Discovery of late Paleozoic fossils in tectonic blocks of the Dabao Formation in the South Qinling Orogenic Belt and their significance

被引:6
|
作者
Wang Tao [1 ]
Wang ZongQi [2 ]
Yan Zhen [1 ]
Yan QuanRen [1 ]
Zhang YingLi [2 ]
Xiang ZhongJin [1 ]
机构
[1] Chinese Acad Geol Sci, Inst Geol, Beijing 100037, Peoples R China
[2] Chinese Acad Geol Sci, Inst Mineral Resources, Beijing 100037, Peoples R China
基金
中国国家自然科学基金;
关键词
South Qinling Orogenic Belt; Dabao Formation; Middle Devonian corals and conodonts;
D O I
10.1007/s11430-011-4183-4
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The Dabao Formation in the South Qinling Orogenic Belt was previously regarded as Ordovician in age and consists of clastic matrix and blocks of siltstone, limestone, chert, and volcanic rocks. However, some Middle Devonian corals, conodonts, and other fossil fragments within the limestone blocks were discovered in recent field investigations, indicating that the Dabao Formation was formed during late Paleozoic. Combined with other regional geological data, the Dabao Formation in the Southern Qinling Orogenic Belt is considered to be a late Paleozoic or early Mesozoic accretionary complex.
引用
收藏
页码:975 / 981
页数:7
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