Estimation of in-situ stress field surrounding the Namcha Barwa region and discussion on the tectonic stability

The Namjag Barwa syntaxis is in the eastern Himalayan syntaxis area with the most intensive neotectonic activity. There are many late Quaternary active fault belts and strong seismicities. The tectonic stability of these active fault belts, such as the Jiali, Dongjiu-Milin, and Motuo fault belts, ma...

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Main Authors: FENG Chengjun, LI Bin, LI Hui, ZHOU Minghui, ZHANG Peng, ZHU Siyu, REN Yazhe, QI Bangshen, WANG Miaomiao, TAN Chengxuan, CHEN Qunce
Format: Article
Language:zho
Published: Institute of Geomechanics, Chinese Academy of Geological Sciences 2022-12-01
Series:Dizhi lixue xuebao
Subjects:
Online Access:https://journal.geomech.ac.cn//article/doi/10.12090/j.issn.1006-6616.20222820
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author FENG Chengjun
LI Bin
LI Hui
ZHOU Minghui
ZHANG Peng
ZHU Siyu
REN Yazhe
QI Bangshen
WANG Miaomiao
TAN Chengxuan
CHEN Qunce
author_facet FENG Chengjun
LI Bin
LI Hui
ZHOU Minghui
ZHANG Peng
ZHU Siyu
REN Yazhe
QI Bangshen
WANG Miaomiao
TAN Chengxuan
CHEN Qunce
author_sort FENG Chengjun
collection DOAJ
description The Namjag Barwa syntaxis is in the eastern Himalayan syntaxis area with the most intensive neotectonic activity. There are many late Quaternary active fault belts and strong seismicities. The tectonic stability of these active fault belts, such as the Jiali, Dongjiu-Milin, and Motuo fault belts, may influence the project's construction. In-situ stress is a critical parameter for estimating regional tectonic stability. Currently, there is a lack of abundant in-situ stress results about the Namjag Barwa syntaxis. It is challenging to assess geological safety risks for major projects. Based on focal mechanism solutions, the paper reveals the orientation of the maximum principal stress surrounding the Namjag Barwa syntaxis using the stress tensor inversion method. According to the critical condition of fault instability, the magnitudes of principal stresses around the Namjag Barwa syntaxis are also estimated by combining the inversion of the stress shape ratio and the frictional coefficient. The results indicate that the maximum principal stress direction in the Namjag Barwa syntaxis area is NE-NNE. The maximum and minimum horizontal principal stresses increase linearly with depth at a gradient of 0.032~0.0355 MPa/m and 0.0227~0.0236 MPa/m, respectively. Heterogeneous features of the in-situ stress field still exist. Generally, the results estimated in this study are in good concordance with the in-situ stress measurements. They can provide reliable in-situ stress parameters for evaluating the tectonic stability in the Namcha Barwa region.
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spelling doaj.art-4a2722823c1448b093075e770a51e9202023-02-14T01:15:04ZzhoInstitute of Geomechanics, Chinese Academy of Geological SciencesDizhi lixue xuebao1006-66162022-12-0128691993710.12090/j.issn.1006-6616.20222820dzlxxb-28-6-919Estimation of in-situ stress field surrounding the Namcha Barwa region and discussion on the tectonic stabilityFENG ChengjunLI BinLI Hui0ZHOU Minghui1ZHANG PengZHU SiyuREN YazheQI BangshenWANG Miaomiao2TAN ChengxuanCHEN QunceChina Geological Survey, Beijing 100037, ChinaHeze Earthquake Monitoring Center Station, Shandong Earthquake Agency, Heze 274020, Shandong, ChinaChang'an University, Xi'an 710064, Shaanxi, ChinaThe Namjag Barwa syntaxis is in the eastern Himalayan syntaxis area with the most intensive neotectonic activity. There are many late Quaternary active fault belts and strong seismicities. The tectonic stability of these active fault belts, such as the Jiali, Dongjiu-Milin, and Motuo fault belts, may influence the project's construction. In-situ stress is a critical parameter for estimating regional tectonic stability. Currently, there is a lack of abundant in-situ stress results about the Namjag Barwa syntaxis. It is challenging to assess geological safety risks for major projects. Based on focal mechanism solutions, the paper reveals the orientation of the maximum principal stress surrounding the Namjag Barwa syntaxis using the stress tensor inversion method. According to the critical condition of fault instability, the magnitudes of principal stresses around the Namjag Barwa syntaxis are also estimated by combining the inversion of the stress shape ratio and the frictional coefficient. The results indicate that the maximum principal stress direction in the Namjag Barwa syntaxis area is NE-NNE. The maximum and minimum horizontal principal stresses increase linearly with depth at a gradient of 0.032~0.0355 MPa/m and 0.0227~0.0236 MPa/m, respectively. Heterogeneous features of the in-situ stress field still exist. Generally, the results estimated in this study are in good concordance with the in-situ stress measurements. They can provide reliable in-situ stress parameters for evaluating the tectonic stability in the Namcha Barwa region.https://journal.geomech.ac.cn//article/doi/10.12090/j.issn.1006-6616.20222820namcha barwain-situ stressfocal mechanics solutionstectonic stability
spellingShingle FENG Chengjun
LI Bin
LI Hui
ZHOU Minghui
ZHANG Peng
ZHU Siyu
REN Yazhe
QI Bangshen
WANG Miaomiao
TAN Chengxuan
CHEN Qunce
Estimation of in-situ stress field surrounding the Namcha Barwa region and discussion on the tectonic stability
Dizhi lixue xuebao
namcha barwa
in-situ stress
focal mechanics solutions
tectonic stability
title Estimation of in-situ stress field surrounding the Namcha Barwa region and discussion on the tectonic stability
title_full Estimation of in-situ stress field surrounding the Namcha Barwa region and discussion on the tectonic stability
title_fullStr Estimation of in-situ stress field surrounding the Namcha Barwa region and discussion on the tectonic stability
title_full_unstemmed Estimation of in-situ stress field surrounding the Namcha Barwa region and discussion on the tectonic stability
title_short Estimation of in-situ stress field surrounding the Namcha Barwa region and discussion on the tectonic stability
title_sort estimation of in situ stress field surrounding the namcha barwa region and discussion on the tectonic stability
topic namcha barwa
in-situ stress
focal mechanics solutions
tectonic stability
url https://journal.geomech.ac.cn//article/doi/10.12090/j.issn.1006-6616.20222820
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