CRETACEOUS SEDIMENTARY FACIES AND THE EVOLUTION IN JIANGHAN BASIN

doi:10.3863/j.issn.1000-2634.2006.06.002

西南石油大学学报(自然科学版) ›› 2006, Vol. 28 ›› Issue (6): 5-8.DOI: 10.3863/j.issn.1000-2634.2006.06.002

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CRETACEOUS SEDIMENTARY FACIES AND THE EVOLUTION IN JIANGHAN BASIN

LI QunGUO Jian-huaZENG FangDUAN Hai-ting

School of Geosciences and Environmental Engineering, Central South University, Changsha Hunan 410083,China

Received:2006-01-04 Revised:1900-01-01 Online:2006-12-20 Published:2006-12-20
Contact: LI Qun

Abstract

Abstract: Based on comprehensive outcrop section measurement, drilling and analysis data, the Cretaceous sequence and its types of sedimentary facies and sedimentary characteristics in Jianghan Basin are systematically studied by using the theories of sequence stratigraphy, sedimentology and loggeology. It is shown that there are two tectonic sequences in Cretaceous affected by Himalayas curtainlike mountain formation movement, Cretaceous is mainly comprised by alluvial fans, braid river, braid river delta and exotic lake facies. In early Cretaceous, alluvial fans and braid rivers were only located in the front part of the fault in the basin because of weak depression and faulting; In late Cretaceous, the basin was totally depressed and faulted because of the aerial expansion, from its margin toward its center, the facies developed from alluvial fans, gradually to braid rivers and braid river deltas or exotic lake, forming a upfine sequence.

Key words: sedimentary facies, facies evolution, filling, Cretaceous, Jianghan Basin

CLC Number:

ＴＥ121

LI Qun GUO Jian-hua ZENG Fang DUAN Hai-ting. CRETACEOUS SEDIMENTARY FACIES AND THE EVOLUTION IN JIANGHAN BASIN[J]. 西南石油大学学报(自然科学版), 2006, 28(6): 5-8.

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CRETACEOUS SEDIMENTARY FACIES AND THE EVOLUTION IN JIANGHAN BASIN

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