摘要
根据晚新生代以来沉积建造、沉积环境、岩浆活动、岸线变迁、地貌及现代地震等资料判断,太仓—奉贤北西向断裂带是上海及邻近地区一条重要的活动性断裂构造带。
According to the sedimentary formation, sedimentary environment, magmatic activities, changes of shoreline, geomorphology and modern earthquakes etc. since the late Neozoic, the Nw—fault zone of Taicang-Fengxian is an important active fracture in Shanghai and its neighbourhood.
关键词
断裂带
地震
地质意义
Gradient zone of gravity anomaly, anomaly zone of air magnetic survey, buried depth of bedrock, mobile tectonic zone
