川东南地区志留系小河坝组砂岩特征及物源分析

Abstract

Abstract: Based on clastic compositions, debris types, heavy minerals,geochemistry (REE, trace elements)and paleocurrent of sandstone, the authors analyze source direction, rock type and tectonic settings of the source region of Xiaoheba Formation of southeastern Sichuan Province.The provenance derives from basic rocks, ultrabasic rocks, basic-intermediate effusive rocks of Neoproterozoic Banxi Group of the west wing of Xuefengshan uplift in east of basin. Tectonic background of source area includes active continental margin, continentalarc-islandsand passive continental margin.Source rock is mainly composed of older recycled sedimentary deposits of uplifted basement rock.South China plate and Yangtze plate spliced by slowly creeping of South China plate toward the Yangtze plate in the Early Silurian Xiaoheba Period,and resulted in slow uplift of whole Yangtze plate,meanwhile, the depocenter migrated continuously to the northwest,thus formed the cycles of supply source inresearch area.

Key words: southeastern Sichuan Province, Silurian, Xiaoheba Formation, provenance analysis, sandstone, geochemistry

CLC Number:

P588.2

Zhu Zhi-jun,Chen Hong-de. Sandstone Characteristics and Provenance Analysis of the Sandstone in Silurian Xiaoheba Formation in Southeastern Sichuan Province, China[J].Journal of Jilin University(Earth Science Edition), 2012, 42(6): 1590-1600.

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Sandstone Characteristics and Provenance Analysis of the Sandstone in Silurian Xiaoheba Formation in Southeastern Sichuan Province, China

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