中国东北漠河盆地的构造背景和地质演化

doi:10.11743/ogg20060414

Abstract

Abstract:

Based on the sedimentary features and facies change of the Upper Jurassic in Mohe basin and supported by many other evidences,it is proposed for the first time that the late Jurassic Mohe basin is a molasse basin controlled by the Yanshanian intracontinental orogeny,which was caused by the activation of the fossil suture zones related to subduction of the Mongolia-Ochotsk ocean.Three stages of the development of the basin have been established and the northward migration feature of its dynamic evolution has been identified.At the end of Jurassic the basin closed and was reformed by the W-E trending thrusts(the main deformation episode) along with continent-continent collision.From the Cretaceous to the Eogene,two phases of reformation happened in the basin and their structure features are nearly NNE trending transtentional faults,with at least three deformation episodes recognized and W-E trending normal faults.In terms of oil and gas exploration potential,the central,eastern,and southern part of the basin are more promising than the rest parts of the basin.

Key words: foreland basin, Yanshanian intracontinental orogeny, formation and reformation, Late Jurassic, Mohe in Heilongjiang

CLC Number:

TE111.2

Wu Genyao, Feng Zhiqiang, Yang Jianguo, Wang Zaijun, Zhang Liguo, Guo Qingxia. Tectonic setting and geological evolution of Mohe basin in Northeast China[J]. Oil & Gas Geology, 2006, 27(4): 528-535.

References

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Tectonic setting and geological evolution of Mohe basin in Northeast China

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