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.
机构:
Peking Univ, Minist Educ, Key Lab Orogen Belts & Crustal Evolut, Beijing 100871, Peoples R China
China Univ Geosci, Sch Earth Sci & Resources, Beijing 100083, Peoples R ChinaPeking Univ, Minist Educ, Key Lab Orogen Belts & Crustal Evolut, Beijing 100871, Peoples R China
Wang, Wei
Zhang, Wanyi
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机构:
China Geol Survey, Res Dev Ctr, Beijing 100037, Peoples R ChinaPeking Univ, Minist Educ, Key Lab Orogen Belts & Crustal Evolut, Beijing 100871, Peoples R China
机构:
State Key Laboratory of Continental Dynamics, Department of Geology, Northwest UniversityState Key Laboratory of Continental Dynamics, Department of Geology, Northwest University
QIN Jiangfeng
LAI Shaocong
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机构:
State Key Laboratory of Continental Dynamics, Department of Geology, Northwest UniversityState Key Laboratory of Continental Dynamics, Department of Geology, Northwest University
LAI Shaocong
LONG Xiaoping
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机构:
State Key Laboratory of Continental Dynamics, Department of Geology, Northwest UniversityState Key Laboratory of Continental Dynamics, Department of Geology, Northwest University