摘要
研究了福建沿海自晚更新世以来控制主要断陷盆地、平原和海湾的断裂活动性状，认为这些构造在所讨论的时段内具有强烈的张性活动，而发生于区内的地震与这些构造的近期张性活动有关。
The fault active behavior of downfaulted basin, plain and bay since the Epileistocene in Fujian province are studied. It is considered that these structures have the intense tension activity in the discussed time interval, and with which the earthquakes occurred in the region are related.
出处
《地壳形变与地震》
CSCD
1998年第4期55-61,共7页
Crustal Deformation and Earthquake
