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江山-绍兴断裂带在杭州湾延伸的探讨
引用本文:李起彤,毛正毅.江山-绍兴断裂带在杭州湾延伸的探讨[J].地质科学,1986,0(3):211-216.
作者姓名:李起彤  毛正毅
作者单位:江苏省地震局
摘    要:江山-绍兴断裂带斜贯浙江境内,是我国东部一条重要的大地构造分区界线。在浙江陆区部分,江山-绍兴断裂带基本上顺浙赣铁路方向,从江山沿金衢盆地南缘,经乌灶至绍兴平水、富盛。过绍兴后,江山-绍兴断裂带是否继续向杭州湾海域延伸以及如何延伸,则认识分歧。

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收稿时间:1984-09-01
修稿时间:1984-09-01;

INVESTIGATION FOR STRETCH OF JIANGSHAN-SHAOXING FAULT ZONE IN HANGZHOU BAY
Li Qitong,Mao Zhengyi.INVESTIGATION FOR STRETCH OF JIANGSHAN-SHAOXING FAULT ZONE IN HANGZHOU BAY[J].Chinese Journal of Geology,1986,0(3):211-216.
Authors:Li Qitong  Mao Zhengyi
Institution:Seismological Bureau of Jiangsu Province, Nanjing
Abstract:Jiangshan-Shaoxing fault zone is a famous deep fault zone in China. There are various view-points on whether and how it stretches to the Hangzhou Bay. According to the field investigation by the authors in the main islands of Hangzhou Bay and the mountain lands around it, and with reference to some new data of the seismic exploration and the oil-drilling, we obtained some new knowledge, i.e. Jiangshan-Shaoxing fault zone’s strike turns from NE to NEE direction over past Pingshui and Fusheng of Shaoxing City, it continues along Changhe and Yandong in north Cixi county, and finally stretches to East China Sea through Dajushan island of Daishan county.
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