摘要
Based on data collected from a temporary seismic network, in addition to some nearby permanent stations, the authors investigate velocity structure and seismicity in Rongchang gas field, where significant injection-induced seismicity has been identified. The relocated hypocenters show that the 2010 ML 5.1 earthquake sequence was distributed in a small area surrounding major injection wells and clustered mostly along pre-existing faults. Major earthquakes show a focal depth less than 5 km with a dominant depth of ~2 km, a depth of major reservoirs and injection wells. The authors conclude that the 2010 ML 5.1 earthquake sequence might be induced by deep well injection of unwanted water at a depth ~3 km in Rongchang gas field.