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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Prince of Songkla University
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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 |
work_keys_str_mv |
AT siripornchaisri nearsurfacegeophysicalinvestigationinmaeonchiangmaithailand AT srivipalerkrattanawaree nearsurfacegeophysicalinvestigationinmaeonchiangmaithailand AT nitimankhemthong nearsurfacegeophysicalinvestigationinmaeonchiangmaithailand AT suwimonudphuay nearsurfacegeophysicalinvestigationinmaeonchiangmaithailand AT mingkhwankruachanta nearsurfacegeophysicalinvestigationinmaeonchiangmaithailand |
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1724582748560031744 |