南华北地区中新生代盆地演化

doi:10.11743/ogg20050220

Abstract

Abstract:

The Late Jurassic-Early Cretaceous volcanic rocks in Dabie orogenic belt are alkali rocks with high potassium content. The corresponding tectonic setting was not a subduction zone, but had certain relationship to plate subduction. The Tancheng-Lujiang fracture zone was characterized by its intenso-wrench or dextral strike-slip movement during Late Jurassic-Early Cretaceous. The Meso-Cenozoic basins in southern North China have significant differences, due to their specific tectonic settings. Taking Pingyu-Bangbu uplift as a boundary, the southern basins, located in the thrust front of Dabie orogenic belt, such as Hefei-Xinyang basin, are triple overlapping basins, which are composed of foreland basin prototype as a result of compressional orogenesis, strike-slip basin prototype as a result of tenso-wrench movement, and extensional counter-inclined normal fault and strike-slip faulted basin prototype. While the northern basins, located in relatively stable landmass, are multiple overlapping basins, which are composed of compressional foreland basin-intracontinental depression prototype, strike-slip basin prototype, depression,transtensional and faulted basin prototype as a result of weak compression, and depression basin prototype as a result of mass subsidence.

Key words: basin prototype, superimposition, Dabie orogenic belt, Tancheng-Lujiang fracture zone, southern North China

CLC Number:

TE111.1

Huang Zeguang, Gao Changlin, Ji Rangshou. Analysis of evolution of Meso-Cenozoic basins in southern North China[J]. Oil & Gas Geology, 2005, 26(2): 252-256.

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Analysis of evolution of Meso-Cenozoic basins in southern North China

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