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论浙江东部早白垩世中期断陷事件和断陷岩套
引用本文:汪迎平,丁保良,李耀西,钱迈平,姜杨.论浙江东部早白垩世中期断陷事件和断陷岩套[J].地质学刊,2007,31(3):176-179.
作者姓名:汪迎平  丁保良  李耀西  钱迈平  姜杨
作者单位:南京地质矿产研究所 江苏南京210016
基金项目:中国地质调查局地质调查项目
摘    要:早白垩世中期中国东南部发生过一次断陷事件,并形成一事件地层单元——断陷岩套。叙述了断陷岩套的形成机理、特征和类型,并利用事件地层单元同时性原理,论证了建组剖面"塘上组"的层位与永康群下部馆头组相同,而非高居永康群之上的"新构造亚层";也论证了嵊县三界一带的所谓"大爽组二段"应为馆头组。这两个断陷岩套中所含生物群证实:事件地层学原理所得的关于其层位与时代的结论是正确的。

关 键 词:早白垩世  事件地层学  断陷岩套  馆头组  塘上组  浙江东部
文章编号:1003-6474(2007)03-0176-04
收稿时间:2007-07-27
修稿时间:2007年7月27日

Fault subsidence event and fault subsidence suite in middle period of early Cretaceous epoch in east Zhejiang
WANG Ying-ping,DING Bao-liang,LI Yao-xi,QIAN Mai-ping,JIANG Yang.Fault subsidence event and fault subsidence suite in middle period of early Cretaceous epoch in east Zhejiang[J].Jiangsu Geology,2007,31(3):176-179.
Authors:WANG Ying-ping  DING Bao-liang  LI Yao-xi  QIAN Mai-ping  JIANG Yang
Institution:Nanjing Institute of Geology and Mineral Resources, Nanjing 210016,China
Abstract:A fault subsidence event was happened in southeast China during the middle period in early Cretaceous,while an event stratiqraphic unit-fault subsidence suite was formed.The genetic mechanism,features and types of the fault subsidence suite are depicted in the text,and the principles of the isochroneity of the event stratiqraphic unit were used to prove the horizon of Tangshang Formation in its type section located at Shuinan of Tiantai basin should be the same with that of Gantou Formation of the lower part of Yongkang Group,but not a new tectonic subbed which was overburdened upon Yongkang Group,and the so called.The second member of Dashuang Formation located near Sanjie of Shengzhou should also be Guantou Formation.The information obtained from the above mentioned fault subsidence suites suggested and concluded that the horizon and age of the fault subsidence suite based on the principle of even stratigraphy were correct.
Keywords:Early Cretaceous Epoch  Event stratigraphy  Fault subsidence suite  Guantou Formation  Tangshang Formation  East Zhejiang
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