Bedrock temperature as a potential method for monitoring change in crustal stress: Theory, in situ measurement, and a case history
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- 作者：Shunyun Chen ; chenshy@ies.ac.cn" class="auth_mail" title="E-mail the corresponding author ; Peixun Liu ; Liqiang Liu ; Jin Ma
- 关键词：Stress temperature ; Conduction temperature ; Crustal stress ; Lushan earthquake ; Seismic activity ; Qinghai-Tibet Plateau
- 刊名：Journal of Asian Earth Sciences
- 出版年：2016
- 出版时间：1 June 2016
- 年：2016
- 卷：123
- 期：Complete
- 页码：22-33
- 全文大小：2830 K
文摘
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Bedrock temperature can be used as an indicator of the state of crustal stress.
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Synchronous response distinguishes stress temperature from conduction temperature.
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Data of the Lushan earthquake verify our method of obtaining crustal stress state.
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Change in stress temperature appears before increases in seismic activities.