石油与天然气地质 ›› 2005, Vol. 26 ›› Issue (1): 109-113.doi: 10.11743/ogg20050115

• 油气地质 • 上一篇    下一篇

沁水盆地新生代抬升冷却事件的确定

任战利1,2, 肖晖2, 刘丽2, 张盛2, 雷利庆2, 秦勇3, 韦重韬3   

  1. 1. 西北大学大陆动力学教育部重点实验室, 陕西西安, 710069;
    2. 西北大学地质学系, 陕西西安, 710069;
    3. 中国矿业大学, 江苏徐州, 221008
  • 收稿日期:2005-01-07 出版日期:2005-02-25 发布日期:2012-01-16
  • 基金项目:

    国家973计划项目"中国煤成气成藏机制及经济开采基础研究"(2002CB211704);"多种能源矿产共存成藏(矿)机理与富集分布规律"(2003CB214605)

Determination of Cenozoic uplift-cooling event in Qinshui basin

Ren Zhanli1,2, Xiao Hui2, Liu Li2, Zhang Sheng2, Lei Liqing2, Qin Yong3, Wei Chongtao3   

  1. 1. Key Laboratory of Continental Dynamics, Ministry of Education, Northwest University, Xi'an, Shaanxi;
    2. Department of Geology, Northwest University, Xi'an, Shaanxi;
    3. China University of Mining, Xuzhou, Jiangsu
  • Received:2005-01-07 Online:2005-02-25 Published:2012-01-16

摘要:

磷灰石、锆石裂变径迹分析资料表明沁水盆地在26.2~11.5Ma前发生过一次抬升冷却事件,具有盆地南、北部抬升冷却早,中部抬升冷却晚的特点,渐新世—中新世的抬升冷却与青藏高原在新近纪的大规模隆升有关。新生代渐新世—中新世发生大规模抬升冷却,地层温度降低,石炭-二叠纪煤系地层生烃过程停止。

关键词: 沁水盆地, 构造热事件, 冷却事件, 裂变径迹

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

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