• 责任者：Yao Qi (Institute of Geology ; China Earthquake Administration ; Beijing 100029 ; China) ; Zhang Wei
• 刊名：Geotectonica et Metallogenia
• 出版年：2010
• 卷期：34（1）
• 关键词：断裂 ; fractures ; 活动构造 ; active tectonics ; 浙江 ; Zhejiang Province
• 页码：p.40-47
• 图表：4 illus., 22 refs.
• 分类号：0300
• issnNo：ISSN1001-1552
• isbnNo：CN44-1595/P

The Changxing-Fenghua Fault (CFF) is a regional fault trending in NW-SE, which diagonally goes across the Hangzhou Bay region. The authors analyzed the distribution and activity of the CFF in the Mesozoic and Cenozoic according to the TM remote sensing image, aeromagnetic anomaly map, Bouguer gravitational anomaly map and artificial seismic profiles. Therefore, the CFF is a tenso-shear fault and belongs to the NW-trending active fault zones of the eastern Chinese continent in the Mesozoic and Cenozoic.