沁水盆地新生代抬升冷却事件的确定

doi:10.11743/ogg20050115

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

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. 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
基金资助:
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 Zhanli^1,2, Xiao Hui², Liu Li², Zhang Sheng², Lei Liqing², Qin Yong³, Wei Chongtao³

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/Abstract

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

中图分类号:

R121.1

任战利,肖晖,刘丽,等. 沁水盆地新生代抬升冷却事件的确定[J]. 石油与天然气地质, 2005, 26(1): 109-113. doi: 10.11743/ogg20050115 Ren Zhanli,Xiao Hui,Liu Li,et al. Determination of Cenozoic uplift-cooling event in Qinshui basin[J]. Oil & Gas Geology, 2005, 26(1): 109-113. doi: 10.11743/ogg20050115

参考文献

[1] 赵庆波.煤成气地质与勘探技术[M].北京:石油工业出版社,1999
[2] 利文阳,马新华,赵庆波,等.中国煤成气地质评价与勘探技术新进展[M].徐州:中国矿业大学出版社,2001
[3] 张建博,王红岩.沁水煤成气有利区预测[M].徐州:中国矿业大学出版社,2001
[4] 秦勇,宋党育.山西南部煤化作用及其古地热系统[M].北京:地质出版社,1998
[5] 任战利,赵重远.鄂尔多斯盆地与沁水盆地中生代晚期地温场对比研究[J].沉积学报,1997, 15(2):134～137Ren Zhanli,Zhao Zhongyuan.Late Mesozoic comparative research on the geothermal field Ordos basin and Qinshui basin[J].Acta Sedimentologica Sinica,1997,15(2):134-137
[6] 任战利,赵重远,陈刚,等.沁水盆地中生代晚期构造热事件[J].石油与天然气地质,1999,20(1):46～48Ren Zhanli,Zhao Zhongyuan,Chen Gang,et al.Tectonical thermal events of late Mesozoic in Qinshui basin[J].Oil & Gas Geology,1999,20(1):46-48
[7] Ren Zhanli,Wang Shicheng,Zhao Zhongyuan.Determination of palaeotemperatare and palaeogeothermal gradient in Qinshui basin[J].Progress in Natural Science,2000,10(4):232-238
[8] 任战利.中国北方沉积盆地构造热演化史研究[M].北京:石油工业出版社,1999
[9] 任战利.沁水盆地沁参1井大地热流值确定[J].地质科学,1998,32(2):251～254Ren Zhanli.Determination of the geothermal heat flow of well Qincan No.1 in Qinshui basin[J].Chinese Journal of Geology,1998,32(2):251-254
[10] 陈衍景,郭光军,李欣.华北克拉通花岗绿岩体中中生代金矿床的成矿地球动力学背景[J].中国科学(D辑),1998,28(1):35～40Chen Yanjing,Guo Guangjun,Li Xin.Geodynamic background of Mesozoic golden ore formation in granitic-greenstone terrain on North China craton[J].Science in China(series D),1998,28(1):35-40
[11] 毛景文,张作衡,余金杰,等.华北及邻区中生代大规模成矿的地球动力学背景:从金属矿床年龄精测得到的启示[J].中国科学(D辑),2003,33(4):289～299Mao Jingwen,Zhang Zuoheng,Yu Jinjie,et al.Geodynamic background of broad ore formation in scale on Mesozoic in North China and adjacent region:guidance from accurate measurements of metallic ores ages[J].Science in China(series D),2003,33(4):289-299
[12] 罗照华,邓晋福,李王文,等.太行山构造岩浆带K-Ar法同位素年龄分析[J].现代地质,1996,10(3):344～349Luo Zhaohua,Deng Jinfu,Li Yuwen,et al.Interpretation of K-Ar ages of Taihang tectonomagmatic belt[J].Geoscience,1996,10(3):344-349
[13] Naeser N D, Naeser C W,McCullon T H.The application of fission track dating to the depositional and thermal history of rock in sedimentary basins[A].In:Naeser N D,McCullon T H.Thermal history of sedimentary basins:methods and case history[C].Beijing:Spring-Verlag,1989.157-180
[14] Fitzgerald P G,Gleadow A J W.Fission track geochronology,tectonics and structure of the Transantarctic mountains in Northern Victoria Land[J].Antactica Chem Geol,1988,73:169-198
[15] Brandon M T,Vance J A.Fission track ages of detrital zircons:implications for the tectonic evolution of the Cenozoic Olympic subduction complex[J]. Am J Sci,1992,292:565-636
[16] Hurford A J.Cooling and uplift patterns in the Lepontine Alps, south central Switzerland,and an age of vertical movement on the Insubric fault line[J].J Contrib Min Petrol,1986,92:413-427
[17] 任战利,赵重远.中生代晚期中国北方沉积盆地古地热梯度及对比[J].石油勘探与开发,2001,28(6):1～4Ren Zhanli,Zhan Zhongyuan.Plaeo-geothermal gradient and comparison of sedimentary basins on Mesozoic in the north China[J].Petroleum Exploration and Development,2001,28(6):1-4
[18] 任战利.中国北方沉积盆地热演化史的对比[J].石油与天然气地质,2000,21(1):33～37Ren Zhanli.Comparison of thermal evolution history in sedimentary basins in the north China[J].Oil & Gas Geology,2000,21(1):33-37
[19] 刘池洋,赵重远,杨新科,等.活动性强、深部作用活跃--中国沉积盆地的两个重要特点[J].石油与天然气地质,2000,21(1):1～6Liu Chiyang,Zhao Zhongyuan,Yang Xingke,et al.Strong activity and active deep action:two important features of Chinese sedimentary basins[J].Oil & Gas Geology,2000,21(1):1-2
[20] 李吉钧,文世宣,张青松,等.青藏高原隆生的时代、幅度和形式的探讨[J].中国科学(D辑),1979,9(6):608～616Li Jijun,Wen Shixuan,Qingsong,et al.Explorations on times,scopes and forms of Qinghai-Xizang plateau uplift[J].Science in China(series D),1979,9(6),608-616

沁水盆地新生代抬升冷却事件的确定

Determination of Cenozoic uplift-cooling event in Qinshui basin

PDF (PC)

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

[1]	史今雄, 曾联波, 谭青松, 王继鹏, 张云钊, 李宏为. 沁水盆地南部煤岩储层天然裂缝有效性及对煤层气开发的影响[J]. 石油与天然气地质, 2020, 41(3): 617-626.
[2]	袁学浩, 姚艳斌, 甘泉, 刘大锰, 周智. TOUGH-FLAC^3D热流固耦合模拟煤储层水力压裂过程[J]. 石油与天然气地质, 2018, 39(3): 611-619.
[3]	王勃, 姚红星, 王红娜, 赵洋, 李梦溪, 胡秋嘉, 樊梅荣, 杨春莉. 沁水盆地成庄区块煤层气成藏优势及富集高产主控地质因素[J]. 石油与天然气地质, 2018, 39(2): 366-372.
[4]	李俊乾, 卢双舫, 薛海涛, 王伟明, 张萍. 高阶煤层气储层非均质性及其定量评价——以沁水盆地南部郑庄区块为例[J]. 石油与天然气地质, 2016, 37(1): 72-79.
[5]	崔军平, 任战利, 李金翔, 阴玲玲, 王文青. 海拉尔盆地呼伦湖凹陷热演化史恢复[J]. 石油与天然气地质, 2015, 36(1): 35-42.
[6]	李天义, 周雁, 方石, 何生, 何治亮, 樊德华. 磷灰石裂变径迹年龄测试分析新方法——激光剥蚀-ICPMS法[J]. 石油与天然气地质, 2013, 34(4): 550-557.
[7]	任战利,萧德铭,迟元林,任延广,梁宇. 松辽盆地基底石炭-二叠系热演化史[J]. 石油与天然气地质, 2011, 32(3): 430-439.
[8]	王韶华, 罗开平, 刘光祥. 江汉盆地周缘中、新生代构造隆升裂变径迹记录[J]. 石油与天然气地质, 2009, 30(3): 255-259.
[9]	任战利, 张盛, 高胜利, 崔军平, 刘新社. 伊盟隆起东胜地区热演化史与多种能源矿产的关系[J]. 石油与天然气地质, 2006, 27(2): 187-193.
[10]	汪新伟, 汪新文, 韩效忠. 运用磷灰石裂变径迹分析十万山盆地的地热史[J]. 石油与天然气地质, 2003, 24(4): 385-390,412.
[11]	任战利. 中国北方沉积盆地热演化史的对比[J]. 石油与天然气地质, 2000, 21(1): 33-37.
[12]	任战利, 赵重远, 陈刚, 王世成. 沁水盆地中生代晚期构造热事件[J]. 石油与天然气地质, 1999, 20(1): 46-48.
[13]	陈刚. 沁水盆地向斜型水封气藏形成条件探讨[J]. 石油与天然气地质, 1998, 19(4): 302-306.
[14]	单秀琴. 沁水盆地煤层储集性能[J]. 石油与天然气地质, 1998, 19(4): 321-325.
[15]	刘树根, 罗志立, 戴苏兰, D. Arne. 川西前陆盆地的“四川运动”及与油气的关系[J]. 石油与天然气地质, 1996, 17(4): 276-281.