词条 | Graviquake |
释义 |
A graviquake is an earthquake occurring in an extensional tectonic setting, where the gravitational energy stored during the interseismic period is delivered by the collapse of a brittle upper crustal volume, slipping along a normal fault and generating the double couple recorded in the moment tensor solution.[1] References1. ^{{cite web|url=https://www.nature.com/articles/srep12110 |title=Normal fault earthquakes or graviquakes | Scientific Reports |website=Nature.com |date= |accessdate=2017-07-08}} {{Earthquake-stub}} 3 : Seismology|Scientific terminology|Gravitation |
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