Near-surface geophysical investigation in Mae On, Chiang Mai, Thailand

The objective of this study is to map a sedimentary layer overlying volcanic basement in Mae On area, Chiang Mai, Thailand. Seismic reflection, multichannel analysis of surface waves and electrical resistivity surveys were conducted to provide additional supporting information in the shallow part...

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Main Authors: Siriporn Chaisri, Srivipa Lerkrattanawaree, Niti Mankhemthong, Suwimon Udphuay, Mingkhwan Kruachanta
Format: Article
Language:English
Published: Prince of Songkla University 2020-12-01
Series:Songklanakarin Journal of Science and Technology (SJST)
Subjects:
Online Access:https://rdo.psu.ac.th/sjstweb/journal/42-6/21.pdf
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spelling doaj-0ee0457d85494cefbddfa0f7fae0fa642020-11-25T03:28:48ZengPrince of Songkla UniversitySongklanakarin Journal of Science and Technology (SJST)0125-33952020-12-014261326133310.14456/sjst-psu.2020.172Near-surface geophysical investigation in Mae On, Chiang Mai, ThailandSiriporn Chaisri0Srivipa Lerkrattanawaree1Niti Mankhemthong2Suwimon Udphuay3Mingkhwan Kruachanta4Department of Physics and Materials Science, Faculty of Science, Chiang Mai University, Mueang, Chiang Mai, 50200 ThailandDepartment of Geological Sciences, Faculty of Science, Chiang Mai University, Mueang, Chiang Mai, 50200 ThailandDepartment of Geological Sciences, Faculty of Science, Chiang Mai University, Mueang, Chiang Mai, 50200 ThailandDepartment of Geological Sciences, Faculty of Science, Chiang Mai University, Mueang, Chiang Mai, 50200 ThailandDepartment of Geological Sciences, Faculty of Science, Chiang Mai University, Mueang, Chiang Mai, 50200 ThailandThe objective of this study is to map a sedimentary layer overlying volcanic basement in Mae On area, Chiang Mai, Thailand. Seismic reflection, multichannel analysis of surface waves and electrical resistivity surveys were conducted to provide additional supporting information in the shallow part of subsurface geometry. The deeper part information is evaluated from the previous magnetic and gravity anomaly maps. The interpretation from seismic reflection is used to constrain gravity forward modeling to obtain a pseudo-geological model. The final model presents that there are a thin Quaternary sediment layer with low electrical resistivity and seismic velocity, overlies volcanic basement with high electrical resistivity and high seismic velocities. The volcanic basement can be recognized as a heterogeneous body with horizontally characteristic layers of volcanic flows based on seismic reflection profiles. The volcanic basement underneath the sediment layer shows a high anomaly on gravity and magnetic maps.https://rdo.psu.ac.th/sjstweb/journal/42-6/21.pdfmae onseismic reflectionmaswelectrical resistivitygravity model
collection DOAJ
language English
format Article
sources DOAJ
author Siriporn Chaisri
Srivipa Lerkrattanawaree
Niti Mankhemthong
Suwimon Udphuay
Mingkhwan Kruachanta
spellingShingle Siriporn Chaisri
Srivipa Lerkrattanawaree
Niti Mankhemthong
Suwimon Udphuay
Mingkhwan Kruachanta
Near-surface geophysical investigation in Mae On, Chiang Mai, Thailand
Songklanakarin Journal of Science and Technology (SJST)
mae on
seismic reflection
masw
electrical resistivity
gravity model
author_facet Siriporn Chaisri
Srivipa Lerkrattanawaree
Niti Mankhemthong
Suwimon Udphuay
Mingkhwan Kruachanta
author_sort Siriporn Chaisri
title Near-surface geophysical investigation in Mae On, Chiang Mai, Thailand
title_short Near-surface geophysical investigation in Mae On, Chiang Mai, Thailand
title_full Near-surface geophysical investigation in Mae On, Chiang Mai, Thailand
title_fullStr Near-surface geophysical investigation in Mae On, Chiang Mai, Thailand
title_full_unstemmed Near-surface geophysical investigation in Mae On, Chiang Mai, Thailand
title_sort near-surface geophysical investigation in mae on, chiang mai, thailand
publisher Prince of Songkla University
series Songklanakarin Journal of Science and Technology (SJST)
issn 0125-3395
publishDate 2020-12-01
description The objective of this study is to map a sedimentary layer overlying volcanic basement in Mae On area, Chiang Mai, Thailand. Seismic reflection, multichannel analysis of surface waves and electrical resistivity surveys were conducted to provide additional supporting information in the shallow part of subsurface geometry. The deeper part information is evaluated from the previous magnetic and gravity anomaly maps. The interpretation from seismic reflection is used to constrain gravity forward modeling to obtain a pseudo-geological model. The final model presents that there are a thin Quaternary sediment layer with low electrical resistivity and seismic velocity, overlies volcanic basement with high electrical resistivity and high seismic velocities. The volcanic basement can be recognized as a heterogeneous body with horizontally characteristic layers of volcanic flows based on seismic reflection profiles. The volcanic basement underneath the sediment layer shows a high anomaly on gravity and magnetic maps.
topic mae on
seismic reflection
masw
electrical resistivity
gravity model
url https://rdo.psu.ac.th/sjstweb/journal/42-6/21.pdf
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