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Stephen A Miller1, Cristiano Collettini, Lauro Chiaraluce
1Institute of Geophysics, Swiss Federal Institute of Technology (ETH), 8093 Zürich, Switzerland. steve.miller@erdw.ethz.ch
1997年意大利的一次地震序列是由深层二氧化碳 (CO2) 流体压力脉冲驱动的. 在主震中释放的脉冲引发了数千次余震,挑战了传统的地震模型.
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