沁水盆地新生代抬升冷却事件的确定

doi:10.11743/ogg20050115

Abstract

Abstract:

ission-track analyses of apatite and zircon show that an uplift-cooling event occurred in Qinshui basin 26.2-11.5Ma ago. It occurred earlier in the northern and southern parts, and later in the central part. Qinshui basin experienced a large uplift-cooling event from Oligocene to Miocene, as a result, the formation temperature decreased and the hydrocarbon generating process in the Permo-Carboniferous coal measure strata ceased.

Key words: Qinshui basin, tectonic-thermal event, cooling event, fission track

CLC Number:

R121.1

Ren Zhanli, Xiao Hui, Liu Li, Zhang Sheng, Lei Liqing, Qin Yong, Wei Chongtao. Determination of Cenozoic uplift-cooling event in Qinshui basin[J]. Oil & Gas Geology, 2005, 26(1): 109-113.

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Determination of Cenozoic uplift-cooling event in Qinshui basin

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