Superposed Basin Types and Exploration Realms in Mesozoic Yingen-Ejina Basins in the West of Nei Mongol

CHEN Qi-lin; ZHOU Hong-rui; WEI Ping-sheng; YANG Zhan-long; BAI Yun-lai

Northwestern Geology > 2006 > 39(1): 89-96.

CHEN Qi-lin, ZHOU Hong-rui, WEI Ping-sheng, et al. Superposed Basin Types and Exploration Realms in Mesozoic Yingen-Ejina Basins in the West of Nei Mongol[J]. Northwestern Geology, 2006, 39(1): 89-96.

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Superposed Basin Types and Exploration Realms in Mesozoic Yingen-Ejina Basins in the West of Nei Mongol

1.
China Geology University, Beijing 100083, China;Nortwest Institute of Geology, PetroChina, Lanzhou 730020, China
2.
China Geology University, Beijing 100083, China
3.
Nortwest Institute of Geology, PetroChina, Lanzhou 730020, China

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Received Date: March 31, 2005
Revised Date: October 31, 2005
Published Date: March 04, 2006

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Abstract

Abstract

Yingen-Ejina Basins in the west of Nei Mongol is shown by superposition of Mesozoic and Cainozoic on basement of pre-Palaeozoic constitutes.Its evolution of the tectonism include hump and fission in high temperature stage in Triassic,initial rift valley devopment stage in the Early and Middle Jurassic,rift basin devopment stage in the Early Cretaceous,open and sag stage in the Later Cretaceous and convergent and extruding stage in continent from Tertiary to Quaternary.In these process of evolution,it deposited mainly hydrocarbon source rocks of lacustrine facies in the Early Cretaceous and secondary coal measures source rocks in Early-Middle Jurassic.The basin can be divided in to three types such a sentire superpo sition,basic superposition and displaced superpo sition according to the superposition correlation among of the tectonic layers.
- Yingen-Ejina basins,
- superposition basin,
- exploration near source rocks,
- exploration realms

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Superposed Basin Types and Exploration Realms in Mesozoic Yingen-Ejina Basins in the West of Nei Mongol

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