆÖøđßĊ÷ÜĒÿî ĂćèćÝĆÖøđßĊ÷ÜĒÿî ĒúąĂćèćÝĆÖøúšćîîć
êćöúĞćéĆï ÝċÜÖúŠćüĕéšüŠćßčößîēïøćèĕéšêĚĆÜëĉęîåćîĔîïøĉđüèîĚĊêĚĆÜĒêŠÖŠĂîĂćèćÝĆÖøđßĊ÷ÜĒÿî ĒúąĔîðŦÝÝčïĆî
ïøĉđüèîĊĚÖ÷Ę ĆÜđðîŨ ìĊĂę ÷ĂĎŠ ćýĆ÷×ĂÜðøąßćßî

ÙćĞ ÿćĞ ÙĆâ : OSL dating Ăć÷čóøąíćêč üéĆ ðśćĀöćÖĀîŠĂ ßčößîēïøćè ĂĞćđõĂĒöŠÝĆî ĂĞćđõĂđßĊ÷ÜĒÿî
ÝĆÜĀüéĆ đßĊ÷Üøć÷

44

Öćø×ĚċîìąđïĊ÷îàćÖéċÖéĞćïøøóŤ

éüÜùìĆ÷ ĒÿĒÿÜÿøĊ Üčš åćîĉß÷ć ĀĂöÿéč ĒúąèĆåíîćÖø ÿÜðøąßć

ÖĂÜÙöčš ÙøĂÜàćÖéċÖéćĞ ïøøóŤ ÖøöìøĆó÷ćÖøíøèĊ 75/10 ë.óøąøćö 6 øćßđìüĊ ÖøÜč đìóöĀćîÙø 10400

ïìÙĆé÷ŠĂ

ÖøöìøĆó÷ćÖøíøèĊ öĊõćøÖĉÝĔîÖćøÙščöÙøĂÜàćÖéċÖéĞćïøøóŤìĊęöĊÙüćöÿĞćÙĆâêŠĂÖćøýċÖþćðøąüĆêĉÙüćö
đðŨîöć×ĂÜēúÖ ïøøóßĊüĉîüĉì÷ć ïøøóßĊüüĉì÷ć éšćîíøèĊüĉì÷ćĀøČĂÖćøúĞćéĆïßĚĆîĀĉî ĒúąüĉüĆçîćÖćø×ĂÜ
ÿęĉÜöĊßĊüĉêïîñČîēúÖ êćöóøąøćßïĆââĆêĉÙčšöÙøĂÜàćÖéċÖéĞćïøøóŤ ó.ý. ģĦĦĢ ÝćÖךĂöĎúàćÖéċÖéĞćïøøóŤĔî
ðøąđìýĕì÷öÖĊ ćøÙîš óïđðîŨ ÝĞćîüîöćÖìęĊĂ÷ĔŠĎ îÖćøÙøĂïÙøĂÜ×ĂÜÖøöìøĆó÷ćÖøíøèĊÝĞćîüîÖüŠćĀöČęîøć÷Öćø
öĊßîĉéàćÖéċÖéĞćïøøóŤðøąöćè Ħġģ ßîĉé/ßČęĂ ĒïŠÜđðŨî àćÖéċÖéĞćïøøóŤöĊÖøąéĎÖÿĆîĀúĆÜ ÝĞćîüî Ĩħ ßîĉé/
ßĂČę àćÖéÖċ éĞćïøøóĕŤ öŠöÖĊ øąéĎÖÿĆîĀúĆÜ ĤĨĢ ßîĉé/ßČęĂ àćÖéċÖéĞćïøøóŤóČßÝĞćîüî ĤĤ ßîĉé/ßęČĂ øŠĂÜøĂ÷éċÖéĞć
ïøøóŤÝĞćîüî Ģ ßîĉé/ßČęĂ ĒúąĂČęîė ÝĞćîüî ģĢ ßîĉé/ßęČĂ ēé÷àćÖéċÖéĞćïøøóŤïćÜÿŠüîìĊęöĊÙüćöÿĞćÙĆâđðŨîĕð
êćöĀúĆÖđÖèæŤÖćøðøąÖćýđðŨîàćÖéċÖéĞćïøøóŤ×ĚċîìąđïĊ÷î àċęÜöĊÙüćöüŠć ĀćÖàćÖéċÖéĞćïøøóŤĕì÷öĊ
ÙüćöÿĞćÙĆâĀøČĂöĊÙčèÙŠćĔîÖćøýċÖþćðøąüĆêĉēúÖ ïøøóßĊüĉî ïøøóßĊüüĉì÷ć ĀøČĂÖćøúĞćéĆïßĚĆîĀĉîìĊęöĊÙčèÿöïĆêĉ
Ă÷ŠćÜĔéĂ÷ŠćÜĀîęċÜ éĆÜîĚĊ Ģ) đðŨîàćÖéċÖéĞćïøøóŤßîĉéĔĀöŠìęĊÙšîóïđðŨîÙøĚĆÜĒøÖ×ĂÜðøąđìý ĀøČĂ×ĂÜēúÖ ĀøČĂ
đðŨîêĆüĂ÷ŠćÜàćÖéċÖéĞćïøøóŤêšîĒïï ģ) đðŨîàćÖéċÖéĞćïøøóŤéĆßîĊìĊęĔߚÚćÜĂĉÜߊüÜĂć÷č×ĂÜßĚĆîĀĉîĕéšĒîŠîĂîĒúą
đðŨîìĊę÷ĂöøĆï×ĂÜðøąđìýĕì÷ĀøČĂøąéĆïÿćÖú Ĥ) đðŨîàćÖéċÖéĞćïøøóŤìęĊöĊúĆÖþèąóĉđýþĀøČĂÙøïëšüîÿöïĎøèŤ
ìĊęÿéč đìŠćìóęĊ ïĔîðøąđìýĕì÷ ĥ) đðŨîàćÖéċÖéĞćïøøóŤ×ĂÜÿĆêüŤìĊęöĊÖøąéĎÖÿĆîĀúĆÜđÞóćąßĚĉîÿŠüîìęĊÿĞćÙĆâ Ēúą Ħ)
đðŨîàćÖéÖċ éĞćïøøóŤßîĉéđéĊ÷üÖîĆ ÖïĆ ßîĉéĀć÷ćÖöćÖìęĊÙšîóïĒúüš

ìĚĆÜîĚĊ Öćø×ċĚîìąđïĊ÷îàćÖéċÖéĞćïøøóŤ×ĂÜðøąđìýĕì÷ öĊüĆêëčðøąÿÜÙŤđóęČĂĔĀšàćÖéċÖéĞćïøøóŤĕì÷ìĊęöĊ
ÙüćöÿĞćÙĆâĕéšøĆïÖćøÙščöÙøĂÜêćöÖãĀöć÷ ĒúąđðŨîđÙøęČĂÜöČĂĔîÖćøúéÙüćöđÿęĊ÷ÜìęĊÝąđÖĉéÙüćöđÿĊ÷Āć÷êŠĂ
àćÖéċÖéĞćïøøóŤìęĊÿĞćÙĆâ×ĂÜðøąđìýìĊęĂćÝđÖĉé×ĚċîĔîĂîćÙê Öćø×ċĚîìąđïĊ÷îàćÖéċÖéĞćïøøóŤêćöìęĊÖĞćĀîéĔî
óøąøćßïĆââĆêĉÙščöÙøĂÜàćÖéċÖéĞćïøøóŤ ó.ý.ģĦĦĢ ðøąÖĂïéšü÷ ÖćøéĞćđîĉîÜćî ģ ךà éĆÜîĚĊ Ģ) ÝĆéìĞć
ìąđï÷Ċ îêćöĒïïìĊÖę ćĞ Āîé ēé÷ÖĞćĀîéøĀĆÿðøąÝĞćàćÖéċÖéĞćïøøóŤ úĆÖþèą øĎðóøøè ÿĆèåćî ×îćé îĞĚćĀîĆÖ
üĆîđéČĂîðŘìĊęóï ßČĚĂÙšîóï ĀøČĂđÝšć×ĂÜ ĀøČĂñšĎÙøĂÜ ÿëćîìęĊìĊęóï óøšĂöøĎðëŠć÷ĔĀšßĆéđÝî Ēúą ģ) ÝĆéìĞć
ðøąÖćýêćöĒïïìĊęÖĞćĀîé ēé÷Ă÷ŠćÜîšĂ÷êšĂÜöĊךĂöĎúêćö Ģ) ĔĀšĂíĉïéĊēé÷ÙüćöđĀĘîßĂï×ĂÜÙèąÖøøöÖćø
ÙščöÙøĂÜàćÖéċÖéĞćïøøóŤðøąÖćýĔîøćßÖĉÝÝćîčđïÖþćĔĀšàćÖéċÖéĞćïøøóŤìęĊ×ĚċîìąđïĊ÷î êĚĆÜĒêŠðŘ ó.ý. ģĦĦĥ –
ó.ý. ģĦħģ ìí. ĕéšéĞćđîĉîÖćø×îċĚ ìąđïĊ÷îàćÖéÖċ éćĞ ïøøóìŤ ĊęöĊÙüćöÿĞćÙĆâéĆÜÖúŠćü ĒúąĕéšðøąÖćý×ċĚîìąđïĊ÷î
àćÖéċÖéĞćïøøóŤĔîðøąÖćýøćßÖĉÝÝćîčđïÖþć ĒúšüÝĞćîüî ģĥĪ êĆüĂ÷ŠćÜ ĒúąÝćÖàćÖéċÖéĞćïøøóŤìĊę×ċĚî
ìąđïĊ÷îĒúšüđĀúćŠ îĊĚ öÝĊ ćĞ îüî ĥĦ êüĆ Ă÷ćŠ ÜìĊđę êø÷Ċ öÖćøðøąÖćýđðŨîàćÖéċÖéĞćïøøóŤìęĊ×ĚċîìąđïĊ÷îìęĊöĊÙčèÿöïĆêĉ
đðîŨ ÿĉęÜìĀęĊ ć÷ćÖĒúąöÙĊ èč ÙćŠ đðîŨ óđĉ ýþÿöÙüøđÖĘïøĆÖþćĕüšđðŨîÿöïĆê×ĉ ĂÜßćêĔĉ îðŘ ó.ý. ģĦħĤ

45 การประชมุ วชิ าการ “ธรณีไทย 2562”, 16-17 กันยายน 2562 ณ โรงแรม เดอะ เบอรเ คลยี  ประตนู ํา้ กรงุ เทพมหานคร

ÖćøÝĆéÖćøÖćøđêöĉ îĚćĞ Ĕêéš îĉ đóČĂę ĔĀđš Öéĉ Ùüćö÷ÜĆę ÷îČ
ÖøèýĊ ċÖþćóĚČîìĊęõćÙêąüîĆ ĂĂÖđÞĊ÷ÜđĀîČĂ

đÖø÷Ċ ÜýĆÖéĉĝ ýøÿĊ č×1, ēó÷ö ÿøćõĉøö÷Ť1,2 Ēúą đÖüøĊ óúđÖîĚĉ 1

1 ÿëćïîĆ üÝĉ Ć÷ìøĆó÷ćÖøîĚĞćĔêšéĉî öĀćüĉì÷ćú÷Ć ×ĂîĒÖŠî Ă.đöČĂÜ Ý.×ĂîĒÖîŠ 40002
2 õćÙüßĉ ćüĉýüÖøøöđÖþêø Ùèąüýĉ üÖøøöýćÿêøŤ öĀćüìĉ ÷ćúĆ÷×ĂîĒÖîŠ Ă.đöČĂÜ Ý.×ĂîĒÖîŠ 40002

ïìÙĆé÷ĂŠ

ÖćøóçĆ îćìøóĆ ÷ćÖøîĚĞćĔêšéĉîìćĞ ĔĀđš Öéĉ ðøąē÷ßîĔŤ îđßÜĉ đýøþåýćÿêøŤ ÿÜęĉ ĒüéúšĂö Ēúąñúðøąē÷ßîŤêŠĂ
öîčþ÷Ť ÖćøîĞćìøĆó÷ćÖøîĚĞćĔêšéĉî×ĚċîöćĔßšĂ÷ŠćÜ÷ęĆÜ÷ČîÙüøìøćïëċÜðøĉöćèÖćøÖĆÖđÖĘïĒúąðøĉöćèÖćøđêĉöîĞĚć
ēé÷íøøößćêĉìĚĆÜìćÜêøÜĒúąìćÜĂšĂö ēé÷ðÖêĉÖćøđêĉöîĚĞćĔêšéĉîêćöíøøößćêĉÝćÖîĞĚćòîĔîĒêŠúąóČĚîìęĊĒêÖêŠćÜ
ÖĆî×îċĚ Ă÷ÖĎŠ ĆïÿõćóõöĎ ĉĂćÖćý ÙüćöúćéđĂĊ÷ÜõöĎ ĉðøąđìý Ăìč Öüìĉ ÷ć ßîĉééîĉ ÿõćóíøèüĊ ìĉ ÷ć ÖćøĔßšìęĊéĉî Ēúą
ĂęČîė îĚĞćòîöĊÖćøàċö×ĂÜúÜÿĎŠîĚĞćĔêšéĉîðøąöćè 10 -30% ×ĂÜðøĉöćèòîìęĊêÖ ĔîïøĉđüèóČĚîìĊęđêĉöîĚĞć
(Recharge area) Ēúą ðøąöćè 0-10% ×ĂÜðøĉöćèòîìęĊêÖ ĔîóČĚîìĊęÿĎâđÿĊ÷îĞĚć (Discharge area) ÖćøĔßšîĚĞć
ïćéćúìĊę÷ÜęĆ ÷îČ ÙüøĔßšĔĀšîĂš ÷ÖüŠćĀøČĂđìŠćÖïĆ ðøĉöćèÖćøđêĉöîĞĚćĔêšéĉîēé÷íøøößćêĉ ĒêŠðŦÝÝčïĆîóïüŠćĀúć÷óČĚîìĊę
öÖĊ ćøĔßîš ćĚĞ đÖĉîÿöéčúöćÖ×îĚċ éĆÜîĚĆîÖćøÝĆéÖćøđêöĉ îĚĞćĔêšéĉî (Managed Aquifer Recharge, MAR) éšü÷üĉíĊÖćø
êćŠ Üė đóČĂę đÿøĉöĒúąđóęĉöðøĉöćèÖćøđêöĉ îĞĚćÝćÖ×ïüîÖćøìćÜíøøößćêĉ ÝÜċ öĊÙüćöÝĞćđðŨîēé÷đÞóćąĔîõćüąÖćø
đðúĊę÷îĒðúÜõĎöĉĂćÖćý (climate change) ĒúąÖćøĔßìš éęĊ îĉ ìęđĊ Öéĉ ×ċĚîĂ÷ćŠ Üøîč ĒøÜĒúąøüéđøĘü Ĕî×èąîĊĚÖćøđêĉö
îĞĚćÿĎŠßĚĆîîĚĞćĔêšéĉî đéĉöîĉ÷öđøĊ÷ÖüŠć ÖćøđêĉöîĚĞćĔêšéĉîđìĊ÷ö (Artificial recharge) ĒêŠõć÷ĀúĆÜöĊïćÜðøąđìý
đøĊ÷ÖüŠć ÖćøđóęĉöÖćøđêĉöîĚĞćĔêšéĉî (enhanced recharge) íîćÙćøîĞĚć (water banking) ĀøČĂ ÖćøÖĆÖđÖĘïîĚĞć
Ĕêšñĉüéĉî (subsurface storage) đðŨîêšî êŠĂöćõć÷ĀúĆÜÖćøđêĉöîĞĚćĔêšéĉîĒóøŠĀúć÷öćÖ×ċĚîĒúąöĊÖćø
éćĞ đîîĉ ÖćøïćÜĒĀŠÜìĕĊę öđŠ ĀöćąÿöêĂŠ ÿõćóĒüéúšĂö ÝċÜđÖĉéÖćøðøĆïðøčÜÖøąïüîÖćøĔĀšøĆéÖčö÷ĉęÜ×ċĚîĒúąđøĊ÷ÖüŠć
ÖćøÝĆéÖćøÖćøđêĉöîĚĞćĔêšéĉî (Managed Aquifer Recharge, MAR) ÙČĂ “ÖćøđêĉöîĚĞćĔêšéĉîēé÷đÝêîć
(intentional recharge) éšü÷îĚĞćÿŠüîđÖĉî (surplus water) ÿŠĎßĆĚîĀĉîĂščöîĚĞć (aquifers) đóČęĂîĞćÖúĆïöćĔßš
(recovery) ĀøČĂđóęČĂðøąē÷ßîŤéšćîÿĉęÜĒüéúšĂö đðŨîÖøąïüîÖćøđêĉöîĚĞćĔêšéĉîìęĊöĊÝĆéÖćøđóęČĂìĞćĔĀšöęĆîĔÝüŠćÖćø
đêĉöîĚĞćĔêšéĉîÝąĕöŠÖøąìïêŠĂÿč×õćó×ĂÜöîčþ÷ŤĒúąÙčèõćóÿęĉÜĒüéúšĂö ßĆĚîîĚĞćïćéćúÝąĕéšøĆïÖćøđêĉöîĚĞćÝćÖ
ÖćøñĆîîĚĞćöćđêĉöñŠćîïŠĂïćéćú (wells) ĀøČĂĔßšÖøąïüîÖćøàċöñŠćîñĉüéĉî (infiltration) ×ĂÜÿøąđêĉöîĚĞć
(basins) øąđïĊ÷Üđêöĉ îćĞĚ Ĕêšéĉî (recharge galleries) ĀøČĂ ĒöîŠ ĚćĞ ĒúąÖćøÝĆéÖćøđêĉöîĚĞćĔêšéĉîîĚĊĕöŠĔߊüĉíĊÖćøđóČęĂ
ÖĞćÝĆéîćĚĞ đÿ÷Ċ

üĆêëðč øąÿÜÙŤ×ĂÜđĂÖÿćøîĚĊđóĂęČ ÿøšćÜÙüćöđךćĔÝ×ĂÜøąïïÖćøÝĆéÖćøÖćøđêĉöîĚĞćĔêšéĉîĒúąÖćøîĞćđÿîĂ
ñúÖćøýċÖþćñúÖøąìïêĂŠ ÿęĉÜĒüéúšĂö×ĂÜóîĚČ ìĊęêŠćÜė ĔîõćÙêąüîĆ ĂĂÖđÞĊ÷ÜđĀîČĂìęĊöĊðŦâĀć×ćéĒÙúîĒĀúŠÜîĞĚć
Ĕêšéîĉ ĒúąðâŦ Āć×ĂÜîĞĚćĔêéš ĉîÖøŠĂ÷ĒúąđÙĘö óøšĂöìĚÜĆ đÿîĂĒîüÙéĉ ĔîÖćøüćÜĒñîđóĂČę ĔĀđš ÖĉéÖćøðäïĉ êĆ Öĉ ćø Öćø
ÝĆéÖćøÖćøđêĉöîĚĞćĔêšéĉîÙüøöĊÖćøðøąđöĉîëċÜÙüćöđðŨîĕðĕéš×ĂÜøąïïêŠćÜė 7 éšćî ĕéšĒÖŠ 1) øąïïĂčìÖüĉì÷ć
×ĂÜóĚČîìęĊîĆĚîė ĀøČĂúčŠöîĚĞć 2) ÖćøÿĞćøüÝìćÜĂčìÖíøèĊüĉì÷ćđóęČĂÙĆéđúČĂÖĒúąðøąđöĉîñúÙüćöđðŨîĕðĕéš×ĂÜ
óČĚîìĊę 3) ÙüćöđÿęĊ÷ÜêĂŠ ÿõćóĒüéúšĂö 4) ÖćøÙĆéđúČĂÖüĉíĊÖćøÖŠĂÿøšćÜ 5) đýøþåýćÿêøŤ ÙŠćĔߚ݊ć÷ ñúðøąē÷ßîŤ
ìęĊĂćÝĕéšøĆï 6) ÖćøöĊÿŠüîøŠüö×ĂÜñĎšìęĊöĊÿŠüîĕéšđÿĊ÷ĒúąÖćø÷ĂöøĆï×ĂÜÿĆÜÙöìĊęđÖęĊ÷üךĂÜĒúą 7) ÖãøąđïĊ÷ïÖćø

46

ðäĉïĆêĉĒúąĂÜÙŤÖøêŠćÜė ĀøČĂ×ĂÜøĆå éĆÜîĚĆîÖŠĂîđøęĉöéĞćđîĉîÖćøÝĆéÖćøđêĉöîĞĚćĔêšéĉîđóČęĂüĆêëčðøąÿÜÙŤĔéė ÙüøöĊ
ÖćøüćÜĒñîðäïĉ êĆ Ēĉ úąđðîŨ ×ĆĚîêĂîĔĀšßĆéđÝî öĔĉ ßđŠ øęöĉ ÝćÖÿŠüîĔéÿŠüîĀîÜċę ×ĂÜøąïïÖćøðøąđöîĉ

ÖćøÝĆéÖćøÖćøđêĉöîĚĞćĔîóČĚîìęĊìęĊöĊÙüćöđÿęĊ÷ÜéšćîÖćøĒóøŠÖøąÝć÷×ĂÜîĚĞćÖøŠĂ÷ĒúąđÙĘö đߊîìĊęõćÙ
êąüĆîĂĂÖđÞĊ÷ÜđĀîČĂ ÙüøéĞćđîĉîÖćøéšü÷ÙüćöøĂïÙĂï öĊöćêøÖćøÖćøđêĉöîĞĚćĔêšéĉîìęĊđĀöćąÿöĒúąüĉíĊÖćø
ÙĆéđúČĂÖóĚČîìĊęøŠüöÖĆïüĉíĊÖćøÖŠĂÿøšćÜìęĊđĀöćąÿö öĊÖćøðøąđöĉîñúÖøąìïđóČęĂĕöŠĔĀšđÖĉéÖćøĒóøŠÖøąÝć÷×ĂÜ
îĚĞćđÙĘööćÖ×ċĚîĀøČĂĂćÝìĞćĔĀšđÖĉéðøąē÷ßîŤìĊęÝąñúĆÖéĆîîĚĞćđÙĘöĂĂÖĕð ÖćøîĞćđÿîĂñúÜćîÙøĆĚÜîĚĊĕéšîĞćñú
ÖćøýċÖþćÖćøđóöęĉ đêĉöîćĞĚ Ĕêéš ĉîēé÷üĉíĊíøøößćêĒĉ úąÖćøÝĆéÖćøÖćøđóęöĉ đêĉöîĞĚćĔêšéĉîìĊęìĞćĔĀšđÖĉéÖćøđðúęĊ÷îĒðúÜ
ÖćøĕĀú×ĂÜîćĞĚ Ĕêéš îĉ ĒúąñúÖøąìïêĂŠ ÿõćóĒüéúšĂöĔîøĎðĒïïêŠćÜė×ĂÜóĚČîìęĊìĊęöĊúĆÖþèąìćÜĂčìÖíøèĊüĉì÷ć
ĒúąÙüćöøčîĒøÜ×ĂÜîĚĞćĔêšéĉîđÙĘöìĊęĒêÖêŠćÜÖĆî đߊî óĚČîìęĊúčŠöîĞĚćÿÜÙøćö óČĚîìĊęúŠčöîĚĞćßĊêĂîÖúćÜ ĒúąóČĚîìęĊúčŠö
îĞĚćöĎú øüöìĆĚÜÖćøÖĆÖđÖĘïîĞĚćñĉüéĉîĕüšĔîóČĚîìęĊòść÷êŠćÜė ñúÖćøýċÖþćÖćøđðúęĊ÷îĒðúÜìĉýìćÜÖćøĕĀúĒúą
øĎðĒïïÖćø×ĂÜîĞĚćĔêšéĉîÝąîćĞ ĕðÿŠĎĒîüìćÜĔîÖćøÙéĆ đúĂČ ÖóîČĚ ìđĊę Āöćąÿö ĀúĊÖđú÷ęĊ ÜÖćøĒóøÖŠ øąÝć÷×ĂÜîĞĚćđÙĘö
ߊü÷úéÙüćöøîč ĒøÜ×ĂÜîĚĞćđÙĘö ĒúąüĉíĊÖćøðøąđöĉîÙüćöđÿęĊ÷Ü×ĂÜÖćøÝĆéÖćøÖćøđêöĉ îĚćĞ Ĕêšéĉîéüš ÷

ïìïćìÖćøÝĆéÖćøđêĉöîĞĚćĔêšéĉîđðŨîĀîšćìĊę×ĂÜĔÙø ĀîŠü÷Üćî×ĂÜøĆåĀøČĂđĂÖßî ìĊęÝąüćÜĒñî ÖĞćĀîé
ÖãđÖãæĒŤ úąÝéĆ ìĞćÙöŠĎ ČĂðäĉïêĆ ĉĒúąĒñîĒöŠïì ìÙĊę øĂïÙúöč ÖćøðøąđöĉîìĚĆÜ 7 éšćîìęĊÖúŠćüöćךćÜêšî øüöìĚĆÜÖćø
ÝĆéìĞćĒñîìęĊÙüćöđĀöćąÿöĔîÖćøéĞćđîĉîÖćøÝĆéÖćøđêĉöîĞĚć (Suitability Map for MAR) đóČęĂĔĀšēÙøÜÖćøÖćø
đêĉöîĞĚćĔêšéĉîĔîóČĚîìĊęêŠćÜėđÖĉéÙüćöĂ÷ŠćÜ÷ĆęÜ÷Čî ÖćøÝĆéÖćøÖćøđêĉöîĞĚćĔêšéĉî (MAR) ĕöŠĔߊđðŨîđøęČĂÜĔĀöŠÿĞćĀøĆï
ðøąđìýĕì÷ ĒêŠÙüćöđךćĔÝìĊęëĎÖêšĂÜĂćÝÝąđðŨîđøČęĂÜĔĀöŠÿĞćĀøĆïïčÙÙúĒúąðøąßćßîïćÜÖúŠčö ÖćøÝĆéÖćøđêĉö
îĞĚćĔêšéĉîĀøČĂîĞĚćïćéćúÝċÜđðŨîÖĉÝÖøøöÿŠüîĀîęċÜ×ĂÜøąïïÖćøóĆçîćìøĆó÷ćÖøîĞĚćĔêšéĉî Ĕî×èąîĊĚĀúć÷ĂÜÙŤÖø
ĒúąĀúć÷ĀîŠü÷ÜćîĕéĔš ĀšÙüćöÿîĔÝĒúąéĞćđîĉîÖćøÖŠĂÿøšćÜĔîóĚČîìęĊêŠćÜėĒúšü ïìïćì×ĂÜîĆÖüĉßćÖćøĔîĂćßĊó
ìęĊđÖĊę÷ÜךĂÜ đߊîîĆÖíøèĊüĉì÷ć îĆÖĂčìÖíøèĊüĉì÷ć ĒúąüĉýüÖøÝąĂ÷ŠĎêøÜĕĀî ÙüøÿøšćÜÙüćöđךćĔÝĔîđøęČĂÜøąïï
ÖćøđêĉöîĚĞćĔĀšëĎÖêšĂÜĒúąîĞćÙüćöøšĎìĊęëĎÖêšĂÜöćߊü÷óĆçîćøąïïĔĀšđÖĉéÙüćö÷ęĆÜ÷Čî Ēúą÷ĆÜđðŨîēĂÖćÿéĊĔîÖćø
đêø÷Ċ öïÙč úćÖøđóĂČę ÝąđðŨîñĕšĎ éøš ĆïĔïĂîčâćêüĉßćßóĊ Ĕîÿć×ćìĊêę šĂÜÙüïÙčöĔîĂîćÙêĂĆîĔÖúšîĊĚ

ÙĞćÿĞćÙĆâ: ÖćøÝĆéÖćøÖćøđêĉöîĚĞćĔêšéĉî (MAR) Ùüćö÷ęĆÜ÷Čî účŠöîĞĚć ē×Ü-ßĊ-öĎú íøèĊüĉì÷ć ĂčìÖ
íøèĊüìĉ ÷ć üßĉ ćßóĊ íøèüĊ ĉì÷ć

47 การประชมุ วชิ าการ “ธรณไี ทย 2562”, 16-17 กนั ยายน 2562 ณ โรงแรม เดอะ เบอรเ คลยี  ประตนู า้ํ กรงุ เทพมหานคร

ÖćøÝéĆ ìćĞ ÙúÜĆ êüĆ Ă÷ćŠ ÜĂćš ÜĂÜĉ ìćÜíøèüĊ ìĉ ÷ć

ßćâđéß ÝĆîìøĆêîŤ, øĆßîĊüøøè ĔÝ×Ăš ĒúąÖĉêêĉ ×ćüüđĉ ýþ

ÖĂÜíøèüĊ ĉì÷ć ÖøöìøĆó÷ćÖøíøèĊ 75/10 ë.óøąøćö 6 øćßđìüĊ ÖøÜč đìóöĀćîÙø 10400

ïìÙéĆ ÷ŠĂ

ÖćøÝĆéìĞćÙúĆÜêĆüĂ÷ŠćÜìćÜíøèĊüĉì÷ć đóęČĂđÖĘïøĆÖþćĒúąøüïøüöĀúĆÖåćîĂšćÜĂĉÜìćÜíøèĊüĉì÷ć
ðøąÖĂïéšü÷êĆüĂ÷ŠćÜìćÜíøèĊüĉì÷ćìęĊöĊÖćøđøĊ÷ÖßęČĂĒêÖêŠćÜÖĆîĔîõćþćĂĆÜÖùþ đߊî Geological material
ĀøČĂ Geoscience data and collections àęċÜēé÷øüöĒúšüĀöć÷ëċÜíøèĊüĆêëč ĕéšĒÖŠ Āĉî ĒøŠ êąÖĂî Ēúą
àćÖéċÖéĞćïøøóŤ đðŨîêšî ךĂöĎúíøèĊüĉì÷ć Āöć÷ëċÜךĂöĎúĒúąđĂÖÿćøìĊęđÖęĊ÷üךĂÜÖĆïíøèĊüĉì÷ć đߊî
øć÷ÜćîÖćøýċÖþćüĉÝĆ÷ ĒñîìęĊ õćóüćé õćóëŠć÷ìęĊöĊîĆ÷ÿĞćÙĆâìćÜíøèĊüĉì÷ć ךĂöĎúÖćøÿĞćøüÝìćÜíøèĊôŗÿĉÖÿŤ
ĒúąñúÖćøüĉđÙøćąĀìŤ ćÜđÙöĒĊ úąìćÜÖć÷õćó đðŨîêšî

ÖĂÜíøèĊüĉì÷ć ÖøöìøĆó÷ćÖøíøèĊ ĕéšéĞćđîĉîÖćøĔîÖćøóĆçîć øüïøüö ĒúąÝĆéđÖĘï
ĀúĆÖåćîìćÜíøèĊüĉì÷ć đóČęĂÖćøđøĊ÷îøĎš ÖćøüĉÝĆ÷ ĒúąÖćøĂšćÜĂĉÜ øüöìĚĆÜÿćöćøëđðŨîĒĀúŠÜđøĊ÷îøšĎìćÜéšćî
íøèĊüĉì÷ć×ĂÜðøąđìýĕì÷ ēé÷öĊĂćÙćøÙúĆÜêĆüĂ÷ŠćÜìćÜíøèĊüĉì÷ć è ýĎî÷ŤüĉÝĆ÷ìøĆó÷ćÖøĒøŠĒúąĀĉî ÝĆÜĀüĆé
øą÷ĂÜ đðŨîÿëćîìĊęøüïøüö ĒúąđÖĘïøĆÖþćêĆüĂ÷ŠćÜìćÜíøèĊüĉì÷ćìĊęÿĞćÙĆâ õć÷ĔîĂćÙćøÙúĆÜêĆüĂ÷ŠćÜ öĊêĎšđÖĘï
êĆüĂ÷ŠćÜ×îćéöćêøåćî ÝĞćîüî 32 êšĎ ßĆĚîđÖĘïêĆüĂ÷ŠćÜìĊęöĊ×îćéóĉđýþ (ÖšĂîĔĀ⊠öĊÝĞćîüîøüö 18 êĆü)
ÿćöćøëÝĆéđÖĘïêĆüĂ÷ŠćÜĕéš 15,000 êĆüĂ÷ŠćÜ ĒúąöĊĀšĂÜðäĉïĆêĉÖćøìĊęøĂÜøĆïÜćîüĉÝĆ÷ Ăćìĉđߊî ĀšĂÜüĉÝĆ÷ÙúĆÜ
êüĆ Ă÷ćŠ Ü ĀšĂÜðäĉïêĆ ĉÖćøýĉúćüøøèîć ĀšĂÜðäĉïĆêĉÖćøõćóëŠć÷êĆüĂ÷ŠćÜ ĀšĂÜðäĉïĆêĉÖćøêĆüĂ÷ŠćÜĒñŠîĀĉîïćÜĒúą
õćóëŠć÷ đðŨîêšî êĚĆÜĒêŠðŘ ó.ý. 2553 ÝîëċÜ ó.ý. 2562 ĒúąöĊêĆüĂ÷ŠćÜĀúĆÖåćîìćÜíøèĊüĉì÷ćÝĆéđÖĘïĔî
øąïïÙúĆÜêĆüĂ÷ŠćÜÝĞćîüî 6,469 êĆüĂ÷ŠćÜ ÿćöćøëÝĞćĒîÖðøąđõìêĆüĂ÷ŠćÜìćÜíøèĊüĉì÷ćĕéšđðŨî 8 ðøąđõì
ĕéšĒÖŠ 1) êĆüĂ÷ŠćÜĀĉîÝćÖóČĚîìĊęìęĆüðøąđìý ÝĞćîüî 4,296 êĆüĂ÷ŠćÜ 2) êĆüĂ÷ŠćÜàćÖéċÖéĞćïøøóŤÝĞćîüî 326
êĆüĂ÷ŠćÜ 3) êĆüĂ÷ŠćÜĒøŠÝĞćîüî 121 êĆüĂ÷ŠćÜ 4) êĆüĂ÷ŠćÜöćêøåćîúĞćéĆïßĚĆîĀĉîÝĞćîüî 663 êĆüĂ÷ŠćÜ 5)
êĆüĂ÷ŠćÜóĉđýþ(Āîĉ ×îćéĔĀâ)Š ÝĞćîüî 497 êĆüĂ÷ŠćÜ 6) êĆüĂ÷ćŠ ÜêąÖĂî ÝĞćîüî 339 êĆüĂ÷ŠćÜ 7) êĆüĂ÷ŠćÜìćÜ
íøèĊüĉì÷ćìćÜēÙøÜÿøšćÜ 1 êĆüĂ÷ŠćÜ Ēúą 8) êĆüĂ÷ŠćÜìćÜíøèĊüĉì÷ćÝćÖêŠćÜðøąđìýÝĞćîüî 226 êĆüĂ÷ŠćÜ
êĆüĂ÷ŠćÜìĆĚÜĀöéÝąëĎÖîĞćđךćøąïïÙúĆÜêĆüĂ÷ŠćÜ đóČęĂÖćøóĆçîćĒúąïøĉĀćøÝĆéÖćøךĂöĎúøąïïÙúĆÜêĆüĂ÷ŠćÜ
×ĂÜðøąđìý óøšĂöìĚĆÜĔĀšïøĉÖćøĔîÖćøÿČïÙšîךĂöĎúĒúąêĆüĂ÷ŠćÜĂšćÜĂĉÜìćÜíøèĊüĉì÷ćĕéšÝćÖåćîךĂöĎúĔîøąïï
ĂĂîĕúîŤ ñŠćîìćÜ http://bgs.dmr.go.th ĒúąÝĆéìĞćøąïïÿČïÙšîéšü÷ÙĉüĂćøŤēÙÿ (QR code) öćĔßšÙüïÙŠĎÖĆï
ïĆêøךĂöĎúêĆüĂ÷ŠćÜ àęċÜĔĀšÙüćöÿąéüÖøüéđøĘüĔîÖćøĔĀšïøĉÖćø ēé÷öĊĒñîÜćîìęĊÝąĔĀšïøĉÖćø×ĂÜÙúĆÜêĆüĂ÷ŠćÜ
đߊî Öćø×Ăđךćđ÷ęĊ÷ößö Öćø×ĂýċÖþćêĆüĂ÷ŠćÜõć÷ĔîÙúĆÜêĆüĂ÷ŠćÜíøèĊüĉì÷ć Öćø×ĂĒïŠÜêĆüĂ÷ŠćÜíøèĊüĉì÷ć
ĒúąÖćø×Ă÷ČöêĆüĂ÷ŠćÜđóČęĂÖćøÝĆéĒÿéÜ øąïïÙúĆÜêĆüĂ÷ŠćÜĂšćÜĂĉÜìćÜíøèĊüĉì÷ć ÖøöìøĆó÷ćÖøíøèĊ ÝąëĎÖ
óĆçîćĕðóøšĂöÖĆîĔîìčÖéšćîìĊęÖúŠćüöćĔîđïČĚĂÜêšî đóęČĂĔĀšđðŨîøąïïåćîךĂöĎúÙúĆÜêĆüĂ÷ŠćÜĂšćÜĂĉÜìćÜ
íøèĊüĉì÷ć×ĂÜðøąđìý ÿćöćøëéĞćđîĉîÖćøñŠćîøąïïĂĂîĕúîŤ ÿąéüÖ ĒúąøüéđøĘü øüöëċÜÖćøóĆçîćĔĀšđðŨî
øąïïÙúĆÜêĆüĂ÷ŠćÜìćÜíøèĊüĉì÷ćĔĀšđðŨîēÙøÜ׊ć÷ìćÜøąïïÙúĆÜêĆüĂ÷ŠćÜ×ĂÜðøąđìýĕì÷ đóęČĂøĂÜøĆïÜćîüĉÝĆ÷
ìćÜéšćîíøèüĊ ìĉ ÷ć×ĂÜðøąđìýĒúąÝąîĞćĕðÿŠÖĎ ćøóĆçîćðøąđìýĔĀđš Ýøâĉ Öćš üĀîšćêŠĂĕðĂĊÖĔîĂîćÙê

48
øĎðìĊę 1 ÙúĆÜêĆüĂ÷ŠćÜĂšćÜĂĉÜìćÜíøèĊüĉì÷ć ÖøöìøĆó÷ćÖøíøèĊ ÖøąìøüÜìøĆó÷ćÖøíøøöØćêĉĒúąÿĉęÜĒüéúšĂö
ðøąđìýĕì÷

49 การประชมุ วชิ าการ “ธรณไี ทย 2562”, 16-17 กนั ยายน 2562 ณ โรงแรม เดอะ เบอรเ คลีย ประตูนํ้า กรงุ เทพมหานคร

ÖćøđßĂęČ öē÷ÜÙüćöøìĎš ćÜíøèüĊ ìĉ ÷ć×ĂÜëĞćĚ ĀúüÜ-×čîîĞĚćîćÜîĂî
đ×ćš ÖïĆ ĀúĆÖÿĎêøÖćøđøĊ÷îÖćøÿĂîĔîēøÜđø÷Ċ îìĂš Üëĉîę

îć÷ĂîÖč úĎ üÜýŤĔĀâŠ

ÖøöìøóĆ ÷ćÖøíøèĊ

ïìÙĆé÷ĂŠ

ÖøèìĊ öĊ ĀöðĎ ść 13 ßĊüêĉ êĉéĔîëćĞĚ ĀúüÜ-×îč îĞĚćîćÜîĂî ĂćĞ đõĂĒöŠÿć÷ ÝĆÜĀüĆéđßĊ÷Üøć÷ øąĀüŠćÜüĆîìęĊ 23
öĉëčîć÷î 2561 ëċÜüĆîìęĊ 10 ÖøÖãćÙö 2561 ìĞćĔĀšëĚĞćĀúüÜÖúć÷đðŨîëĞĚćìęĊđðŨîìĊęøĎšÝĆÖĂ÷ŠćÜĒóøŠĀúć÷ìĆęüēúÖ
ÝćÖîîĚĆ ÖćøëĂéïìđø÷Ċ î ÖćøÿĞćøüÝĒúąôîŚŪ ôëĎ ĚĞćĀúüÜ×ĂÜĀîüŠ ÷ÜćîêŠćÜ ė ÝÜċ ĕéđš Öéĉ ×ċĚîĂ÷ćŠ ÜđðŨîøąïï

õć÷ĔêšÖćøéĞćđîĉîÜćî×ĂÜõćÙÖćøýċÖþćĔîìšĂÜëĉęîøŠüöÖĆïÖøąìøüÜìøĆó÷ćÖøíøøößćêĉĒúą
ÿęĉÜĒüéúšĂö ĕéšđÖĉéĒîüÙĉéĔîÖćøđßČęĂöē÷ÜÙüćöøšĎìćÜíøèĊüĉì÷ć ëĚĞćüĉì÷ć ĒúąĂčìÖíøèĊüĉì÷ć đךćÖĆïïìđøĊ÷î
ĔîøąïïÖćøđø÷Ċ îÖćøÿĂîĔîìšĂÜëęĉîìęĊÿĂéÙúšĂÜÖĆïöćêøåćî×ĂÜÖøąìøüÜýċÖþćíĉÖćø×Ěċî ēé÷öĊđðŜćĀöć÷ìĊęÝą
ĂćýĆ÷öøéÖìćÜíøèĊĔîìšĂÜëĉęîìęĊđðŨîìĊęøĎšÝĆÖÖĆîéĊĔîóĚČîìĊę öćđðŨîåćîÖćøđøĊ÷îøĎšìĊęìĚĆÜÙøĎĒúąîĆÖđøĊ÷îđךćëċÜĕéšÜŠć÷
ÿćöćøëêŠĂ÷ĂéđךćÖĆïÖćøđøĊ÷îøšĎĔîøąïï×ĂÜßčößî ēé÷ÝĆéìĞćđðŨîßčéÖćøđøĊ÷îøĎš đøęČĂÜ “ëĚĞćĀúüÜÖĆïÖćø
đðúęĊ÷îĒðúÜìćÜíøèĊüìĉ ÷ćïîđðúĂČ ÖēúÖ” ÿĞćĀøĆïîĆÖđø÷Ċ îøąéïĆ ßîĚĆ öĆí÷öýÖċ þćðìŘ Ċę ģ ìęĔĊ ßšøŠüöÖïĆ ĒĀúÜŠ đøĊ÷îøĎš
ĔîìšĂÜëęĉî (ëĚĞćĀúüÜ-×čîîĞĚćîćÜîĂî) Ĕîøć÷üĉßćüĉì÷ćýćÿêøŤóĚČîåćî ÖúčŠöÿćøąÖćøđøĊ÷îøĎšüĉì÷ćýćÿêøŤêćö
ĀúÖĆ ÿĎêøĒÖîÖúćÜÖćøýċÖþć×îĚĆ óîĚČ åćî ó.ý. ģĦĦĢ (ÞïïĆ ðøĆïðøÜč ģĦħġ) ×ĂÜÖøąìøüÜýÖċ þćíÖĉ ćø

ÖćøîĞćđÿîĂĔîÙøĆĚÜîĊĚ đðŨîÖćøÿąìšĂîĒîüÙĉéìęĊĔßšĔîÖćøóĆçîćßčéÖćøđøĊ÷îøĎš “ëĞĚćĀúüÜÖĆïÖćø
đðúęĊ÷îĒðúÜìćÜíøèĊüĉì÷ćïîđðúČĂÖēúÖ” àęċÜÙèąñšĎÝĆéìĞćĕéšĔĀšÙüćöÿĞćÙĆâÖĆïÙüćöÿĂéÙúšĂÜÖĆïøąïïÖćø
đø÷Ċ îÖćøÿĂîêćööćêøåćî×ĂÜÖøąìøüÜýċÖþćíĉÖćø ÙüćöđĀöćąÿöÖĆïßüŠ ÜüĆ÷×ĂÜîĆÖđø÷Ċ î ÖćøöĊÿŠüîøŠüö×ĂÜ
ïčÙúćÖøĔîøąïïÖćøýċÖþć îĆÖüĉßćÖćøĔîÿć÷ĂćßĊó ĒúąĂÜÙŤÖøđĂÖßîĔîÖćøìĞćÜćîøŠüöÖĆîđóęČĂóĆçîćßčéÖćø
đø÷Ċ îøšĎ ĒúąìĊÿę ĞćÙâĆ ÷Üęĉ ÙĂČ ĔĀšÙüćöÿćĞ ÙâĆ ÖĆïÙüćö÷ÜęĆ ÷Čî×ĂÜÖøąïüîÖćøÖćøýÖċ þćđø÷Ċ îøšĎìęĊÝąđÖĉé×Ěîċ ĔîìšĂÜëęĉî

ïìÿøčð×ĂÜÖćøóĆçîćßčéÖćøđøĊ÷îøšĎĔîÙøĆĚÜîĊĚîĞćĕðÿŠĎêšîĒïïÖćøðøĆïðøčÜĒîüìćÜÖćøđñ÷ĒóøŠĂÜÙŤ
ÙüćöøĎšĒúąÖćøìĞćÜćî×ĂÜÖøöìøĆó÷ćÖøíøèĊĔîìćÜìĊęĔĀšÙüćöÿĞćÙĆâÖĆïñšĎĔߚךĂöĎúĒúąÖćøöĊñĎšøĆïïøĉÖćøđðŨî
ýîĎ ÷ŤÖúćÜöćÖ×îĚċ àÜęċ ÿĂéøĆïÖĆïÿõćóÙüćöêšĂÜÖćøĔîÖćøóĆçîćðøąđìýĔî÷čÙðŦÝÝïč îĆ

50

ÖćøêøüÝÿĂïÙüćöêŠĂđîęĂČ Ü×ĂÜĀúčö÷čïĒúąēóøÜĔêšéîĉ éüš ÷üĉíĊÖćøÿćĞ øüÝíøèôĊ ÿŗ Öĉ ÿŤ
óĚČîìĂęĊ ĞćđõĂìčŠÜĀüšć ÝĆÜĀüéĆ ÿêúĎ

ýõč üĉß⍠÷ĂĒÿÜøĆêî,Ť ÝĆÖøóîĆ íŤ ÙćĞ ïâč đøČĂÜ, íâĆ øĆêîŤ üîĉ Ć÷óćîĉß Ēúą õèĆ æøÖĆ þŤ ßćâèøÜÙŤ

ÖĂÜđìÙēîēú÷ĊíøèĊ ÖøöìøĆó÷ćÖøíøèĊ 75/10 ë.óøąøćö 6 øćßđìüĊ ÖøčÜđìóöĀćîÙø 10400

ïìÙĆé÷ŠĂ

Āúčö÷čï ÝĆéđðŨîíøèĊóĉïĆêĉõĆ÷ĀîċęÜĔîóČĚîìĊęĂĞćđõĂìčŠÜĀüšć ÝĆÜĀüĆéÿêĎú ìęĊÖŠĂĔĀšđÖĉéÙüćöđÿĊ÷Āć÷ìĚĆÜêŠĂ
ßĊüĉêĒúąìøĆó÷Ťÿĉî×ĂÜÙîĔîóČĚîìĊę ðŘ 2562 ÖøöìøĆó÷ćÖøíøèĊ ēé÷ÿĞćîĆÖÜćîìøĆó÷ćÖøíøèĊđ×ê 4 ĕéšøĆïĒÝšÜ
ÖćøđÖĉéĀúčö÷čïÝĞćîüî 3 ĒĀŠÜÙČĂ ïšćîíćøðúĉü êĞćïúìčŠÜĀüšć ïšćîìŠčÜ÷ćüîšč÷ ĒúąĀîšćÿĞćîĆÖÜćîĂÜÙŤÖćø
ïøĉĀćøÿŠüîêĞćïúðśćĒÖŠïŠĂĀĉî êĞćïúðśćĒÖŠïŠĂĀĉî ĂĞćđõĂìŠčÜĀüšć ÝĆÜĀüĆéÿêĎú ÖćøêøüÝÿĂïĀúčö÷čïĒúąÙüćö
êŠĂđîęČĂÜ×ĂÜēóøÜĔêšéĉîÿćöćøëìĞćéšü÷ÖćøÿĞćøüÝíøèĊôŗÿĉÖÿŤéšü÷üĉíĊüĆéÿõćóêšćîìćîĕôôŜćĒïï 2 öĉêĉ ĒúąüĉíĊ
üéĆ éšü÷ÿâĆ âćèđøéćøŤ

ÖćøÿĞćøüÝĔîÙøĚĆÜîĚĊ öĊüĆêëčðøąÿÜÙŤđóęČĂêøüÝÿĂïēÙøÜÿøšćÜĔêšéĉî ĒúąÙüćöêŠĂđîČęĂÜ×ĂÜĀúčö÷čïĒúą
ēóøÜĔêšéĉî ïøĉđüèïšćîíćøðúĉü ïšćîìŠčÜ÷ćüîčš÷ ĒúąĀîšćĂïê.ðśćĒÖŠïŠĂĀĉî ĂĞćđõĂìčŠÜĀüšć ÝĆÜĀüĆéÿêĎú ēé÷Ĕßš
üĉíÖĊ ćøÿĞćøüÝüĆéÿõćóêšćîìćîĕôôŜćĒïï 2 öĉêĉĒúąüĆééšü÷ÿĆââćèđøéćøŤ ÖĞćĀîéĒîüÿĞćøüÝÖćøüĆéÙŠćÿõćó
êćš îìćîĕôôŜć 20 Ēîü øüöøą÷ąìćÜìĆĚÜÿîĚĉ 6,430 đöêø ĒîüÿćĞ øüÝéüš ÷ÿâĆ âćèđøéćøŤ 2 Ēîü øüöøą÷ąìćÜ
300 đöêø ñúÖćøÿĞćøüÝÿćöćøëĒïŠÜúĆÖþèąíøèĊüĉì÷ćĔêšéĉîðøąÖĂïéšü÷ßĆĚîĀĉîðĎîàęċÜđðŨîĀĉîåćîöĊÙŠćÿõćó
êšćîìćîĕôôŜćöćÖÖüŠć 150 ēĂĀŤöđöêø ðŗéìĆïéšü÷ßĚĆîêąÖĂîéĉîđĀîĊ÷üðîìøć÷ öĊÙŠćÿõćóêšćîìćîĕôôŜć
øąĀüŠćÜ 10-30 ēĂĀŤöđöêø ĒúąßĆĚîñĉüéĉîđðŨîßĆĚîÖøüéĒúąýĉúćĒúÜìęĊöĊÙŠćÿõćóêšćîìćîĕôôŜćøąĀüŠćÜ 100-
200 ēĂĀŤöđöêø ÝćÖÖćøĒðúÙüćöĀöć÷ךĂöĎúÖćøÿĞćøüÝóï 1)ïøĉđüèĀĉîðĎîìęĊöĊøĂ÷ĒêÖĒúąÿćöćøëóĆçîć
Öúć÷đðŨîēóøÜĕéšĔîĒîüđÖČĂïđĀîČĂ-Ĕêš ðøćÖãìćÜìĉýêąüĆîĂĂÖ×ĂÜóČĚîìęĊïšćîíćøðúĉü 2)ĒîüÙüćöêŠĂđîČęĂÜ
×ĂÜēóøÜĔêéš ĉîìýĉ đĀîĂČ -Ĕêš ïøđĉ üèÿüî÷ćÜóćøć ĒúąïøĉđüèĔÖúšëîîúćé÷ćÜ óČĚîìęĊïšćîìŠčÜ÷ćüîčš÷ Ēúą 3)óï
ĒîüøĂ÷ĒêÖ×ĂÜßĚĆîĀĉîðĎîìęĊĂćÝóĆçîćđðŨîēóøÜĕéšđóęĉöđêĉöïøĉđüèĀîšć Ăïê.ðśćĒÖŠïŠĂĀĉî ìĚĆÜîĚĊÝćÖñúÖćø
ÿĞćøüÝ ÿćöćøëÿøčðĔîđïĚČĂÜêšîĕéšüŠćĒîüøĂ÷ĒêÖĀøČĂēóøÜĔêšéĉîĀúĆÖĔîóĚČîìęĊĂ÷ŠĎĔîĒîüđÖČĂïđĀîČĂ-Ĕêš àęċÜÙüø
đòćŜ øąüÜĆ ĒúąÜéðúÖĎ ÿÜĉę ÖĂŠ ÿøšćÜđóöĉę đêöĉ ĔîóČĚîìĊéę ĆÜÖúćŠ ü

ÙĞćÿĞćÙĆâ: ÖćøÿĞćøüÝíøèĊôŗÿĉÖÿŤ, ÖćøüĆéÿõćóêšćîìćîĕôôŜćĒïï 2 öĉêĉ, üĉíĊüĆééšü÷ÿĆââćèđøéćøŤ,
Ă.ìÜŠč Āüćš Ý.ÿêúĎ

51 การประชมุ วิชาการ “ธรณไี ทย 2562”, 16-17 กันยายน 2562 ณ โรงแรม เดอะ เบอรเ คลีย ประตูนา้ํ กรงุ เทพมหานคร
êĞćĒĀîŠÜìĊêę ÜĚĆ ĒúąúĆÖþèąõĎöðĉ øąđìýïøĉđüèĀúöč ÷ïč Ă.ìŠčÜĀüšć Ý.ÿêĎú

52

W E
ßĆĚî

ßĚĆ Āĉ
Āĉ øĂ÷

W E
ßĚîĆ

ßĆĚ Āĉ
Āĉ øĂ÷

êüĆ Ă÷ŠćÜñúÖćøÿĞćøüÝÖćøüéĆ ÿõćóêćš îĕôôŜćĒïï 2 öĉêĉ ĒúąÿõćóóĚîČ ìĊęÖćøÿćĞ øüÝ







































72

Öćøðøą÷čÖêĔŤ ßîš üêĆ ÖøøöîćēîđóČęĂÿŠÜđÿøöĉ ÖćøĔßðš øąē÷ßîŤÝćÖìøĆó÷ćÖøíøèĊ
ÿĞćĀøĆïïĞćïéĆ öúóþĉ ìĊęđðîŨ öêĉ øêŠĂÿÜęĉ ĒüéúĂš ö

öÜÙú ÞüĊÝĆîìøŤ, üĆîđóĘâ ĂŠüöĔÝïčâ, øćßîĆ đúýĉ ó÷ÙĆ ÛøêĆ îŤ, îêĉ ĉÖćâÝîŤ òćđÜĉî,
îĉê÷ć ì÷č đüĊ÷Ü, Ēúą ÝøĊ ąüøøè đöĂöąîć

ÖĂÜüđĉ ÙøćąĀŤĒúąêøüÝÿĂïìøĆó÷ćÖøíøèĊ ÖøöìøĆó÷ćÖøíøèĊ
75/10 ë.óøąøćö 6 øćßđìüĊ ÖøÜč đìóöĀćîÙø 10400

ïìÙĆé÷ĂŠ

ÖćøüĉÝ÷Ć îĊĚđðŨîÖćøîĞćîüêĆ Öøøöéćš îîćēîđìÙēîēú÷Ċöćðøą÷čÖêŤĔßšĔîÖćøÿĆÜđÙøćąĀŤêĆüđøŠÜðäĉÖĉøĉ÷ćìćÜ
ĒÿÜĕììćđîĊ÷öĕéĂĂÖĕàéŤĔĀšöĊĂîčõćÙ×îćéîćēîđöêø÷ċéêĉéïîóĚČîñĉüíøèĊüĆêëčÿĞćĀøĆïîĞćĕðĔßš
ïĞćïĆéöúóĉþÝćÖÿĊ÷šĂöñšć ÿćøúąúć÷ĕììćđîĊ÷öĕéĂĂÖĕàéŤĂîčõćÙ×îćéîćēîđöêøÿĆÜđÙøćąĀŤ×Ěċîéšü÷üĉíĊēàú
đÝúðøą÷čÖêŤēé÷ĔßšĂĆêøćÿŠüîêŠĂēöú×ĂÜ Titanium (IV) isopropoxide (TTIP) : Ethanol : Acetic acid :
Triton X-100 : conc. HCl đðŨî 1 : 45 : 4 : 0.5 : 0.1 ēöú êćöúĞćéĆï ÝćÖîĚĆîìĞćÖćøđÙúČĂïÿćøúąúć÷
ìęĊÿĆÜđÙøćąĀŤ×ĚċîúÜïîíøèĊüĆêëčÿĂÜßîĉé ĕéšĒÖŠ ĀĉîðĎî ĒúąĀĉîóĆööĉÿ éšü÷đìÙîĉÙ Spray coating ĒúąđñćìęĊ
ĂčèĀõĎöĉ 500oC đðŨîđüúć 60 îćìĊ (Heating rate 3 oC/min) ñúÖćøýċÖþćēÙøÜÿøšćÜñúċÖ×ĂÜĕììćđîĊ÷ö
ĕéĂĂÖĕàéŤìĊęÿĆÜđÙøćąĀŤ×ċĚîēé÷đìÙîĉÙ X-ray Diffraction (XRD) óïüŠćöĊēÙøÜÿøšćÜñúċÖđðŨîĒïïĂîćđìÿ Ēúą
ÙĞćîüè×îćéñúċÖēé÷Ĕßš ÿöÖćø Scherrer óïüŠćñúċÖĕììćđîĊ÷öĕéĂĂÖĕàéŤìĊęÿĆÜđÙøćąĀŤĕéšöĊ×îćé 16 îćēî
đöêø ñúÖćøýċÖþćÙčèúĆÖþèąóČĚîñĉüìćÜÖć÷õćóĒúąĂÜÙŤðøąÖĂïìćÜđÙöĊ×ĂÜíøèĊüĆêëčìęĊđÙúČĂïéšü÷ĕììć
đîĊ÷öĕéĂĂÖĕàéŤĂîčõćÙ×îćéîćēîđöêøéšü÷đìÙîĉÙ Scanning Electron Microscope – Energy
Dispersive X-ray Spectrometer (SEM-EDX) óïüŠćïøĉđüèóČĚîñĉü×ĂÜíøèĊüĆêëčìĚĆÜÿĂÜßîĉéöĊĂîčõćÙĕììć
đîĊ÷öĕéĂĂÖĕàéŤÖøąÝć÷êĆüĂ÷ŠĎĂ÷ŠćÜÿöĞęćđÿöĂ ñúÖćøìéÿĂïðøąÿĉìíĉõćó×ĂÜĀĉîðĎîĒúąĀĉîóĆööĉÿìęĊđÙúČĂï
éšü÷ĕììćđîĊ÷öĕéĂĂÖĕàéŤĂîčõćÙ×îćéîćēîđöêøĔîÖćø÷ŠĂ÷ÿúć÷ÿĊ÷šĂöñšćøĊĒĂÖìĊôïúĎÙüćöđךöךîđøęĉöêšî
15 mg/L éšü÷ĒÿÜ UVC 20 watt đðŨîđüúć 12 ßö. óïüŠćÙŠćđÞúĊę÷ðøąÿĉìíĉõćóĔîÖćøïĞćïĆéÿĊ÷šĂöñšćøĊĒĂÖ
ìĊôïúĎÙĉéđðŨîøšĂ÷úą 65.84 Ēúą 34.47 êćöúĞćéĆï ÝćÖñúÖćøìéúĂÜĒÿéÜĔĀšđĀĘîüŠćÖćøîĞćîćēîđìÙēîēú÷Ċ
öćðøą÷čÖêŤĔßšøŠüöÖĆïíøèĊüĆêëčìęĊöĊÙčèÿöïĆêĉìćÜÖć÷õćóĒúąìćÜđÙöĊìĊęđĀöćąÿöÿćöćøëđóęĉöÙčèðøąē÷ßîŤ
ĔĀšÖïĆ íøèĊüĆêëčđóČĂę ÖćøĔßšÜćîéćš îêŠćÜėĕéšĂ÷ŠćÜĀúćÖĀúć÷öćÖ÷Üĉę ×îċĚ

õćóĒÿéÜÙčèúĆÖþèąóČîĚ ñüĉ ìćÜÖć÷ĒúąíćêčĂÜÙðŤ øąÖĂï×ĂÜĀĉîðîĎ ēé÷Ĕßđš ìÙîĉÙ SEM-EDX

73 การประชมุ วชิ าการ “ธรณีไทย 2562”, 16-17 กนั ยายน 2562 ณ โรงแรม เดอะ เบอรเ คลีย ประตูนํ้า กรุงเทพมหานคร

õćóĒÿéÜÙčèúĆÖþèąóČĚîñĉüìćÜÖć÷ ÖćøÖøąÝć÷êĆüĒúąðøĉöćèíćêčĂÜÙŤðøąÖĂï×ĂÜĀĉîðĎîđÙúČĂïĕììć
đî÷Ċ öĕéĂĂÖĕàéŤēé÷Ĕßđš ìÙîÙĉ SEM-EDX mapping

õćóĒÿéÜÙèč úÖĆ þèąóČĚîñĉüìćÜÖć÷ĒúąíćêčĂÜÙŤðøąÖĂï×ĂÜĀîĉ óöĆ öĉÿēé÷Ĕßđš ìÙîĉÙ SEM-EDX

74

Öćøðøą÷čÖêŤĔßšĂćÖćý÷ćîĕøÙš î×ĆïÿćĞ ĀøĆïÜćîÿĞćøüÝíøèóĊ ïĉ êĆ õĉ ÷Ć

Ýæč ćöćý ÝîĆ ĒðÜđÜîĉ 1*, üĊøąßćêĉ üĉđüÖüîĉ 1, üÿĉ čìíóĉ ÜýŤ ÙøĊ øĊ êĆ îđÿëĊ÷ø2
üøćõøèŤ Ýêĉ ÿüč øøè2, øąüĊ óöčŠ àĂŠ îÖúîĉę 1 Ēúą ðŗ÷ćõøèŤ Āîĉ ĒÿÜ1

1 ÿŠüîöćêøåćîĒúą×šĂöĎúíøèĊóïĉ êĆ ĉõĆ÷ ÖĂÜíøèüĊ ĉì÷ćÿĉÜę ĒüéúšĂö ÖøöìøĆó÷ćÖøíøèĊ
2 ÿŠüîíøèĊüìĉ ÷ćÿÜĉę ĒüéúšĂöĒúąÖćøđðú÷Ċę îĒðúÜÿõćóõöĎ ĉĂćÖćý

ÖĂÜíøèĊüìĉ ÷ćÿęĉÜĒüéúšĂö ÖøöìøĆó÷ćÖøíøèĊ 75/10 ë. óøąøćö 6 øćßđìüĊ ÖøÜč đìóöĀćîÙø 10400
*Corresponding author: Ýæč ćöćý ÝĆîĒðÜđÜîĉ
e-mail: [email protected]

ïìÙéĆ ÷ĂŠ

ĂćÖćý÷ćîĕøšÙî×Ćï ĀøČĂēéøî (Drone) đðŨîĂćÖćý÷ćîìęĊÿćöćøëïĆÜÙĆïÝćÖøą÷ąĕÖú Ĕî÷čÙĒøÖĔßš
đðŨîđÙøČęĂÜïĉîÿĂéĒîöĕøšÙî×ĆïĔîÜćîìćÜìĀćø ÿĞćĀøĆïÿĞćøüÝóČĚîìęĊĀøČĂðäĉïĆêĉÖćøĒìîîĆÖïĉîĔîóĚČîìęĊđÿęĊ÷Ü
ĂĆîêøć÷ ĒêŠðÝŦ Ýïč îĆ öÖĊ ćøĔßðš øąē÷ßîŤÝćÖĂćÖćý÷ćîĕøšÙî×ĆïìęĊĀúćÖĀúć÷ đߊî ïĆîìċÖõćóöčöÿĎÜ ïĆîìċÖõćó
ÖćøëŠć÷ìĂéÿéêŠćÜė đðŨîóćĀîąĔîÖćø×îÿŠÜđüßõĆèæŤ đðŨîđÙøČęĂÜÞĊéóŠîðčŞ÷ĒúąÿćøđÙöĊĔîÜćîđÖþêøÖøøö
ĒúąÜćîÿćĞ øüÝíøèüĊ ĉì÷ćĒúąíøèóĊ ĉïĆêõĉ Ć÷ đðŨîêšî

ĂćÖćý÷ćîĕøšÙî×ĆïÿćöćøëîĞćöćðøą÷čÖêŤĔßšÖĆïÖćøÿĞćøüÝíøèĊóĉïĆêĉõĆ÷ ĕéšĒÖŠ íøèĊüĉì÷ćĒñŠîéĉîĕĀü
øĂ÷đúČęĂîöĊóúĆÜ éĉîëúŠö ĒúąÖćøđðúęĊ÷îĒðúÜßć÷òũŦÜ ÿĞćĀøĆïÜćîÿĞćøüÝíøèĊüĉì÷ćĒñŠîéĉîĕĀüĒúąøĂ÷đúČęĂî
öĊóúĆÜ ĂćÖćý÷ćîĕøšÙî×ĆïÿćöćøëîĞćöćĔßšĔîÖćøÿĞćøüÝóČĚîìĊę đóČęĂÝĆéìĞćĒñîìĊęúĆÖþèąóČĚîñĉüõĎöĉðøąđìý
đßĉÜđú× đÿšîßĚĆîÙüćöÿĎÜ ĒúąĒñîìęĊõĎöĉðøąđìý×ĂÜóČĚîìĊęýċÖþć ךĂöĎúõćóìĊęĕéšÝćÖÖćøïĉîÿĞćøüÝÝąëĎÖîĞćĕð
ðøąöüúñúéšü÷ēðøĒÖøö Agisoft photoscan đóęČĂÿøšćÜĒñîìęĊúĆÖþèąóČĚîñĉüõĎöĉðøąđìýđßĉÜđú×đÿšîßĆĚîÙüćö
ÿĎÜ ĒúąĒñîìõęĊ Ďöĉðøąđìý×ĂÜóîČĚ ìęýĊ Öċ þć ÿćĞ ĀøĆïÖćøĒðúÙüćöĀöć÷íøèĊÿĆèåćîìĊęïŠÜßĊĚüŠćđðŨîøĂ÷đúČęĂîöĊóúĆÜ
đóĂęČ ÙĆéđúĂČ ÖóîČĚ ìę×Ċ čéøĂŠ ÜÿćĞ øüÝíøèĊüĉì÷ćĒñîŠ éĉîĕĀüĒúąøĂ÷đúČęĂîöóĊ úĆÜ

ÿĞćĀøĆïÖćøýċÖþćéĉîëúŠö ĂćÖćý÷ćîĕøšÙî×ĆïÿćöćøëîĞćöćðøą÷čÖêŤĔßšĔîÖćøÿĞćøüÝøĂ÷ĒêÖ
øŠĂÜøĂ÷éĉîëúŠö ĒúąÖĞćĀîéóĚČîìĊęđÿĊę÷ÜõĆ÷éĉîëúŠö đóČęĂĔßšđðŨîךĂöĎúĔîÖćøÝĆéìĞćöćêøÖćøðŜĂÜÖĆîĒúąïøøđìć
ñúÖøąìïÝćÖéîĉ ëúŠö Ĕîéćš îÖćøÿćĞ øüÝÖćøđðúęĊ÷îĒðúÜßć÷òũŦÜ ĂćÖćý÷ćîĕøšÙî×ĆïÿćöćøëĔßšĔîÖćøêĉéêćö
ÖćøđðúęĊ÷îĒðúÜ×ĂÜĒîüßć÷òŦũÜ đóČęĂđðŨîĒîüìćÜĔîÖćøÖĞćĀîéöćêøÖćøúéñúÖøąìïÝćÖÖćøđðúĊę÷îĒðúÜ
ßć÷òŦũÜĔĀšđĀöćąÿöĔîĒêŠúąóĚČîìęĊ éĆÜîĆĚî ĂćÖćý÷ćîĕøšÙî×ĆïÝċÜđðŨîđìÙēîēú÷ĊìĊęöĊÙüćöìĆîÿöĆ÷ ÿćöćøëîĞćöć
ðøą÷čÖêŤĔßšĒúąđðŨîðøąē÷ßîêŤ ĂŠ ÖćøÿĞćøüÝíøèóĊ ïĉ êĆ õĉ ÷Ć

ÙĞćÿĞćÙĆâ : ĂćÖćý÷ćîĕøšÙî×Ćï íøèĊóĉïĆêĉõĆ÷ øĂ÷đúČęĂîöĊóúĆÜ éĉîëúŠö ÖćøđðúĊę÷îĒðúÜßć÷òũŦÜ
Agisoft photoscan

75 การประชมุ วชิ าการ “ธรณไี ทย 2562”, 16-17 กันยายน 2562 ณ โรงแรม เดอะ เบอรเ คลยี  ประตูนํ้า กรุงเทพมหานคร

ÖćøĒðøÿèĆ åćîđðúČĂÖēúÖߊüÜĂć÷đč ìĂøŤđß÷Ċ øõĊ ćÙêąüîĆ ĂĂÖđÞĊ÷ÜđĀîČĂ×ĂÜĕì÷

Ăõüĉ çč ĉ üøĉ îĆîìîÖúč 1, ðŦââć Ýćøýč øĉ 2ĉ *, Noriko Hasebe3, ĒúąóĉþèčóÜýŤ ÖćâÝîó÷îêŤ4

1 Akita University, Akita, Japan
2 ĀîüŠ ÷üĉÝĆ÷ MESA, Ùèąüĉì÷ćýćÿêøŤ, ÝčāćúÜÖøèŤöĀćüĉì÷ćúĆ÷, Öìö

3 Kanazawa University, Kanazawa, Japan
4 õćÙüßĉ ćíøèüĊ ìĉ ÷ć, Ùèąüìĉ ÷ćýćÿêø,Ť ÝčāćúÜÖøèöŤ Āćüĉì÷ćú÷Ć , Öìö

* [email protected]

ïìÙĆé÷ŠĂ

õćÙêąüĆîĂĂÖđÞĊ÷ÜđĀîĂČ ÙøĂïÙúöč ìøĊę ćïÿÜĎ ēÙøćßàċęÜðøąÖĂïĒĂŠÜêąÖĂîĂĊÿćîìĊęĒïŠÜ÷ŠĂ÷ĂĂÖđðŨî 2

ĒĂŠÜÙČĂ ĒĂŠÜĂčéø-ÿÖúîÙøĒúąĒĂŠÜēÙøćß-Ăčïú ēé÷ĒĂŠÜìĆĚÜÿĂÜĒ÷ÖÝćÖÖĆîéšü÷đìČĂÖđ×ćõĎóćîìĊęüćÜêĆüĔîĒîü

êąüĆîêÖđÞĊ÷ÜđĀîČĂ-êąüĆîĂĂÖđÞĊ÷ÜĔêš ēé÷ìęĊÖćøđÖĉéđðŨîìĊęøćïÿĎÜĒúąđìČĂÖđ×ćõĎóćîÖĞćúĆÜđðŨîÝčéÿîĔÝĔî

ðÝŦ Ýïč Ćî ÖćøýċÖþćîĚĊöĊüĆêëčðøąÿÜÙŤđóęČĂêøüÝĀćÿõćóÖćøĒðøÿĆèåćîìęĊìĞćĔĀšđÖĉéìĊęøćïÿĎÜ ēé÷ĂćýĆ÷ýċÖþćÝćÖ

ìĆĚÜךĂöĎúõćóēìøÿĆöñĆÿĒúą×šĂöĎúíøèĊüĉì÷ćÿîćöĒúąÖćøêøüÝĀćĂć÷čìĞćĔĀšìøćïüŠćßĆĚîĀĉîêąÖĂî×ĂÜìęĊøćï

ÿĎÜēÙøćßöĊÖćøđĂĊ÷ÜđìöćÖÖüŠćðÖêĉĒúąöĊēÙøÜÿøšćÜĂĆîđðŨîñúÝćÖÖćøđðúęĊ÷îúĆÖþèą (deformation) ×ĂÜßĚĆî

Āĉîēé÷đÞóćąÖćøđÖĉéøĂ÷ēÙšÜĔîĀĉî (rock folding) ìĞćĔĀšđÖĉéøĎððøąìčîĒïïêŠćÜė ĒúąÖćøÙéēÙšÜĒúąÖćø

đúČęĂîêĆüðøćÖäßĆéĔîïøĉđüè×ĂïìĊęøćïÿĎÜ ĔîÖćøýċÖþćüĉÝĆ÷îĊĚĕéšđÖĘïêĆüĂ÷ŠćÜĀĉîêąÖĂîÝćÖĀöüéóøąüĉĀćø

ĀöüéõĎÖøąéċÜ ĒúąĀöüéõĎóćî ×ĂÜÖúŠčöĀĉîēÙøćßđóČęĂĀćĂć÷čéšü÷üĉíĊ AFT ñúÖćøýċÖþćóïüŠćêąÖĂîìøć÷ìĊę

ýċÖþćÿŠüîĔĀâŠđðŨîàĆïĂćøŤēÙÿ Ăć÷č×ĂÜĀĉîìøć÷ēðøēêÙüĂøŤêĕàêŤìĊęöĊìĚĆÜìøć÷úąđĂĊ÷éëċÜĀ÷ćïðćîÖúćÜ ñú

ÝćÖÖćøĀćĂć÷čêąÖĂîéšü÷üĉíĊ AFT ĔîÙøĆĚÜîĊĚñîüÖÖĆïÖćøĀćĂć÷čÝćÖÜćîüĉÝĆ÷ĔîĂéĊê ÿćöćøëÖĞćĀîéߊüÜĂć÷č

×ĂÜĀĉîêąÖĂîÖúčŠöēÙøćßĂĂÖđðŨî 4 ߊüÜ ĕéšĒÖŠ ߊüÜ 70±12 úšćîðŘ, ߊüÜ 50±5 úšćîðŘ, ߊüÜ 34±3 úšćîðŘ,

ĒúąßŠüÜ 21±2 úšćîðŘ àęċÜÿŠüîĔĀâŠđðŨîñúÝćÖÖćøĒðøÿĆèåćî (tectonic setting) ìĊęđÖĊę÷üךĂÜÖĆïïøøóê

øĆÜÿøøÙŤĀĉöćúĆ÷ (Himalaya Orogeny) àęċÜÖøąìĞćêŠĂóČĚîìęĊÝîđÖĉéÖćøđðúęĊ÷îúĆÖþèąĔîĀĉîêąÖĂîēÙøćß ēé÷

ߊüÜĒøÖĒÿéÜëċÜđĀêčÖćøèŤíøèĊĒðøÿĆèåćîĒïïïĊïĂĆé(compression tectonics) Ĕîìĉý

êąüĆîĂĂÖđÞĊ÷ÜđĀîČĂ–êąüĆîêÖđÞĊ÷ÜĔêšÝîđÖĉéēÙøÜÿøšćÜðøąìčîõĎóćî (Phu Phan anticlinal structure)

ĒúąÿŠÜñúĔĀšđÖĉéĒĂŠÜêąÖĂî÷ŠĂ÷ēÙøćß-Ăčïú (Khorat-Ubon Subbasin) ìćÜêĂîĔêš ĒúąĂčéø-ÿÖúîÙø

(Udon-Sakon Nakhon Subbasin) ìćÜêĂîđĀîČĂìęĊüćÜêĆüĕðìĉýêąüĆîêÖđÞĊ÷ÜđĀîČĂ-êąüĆîĂĂÖđÞĊ÷ÜĔêš ÿŠüî

ߊüÜìĊęÿĂÜđÖĉéÖćø÷ÖÖøŠĂî (exhumation) øčîĒøÜÝîÿŠÜñúĔĀšĒĂŠÜēÙøćß÷ÖêĆüÖúć÷đðŨîìęĊøćïÿĎÜēÙøćß Ēúą

ĂćÝđðŨîÝčéđøęĉöêšî×ĂÜÖćøđÖĉéđìČĂÖđ×ćõĎóćî ĒúąßŠüÜìęĊÿćöëċÜߊüÜÿčéìšć÷ÿĂéÙúšĂÜÖĆïÖćøđÖĉéøĂ÷đúęČĂîìĚĆÜ

ĒîüøąéĆïĒúąĒîüéÜęĉ àęċÜ×îćéøĂ÷đúęČĂîöÖĊ ćøóçĆ îćìĊøę Ă÷đéöĉ ììęĊ ĞćĔĀđš Öéĉ ÖćøđðúĊę÷îúÖĆ þèąÖúć÷đðŨîìĊęøćïÿĎÜ

ēÙøćßĒúąđìĂČ Öđ×ćõóĎ ćî àÜċę êĂîîĚĊîŠćÝąÿĂéÙúšĂÜÖïĆ Öćø÷čïêĆüĀúĆÖ (major subsidence) ìęĊìĞćĔĀšđÖĉéìĊęøćï

účŠöîĚĞćđÝšćóøą÷ć (Chao Phraya Basin) ĒúąĒĂŠÜøąĀüŠćÜđ×ć (intermontane basin) ĔîðŦÝÝčïĆî ĒúąđÖĉé

Öćø÷ÖêĆü (uplift) ×ĂÜđìČĂÖđ×ćêąîćüýøĊ (Tenasserim Range) Öćø÷ÖêĆüîĊĚ÷ĆÜÙÜéĞćđîĉîöćÝîëċÜðŦÝÝčïĆî

ēé÷öĊĂĆêøćÖćø÷ÖÖøŠĂîēé÷đÞóćąĔîߊüÜĂć÷čđìĂøŤđßĊ÷øĊ êĆĚÜĒêŠ 0.012 öö/ðŘ ÝîëċÜ 0.004 öö/ðŘ (ĀøČĂ 12

ÝîëċÜ 4 đöêø/úćš îðŘ)

ÙĞćÿćĞ ÙâĆ : ìøĊę ćïÿÜĎ , ēÙøćß, ÖćøĒðøÿèĆ åćî, Ăć÷Ýč ćÖ AFT, Öćø÷ÖÖøŠĂî, đìČĂÖđ×ćõóĎ ćî

76

ÖćøóĆçîćđìÙîĉÙĔĀöŠđóęĂČ đóĉęöðøąÿĉìíĉõćóĔîÖćøÿćĞ øüÝĒøŠ
ēé÷Ĕßšêîš ĕöšđðŨîÿČĂę ÖúćÜ (Developing new techniques to
enhance mineral exploration using biological media)

éø.ýĉøóĉ ø ÿÜĎ ðćîđ×ć

ÿćĞ îĆÖÜćîìøóĆ ÷ćÖøíøèđĊ ×ê 3 ÖøöìøĆó÷ćÖøíøèĊ ÙúĂÜ 5 Ă.ÙúĂÜĀúüÜ Ý.ðìöč íćîĊ 12120

ïìÙĆé÷ĂŠ

ÖćøýċÖþćüĉÝĆ÷îĚĊ öĊüĆêëčðøąÿÜÙŤđóČęĂóĆçîćđìÙîĉÙĔĀöŠ ė ĔîÖćøđóĉęöðøąÿĉìíĉõćóÖćøÿĞćøüÝĒøŠēé÷üĉíĊ
ßĊüíøèđĊ ÙöĊ øüŠ öÖïĆ ÖćøĔßêš üĆ Ă÷ŠćÜìćÜÖćøÿĞćøüÝíøèĊđÙöĊĂČęî ė đߊîêĆüĂ÷ŠćÜéĉî ìĚĆÜìęĊĂ÷ĎŠïøĉđüèñĉüéĉîĒúąĔêšñĉü
éĉî đóČĂę Öćøðøą÷čÖêĔŤ îÖćøÿĞćøüÝĀćĒĀúÜŠ ĒøĔŠ îðøąđìýĕì÷êĂŠ ĕð

ēÙøÜÖćøîĚĊĕéšéĞćđîĉîÖćøĔî 2 óČĚîìĊęýċÖþćìęĊöĊÿĉęÜĒüéúšĂöĔîÖćøđÖĉéĒøŠìĂÜÙĞćĒúąúĆÖþèąõĎöĉðøąđìý
êŠćÜÖĆî ĕéšĒÖŠ ĒĀúŠÜĒøŠìĂÜÙĞćïšćîñćăĚĊ ĂĞćđõĂĒöŠÿć÷ ÝĆÜĀüĆéđßĊ÷Üøć÷ ĒúąïøĉđüèÿĞćøüÝĒøŠìĂÜÙĞćïšćîĀĆüîć
ĂĞćđõĂđöĂČ Ü ÝĆÜĀüéĆ đú÷ đóČęĂìęĊÝąêøüÝÿĂïĒúąđðøĊ÷ïđìĊ÷ïýĆÖ÷õćó×ĂÜđìÙîĉÙÖćøÿĞćøüÝĒøŠìęĊÝąóĆçîćĔî 2
óČĚîìęĊìęĊêŠćÜÖĆî îĂÖÝćÖîĚĊ ÖćøðøąöüúñúìćÜÿëĉêĉēé÷üĉíĊ Minimum hypergeometric probability (MHP)
ĒúąüĉíĊ Student’s t test (t test) ĕéšëĎÖĔßšđðŨîđÙøČęĂÜöČĂĔîÖćøüĆéðøąÿĉìíĉõćó (ÙüćöëĎÖêšĂÜĒúąĒöŠî÷Ğć)
×ĂÜđìÙîÙĉ ÖćøÿĞćøüÝĒøìŠ ęĊÝąóçĆ îć×Ěîċ öć

ñúÝćÖÖćøðøąöüúñúìćÜÿëêĉ ĉ ĒúąÖćøÙĞćîüèÙćŠ MHP Ēúą t test óïüŠć êĆüĂ÷ŠćÜóČßÝĞćóüÖĕôÖĆÿ
(Ficus genus) ĔîóĚČîìĊęĒĀúŠÜĒøŠìĂÜÙĞćïšćîñćăĊĚ ÝĆÜĀüĆéđßĊ÷Üøć÷ ĒÿéÜýĆÖ÷õćóĔîÖćøïŠÜßĚĊĒĀúŠÜĒøŠĕéš
đîęČĂÜÝćÖöĊÝĞćîüîíćêčìĊęĒÿéÜÙŠć MHP Ă÷ŠćÜöĊîĆ÷ÿĞćÙĆâĔîÖćøïŠÜßĊĚĒĀúŠÜĒøŠ ēé÷íćêčìĊęĒÿéÜýĆÖ÷õćóđĀúŠćîĚĊ
ĕéšĒÖŠ Dy, Eu, Er, Gd, Lu, Tm, Y, Pd, Ēúą Se Ĕî×èąìĊęêĆüĂ÷ŠćÜéĉîïøĉđüèñĉüéĉî (organic-rich soil) öĊíćêč
ìĊęĒÿéÜýĆÖ÷õćó 2 íćêčÙČĂ Pb Ēúą Zn ĒúąêĆüĂ÷ŠćÜéĉîĔêšñĉüéĉî (subsurface soil) öĊ 2 íćêčđߊîÖĆîÙČĂ K
Ēúą Zn àċęÜíćêčéĆÜÖúŠćüîĚĊîŠćÝąđðŨîíćêčßĊĚîĞć (pathfinder) ĔîÖćøÿĞćøüÝĀćĒĀúŠÜĒøŠìĂÜÙĞćĕéš éĆÜîĚĆîÖćø
ðøą÷čÖêŤĔßšĔîÜćîÿĞćøüÝìęĊĕéšÝćÖÖćøýċÖþćüĉÝĆ÷ĔîđïĚČĂÜêšîîČĚ ÿćöćøëđÖĘïêĆüĂ÷ŠćÜéĉîĒúąüĉđÙøćąĀŤĀćíćêč Zn,
Pb Ēúą K ĒúąêĆüĂ÷ŠćÜĔï×ĂÜóČßÝĞćóüÖĕôÖĆÿ ĀøČĂĔï×ĂÜêšîĕöšĔĀâŠĔîóČĚîìĊę ēé÷üĉđÙøćąĀŤĀćíćêčéĆÜÖúŠćü
ךćÜêšî àċęÜöĊÙüćöîŠćÝąđðŨîÿĎÜìęĊݹߊü÷ĔîÖćøïŠÜßĊĚĒĀúŠÜĒøŠìĂÜÙĞćïøĉđüèîĊĚĕéš ĀøČĂðøą÷čÖêŤĔßšĔîïøĉđüèìęĊöĊ
ÿęĉÜĒüéúšĂöÖćøđÖĉéĒĀúŠÜĒøŠĒúąõĎöĉðøąđìýĔÖúšđÙĊ÷ÜÖĆîĕéš ÿĞćĀøĆïóĚČîìĊęïšćîĀĆüîć ÝĆÜĀüĆéđú÷ êĆüĂ÷ŠćÜéĉî
ïøĉđüèĔêšñĉüéĉîĒÿéÜðøąÿĉìíĉõćóÿĎÜĔîÖćøïŠÜßĚĊĒĀúŠÜĒøŠ đîęČĂÜÝćÖöĊíćêčìęĊĒÿéÜîĆ÷ÿĞćÙĆâìĆĚÜÙŠć MHP Ēúą t
test ĕéšĒÖŠ U Ēúą Se îĂÖÝćÖîĚĊ ÷ĆÜöĊíćêčìęĊĒÿéÜîĆ÷ÿĞćÙĆâ×ĂÜ MHP Ă÷ŠćÜđéĊ÷ü ĕéšĒÖŠ íćêčìĂÜÙĞć (Au), Bi,
Lu, Sn Ēúą Te ĔîêĆüĂ÷ŠćÜéĉîïøĉđüèñĉüéĉî íćêč Bi, Cs, Sn Ēúą Tl ĔîêĆüĂ÷ŠćÜéĉîïøĉđüèĔêšñĉüéĉî Ēúąíćêč
Cu Ēúą Ni ĔîêüĆ Ă÷ŠćÜĔï×ĂÜêîš ÷ćÜóćøć (Hevea brasiliensis Muell.Arg.) éĆÜîĚĆî ĔîÖćøÿĞćøüÝĒøŠïøĉđüèîĚĊ
ÿĞćĀøĆïêĆüĂ÷ŠćÜéĉîÙüøÝąüĉđÙøćąĀŤíćêčéĆÜìęĊÖúŠćüöćĔîóĚČîìęĊïšćîĀĆüîć àċęÜÙćéüŠćîŠćÝąđðŨîêĆüßĊĚîĞć×ĂÜĒĀúŠÜĒøŠ
ìĂÜÙĞć êĆüĂ÷ŠćÜÝćÖĔïêšî÷ćÜóćøćĒÿéÜĔĀšđĀĘîüŠć ĒöšÝąđðŨîêšîĕöšìĊęöîčþ÷ŤðúĎÖ×ċĚîöć ĒêŠ÷ĆÜĒÿéÜýĆÖ÷õćóĔî
ÖćøïŠÜßĚĊĒĀúŠÜĒøŠìĂÜÙĞćĔîóČĚîìęĊîĚĊĕéš êĆüĂ÷ŠćÜĔïêšîđðúšć (Croton persimilis mull.Arg.) ĒÿéÜýĆÖ÷õćóĔî
ÖćøĔßšÿĞćøüÝĒøŠđߊîÖĆî đîČęĂÜÝćÖĒÿéÜÙŠćñĉéðÖêĉđĀîČĂĒĀúŠÜĒøŠ ÿĞćĀøĆïøą÷ąĀŠćÜøąĀüŠćÜÝčéđÖĘïêĆüĂ÷ŠćÜ 100
đöêø ìĊęĔßšĔîÖćøýċÖþćüĉÝĆ÷îĊĚ ðøćÖãüŠćöĊðøąÿĉìíĉõćóđóĊ÷ÜóĂêŠĂÖćøÿĞćøüÝĀćĒĀúŠÜĒøŠĔîïøĉđüèóĚČîìęĊýċÖþć
ìÜĚĆ 2 óĚîČ ìĊéę ÜĆ ÖúćŠ ü

77 การประชมุ วิชาการ “ธรณีไทย 2562”, 16-17 กันยายน 2562 ณ โรงแรม เดอะ เบอรเคลีย ประตนู ้ํา กรุงเทพมหานคร

ñúÝćÖÖćøýċÖþćüĉÝĆ÷îĊĚ îĂÖÝćÖÝąÙšîóïýĆÖ÷õćóìĊęàŠĂîĂ÷ŠĎ×ĂÜêšîĕöšĔîÖćøߊü÷ÿĞćøüÝĀćĒøŠìĂÜÙĞć
Ēúšü ÷ÜĆ ĕéßš Šü÷Āćíćêìč ęĊđðŨîêĆüßĊĚîćĞ ×ĂÜÖćøÿĞćøüÝĒøìŠ ĂÜÙĞćĔîĒêúŠ ąêĆüĂ÷ćŠ ÜìęđĊ ÖïĘ ĔîĒêŠúąóČĚîìęĊýċÖþć
ĂĊÖìĆĚÜ÷ĆÜđðŨîךĂöĎúìĊęìĞćĔĀšßŠü÷úéÙŠćĔߚ݊ć÷ĔîÖćøÿĞćøüÝĒøŠĕéš ēé÷đÞóćąÙŠćüĉđÙøćąĀŤìćÜđÙöĊ ÝćÖ
ðÖêĉìĊęÝąüĉđÙøćąĀŤíćêčđðŨîÝĞćîüîöćÖ ĀøČĂđÖČĂïìčÖêĆüĔîêćøćÜíćêč àċęÜìĞćĔĀšöĊÙŠćĔߚ݊ć÷ĔîÖćø
üĉđÙøćąĀŤêĆüĂ÷ŠćÜÙŠĂîךćÜÿĎÜ ĒêŠñúÝćÖÜćîüĉÝĆ÷îĚĊÝąìĞćĔĀšÿćöćøëđúČĂÖüĉđÙøćąĀŤđÞóćąíćêčìęĊĒÿéÜ
ýÖĆ ÷õćóĔîÖćøïŠÜßĚĊĒĀúŠÜĒøŠĕéšêćößîĉéêĆüĂ÷ŠćÜìęĊĔßšĔîÖćøÿĞćøüÝ àęċÜÝąđðŨîÖćøðøąĀ÷ĆéÙŠćĔߚ݊ć÷Ĕî
ÖćøÿĞćøüÝĒøŠĔîøą÷ą÷ćüĕéš

ÙĞćÿćĞ ÙâĆ : ßĊüíøèĊđÙöĊ íøèđĊ ÙöĊ ÿĞćøüÝĒøŠ êüĆ Ă÷ćŠ ÜóßČ êüĆ Ă÷ŠćÜéĉî ĒĀúŠÜĒøìŠ ĂÜÙćĞ
óĚČîìęĊýċÖþćĒĀúŠÜĒøìŠ ĂÜÙĞćïšćîñćăĊĚ êĞćïúēðÜś Üćö ĂćĞ đõĂĒöŠÿć÷ ÝÜĆ ĀüéĆ đß÷Ċ Üøć÷

78

79 การประชุมวชิ าการ “ธรณีไทย 2562”, 16-17 กันยายน 2562 ณ โรงแรม เดอะ เบอรเ คลยี  ประตนู ้าํ กรงุ เทพมหานคร

ÖćøóĆçîćēðøĒÖøöòÖř ĂïøöíøèüĊ ìĉ ÷ćđóČęĂÖćøĂîčøÖĆ þŤĒĀúÜŠ öøéÖìćÜíøèĊ
ÿĞćĀøĆïđ÷ćüßîēÙøćßÝĊēĂóćøÙŤ

ýõč öĉêø ÝîĆ ìąÙćö

ÿĞćîÖĆ ÜćîìøĆó÷ćÖøíøèĊ đ×ê 2 ÖøöìøĆó÷ćÖøíøèĊ ê.ĔîđöČĂÜ Ă.đöĂČ Ü Ý.×ĂîĒÖîŠ 40000
Corresponding author, E-Mail : [email protected]

ïìÙéĆ ÷ĂŠ

Ăčì÷ćîíøèĊēÙøćßđðŨîĂčì÷ćîíøèĊĔîøąéĆïðøąđìýđöęČĂðŘ ó.ý. 2561 óøšĂöêĚĆÜđðŜćóĆçîć×ĆïđÙúČęĂî
ĕðÿĎŠĂčì÷ćîíøèĊĔîøąéĆïēúÖ ēé÷ĂÜÙŤÖćø÷ĎđîÿēÖÖĞćĀîéêĆüßĊĚüĆéÿĞćÙĆâĔîéšćîÖćøÿČęĂÿćøĒúąĔĀšÖćøýċÖþćìĊę
êĂš ÜöēĊ ðøĒÖøöđÖ÷Ċę üÖĆïÖćøđø÷Ċ îøšĎđóĂČę ÖćøĂîøč ÖĆ þŤĒĀúŠÜöøéÖìćÜìęĊđĀöćąÿöÖĆïÙüćöêšĂÜÖćø×ĂÜđ÷ćüßîĒúą
ÿćöćøëîĞćēðøĒÖøöĕðĔßšĕéšĂ÷ŠćÜöĊðøąÿĉìíĉõćó ÖćøüĉÝĆ÷ÙøĚĆÜîĚĊöĊüĆêëčðøąÿÜÙŤđóęČĂóĆçîćēðøĒÖøöòřÖĂïøö
íøèĊüĉì÷ćđóČęĂÖćøĂîčøĆÖþŤĒĀúŠÜöøéÖìćÜíøèĊÿĞćĀøĆïđ÷ćüßîēÙøćßÝĊēĂóćøŤÙ ĒúąđóęČĂđðøĊ÷ïđìĊ÷ïñúÖćø
đøĊ÷îøšĎ×ĂÜđ÷ćüßîìĊęđøĊ÷îēðøĒÖøöòřÖĂïøö ēé÷ĔßšøĎðĒïïÖćøüĉÝĆ÷ĒúąóĆçîćĀúĆÖÿĎêø (Curriculum
Research & Development) ñúÖćøüĉÝĆ÷ óïüŠć ēðøĒÖøöòřÖĂïøöíøèĊüĉì÷ćđóęČĂÖćøĂîčøĆÖþŤĒĀúŠÜöøéÖ
ìćÜíøèĊÿĞćĀøĆïđ÷ćüßîēÙøćßÝĊēĂóćøŤÙìĊęóĆçîć×ċĚî öĊÙüćöđĀöćąÿöĔîøąéĆïöćÖìĊęÿčé ÖćøìéÿĂïÖŠĂîđøĊ÷î
ĒúąĀúĆÜđøĊ÷î×ĂÜđ÷ćüßîìĊęđøĊ÷îêćöēðøĒÖøöòřÖĂïøööĊÙąĒîîđÞúĊę÷ đìŠćÖĆï 8.83 ÙąĒîî Ēúą 17.40
ÙąĒîî êćöúĞćéĆï ĒúąđöęČĂđðøĊ÷ïđìĊ÷ïÙąĒîîÖŠĂîđøĊ÷îĒúąĀúĆÜđøĊ÷î óïüŠć đ÷ćüßîöĊÙąĒîîĀúĆÜđøĊ÷î
ÿÜĎ ×ċĚîÖüŠćÖĂŠ îÖćøđø÷Ċ îĂ÷ćŠ ÜîĆ÷ÿĞćÙĆâìćÜÿëĉêìĉ ĊęøąéïĆ .05

ÙćĞ ÿćĞ ÙâĆ : ēðøĒÖøöòřÖĂïøö, íøèüĊ ĉì÷ć, ÖćøĂîøč ĆÖþŤ, ĒĀúŠÜöøéÖìćÜíøè,Ċ Ăčì÷ćîíøèēĊ Ùøćß
Keywords: Training Program, Geology, Conservation, Geoheritage, Khorat Geopark