Months‐Long Crustal Deformation Driven by Aseismic Slips and Pore Pressure Transients Triggered by Local and Regional Earthquakes

Months‐Long Crustal Deformation Driven by Aseismic Slips and Pore Pressure Transients Triggered by Local and Regional Earthquakes
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数月——由局部和区域地震引发的抗震滑移和孔隙压力瞬变驱动的长期地壳变形

DOI:
10.1029/2021gl095148
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发表时间:
2021-08
影响因子:
5.2
通讯作者:
Lianxing Wen
Lianxing Wen
中科院分区:
地球科学1区
文献类型:
--
作者:
Zhou Lu;Lianxing Wen

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2010-2017年期间,在加州安扎附近的钻孔应变仪中观察到了三次Mw 4.5+地方地震和一次Mw 7.2区域地震后的强烈应变和孔隙压力变化。应变变化在地震后立即出现,持续时间为40-100
Strong strain and pore pressure changes are observed after three Mw 4.5+ local and one Mw 7.2 regional earthquake during 2010–2017 in borehole strainmeters near Anza, California. The strain change emerges immediately after the earthquakes and lasts 40–100
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