华北板块东南缘原型沉积盆地类型与构造演化

doi:10.11743/ogg20060216

Abstract

Abstract:

The types of original sedimentary basins on southeastern margin of North China plate were controlled by tectonic evolution. North China and Yangtze plates experienced the changes from"divergence"to"convergence"in Paleozoic-Middle Triassic. The southeastern margin of North China plate correspondingly experienced the changes from passive continental margin in Sinian-Middle Ordovician(Z-O₂)to uplifting and denudation in Late Ordovician to Early Carboniferous (O₃-C₁). During late Early Carboniferous-Middle Triassic (C₂-P₂), foreland flysch depositional basins were formed on the continental margin due to convergence of plates. During Late Triassic ?Early Jurassic, Qinling-Dabie orogenic zone was formed through the collision of the two plates, coupled with the formation of molasses sedimentary basins. During Middle Jurassic-Early Cretaceous, the margin of the orogenic belt detached while the epiorogenic subsidence occurred within the orogenic belt, resulting in a complicated structural pattern with outstretching on the trailing edge and thrusting on the leading dege. Outstretched fault-depression and down-warped basins were formed later under the control of the activities of Palaeo-Pacific plate and Pacific plate.

Key words: foreland flysch sedimentary basin, foreland molasses sedimentary basin, detached structure, type of original basin, North China plate

CLC Number:

TE111.1

Yu Hezhong, Han Shouhua, Xie Jinlong, Guo Qingxin, Wu Jinyun. Types of original sedimentary basins and tectonic evolution on southeastern margin of North China plate[J]. Oil & Gas Geology, 2006, 27(2): 244-252.

References

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Types of original sedimentary basins and tectonic evolution on southeastern margin of North China plate

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