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《Global Geology》 2010-04
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Evolution of Devonian depositional environment in northern Longmenshan tectonic belt

PANG Yan-jun1,ZHANG Ben-jian1,FENG Ren-wei2,WANG Ying-rong1 1.Geological Institute of Northwest Sichuan,Southwest Oil and Gas Field Branch,Jiangyou 643000,Sichuan,China; 2.Department of Resources and Environment,Southwest Petroleum University,Chengdu 610500,China  
The northern Longmenshan tectonic belt located at the egde of Upper Yangtze ancient land in Devonian,inherited the continental shelf slope fault.The depositional environment is controlled by Beichuan and Nanba faults in slope area,and divided into ocean trough,platform edge shoal,open platform and restricted platform areas from west to east at plane.At the end of Silurian,Caledonian movement uplifted the whole Yangtze platform to be ancient land,which supplied massive terrestrial materials to Devonian deposition.In Early Devonian,the crust declined and transgression started.The depositional environment in Ganxi,Pingyipu and Liuhe between the Qingchuan—Nanba fault and Majiaoba—Yanmenba fault is of neritic carbonate rocks and shoreland clastic rocks.In Middle Devonian,the transgression is more intensive with space of more extensive.Tianjingshan ancient uplift is completely covered by sea water and reached to Chaotianyilongdongbei in the Hannan ancient land,while the geomorphic difference between Sichuan and Guizhou ancient lands became smaller with reduced provenance supply,the sediments are mixed mainly by clastic and carbonate rocks.In Late Devonian,the maritime space terminated in the margin of Tianjingshan ancient uplift with the further expansion of transgression.There was only carbonate deposition with no source supply in this area.The evolution of depositional environment of Longmenshan in Devonian mainly experienced the Pingyipu,Ganxi—Guanwushan and Shawozi-Maoba sedimentary cycles.The general pattern is long-time and slow-velocity transgression,and short-time,high-velocity and large-range regression.
【CateGory Index】: P512.2
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