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晋江下游平原—泉州湾地处长乐—诏安断裂带中段,是泉州—汕头地震带内地震活动活跃地段之一。本文初步论述了晋江下游平原—泉州湾形成机制及其与地震的关系。
The lower reaches of the Jinjiang Plain - Quanzhou Bay, is located in the middle part of the Changle-Zhao’an Fault Zone and is one of the active seismic activities in the Quanzhou-Shantou seismic zone. This paper discusses the formation mechanism of Quanzhou Bay, a downstream plain of Jinjiang, and its relationship with earthquakes.