Publish in OALib Journal
ISSN: 2333-9721
APC: Only $99

Paper Submission

Views	Downloads

Relative Articles
汝箕沟晚中生代玄武岩的确定与煤变质作用关系简论
汝箕沟煤系脉石英包体与煤变质研究
宁夏汝箕沟煤田火区高光谱定量遥感探测研究
国产随钻测量定向钻进系统在汝箕沟煤矿的应用
宁夏汝箕沟矿区煤层气地质学特征
贺兰山汝箕沟地区及中卫探区上三叠统烃源岩初步评价?
高光谱技术在汝箕沟煤田烧变岩和Fe3+丰度信息提取中的方法研究
鄂尔多斯盆地西缘汝箕沟大岭－鼓鼓台玄武岩锆石U-Pb定年及其构造意义
河南？汝？烟煤？
对开展？孔？易水文地？观？工作的几点意？
More...

地质学报 2006

鄂尔多斯盆地西缘汝箕沟煤矿区的石英脉及其地质意义

, PP. 768-774

Keywords: 鄂尔多斯盆地西缘,宁夏汝箕沟,无烟煤,石英脉,发育特征,地质意义

Full-Text Cite this paper Add to My Lib

Abstract:

鄂尔多斯盆地西缘地处特殊的大地构造位置,其间的宁夏汝箕沟出产世界上最优质的无烟煤,该区多年来一直被多学科科研人员所关注。笔者从地质背景入手,较详细的论述了汝箕沟矿区石英脉的岩性、与围岩的接触关系、规模、时空分布、产状、组合、矿物包裹体等发育特征,比较了该区石英脉与诸多煤田和煤系中脉岩的差异。综合分析认为,该区石英脉与推测隐伏火成岩体紧密相关,深部岩浆分异后期的气成热液上涌是石英脉形成的主导因素。石英脉对该区构造热事件、深大断裂活动、煤变质类型等有一定指示意义。本文研究表明,汝箕沟侏罗纪煤变质与盆地油、气成藏同受晚侏罗世―早白垩世期间的构造热事件影响,同一重大地质事件在盆地内部和边缘表现形式有别,各地响应方式不同。

References

[1]	高峰,王岳军,刘顺生,等.2000.利用磷灰石裂变径迹研究鄂尔多斯盆地西缘热历史.大地构造与成矿学,24(1):87～91.
[2]	李思田,程守田,杨士恭,等.1992.鄂尔多斯盆地东北部层序地层及沉积体系分析.北京:地质出版社,13～21.
[3]	柳益群,李文厚,冯乔.1997.鄂尔多斯盆地东部上三叠统含油砂岩的古地温及成岩阶段.地质学报,71(1):65～74.
[4]	潘爱芳,赫英,马润勇.2004.鄂尔多斯盆地地表元素地球化学场与能源矿产关系初探.石油与天然气地质,25(6):629～633.
[5]	苏春乾,杨兴科,刘继庆,张忠义.2004.从贺兰山区的三叠--侏罗系论国内前陆盆地的研究.岩石矿物学杂志,23(4):318～326.
[6]	吴传荣,张慧,李远虑,李小彦,汪程生.1995.西北早--中侏罗世煤岩煤质与煤变质研究.北京:煤炭工业出版社,78～97,128～157.
[7]	张慧,李小彦.1993.汝箕沟煤中矿物研究及其意义.矿物学报,13(4):362-367.
[8]	张慧,吴传荣,李小彦,闫述.1994.汝箕沟煤系脉石英包体与煤变质研究.煤田地质与勘探,22(3):23～26.
[9]	Bureau of Geology and Mineral Resources of Ningxia Hui Autonomous Region.1990.Regional Geology of Ningxia Hui Autonomous Region.Beijing:Geological Publishing House,145 ～ 171 (in Chinese).
[10]	Gao Feng,Wang Yuejun,Liu Shunsheng,et al.2000.Thermal history study in the west of the ordos basin using apatite fission track analysis.Geotectonica et Metallogenia,24 (1):87 ～ 91 (in Chinese with English abstract).
[11]	Li Sitian,Cheng Shoutian,Yang Shigong.1992.Sequence stratigraphy and depositional system analysis of the Northeastern Ordos basin.Beijing:Geological Publishing House,13 ～ 21 (in Chinese).
[12]	Liu Chiyang,Zhao Hongge,Wang Feng,Chen Hong.2005.Mesozoic structure attribute in the west(margin) of Ordos basin.Acta Geologica Sinica,71 (1):65～ 74 (in Chinese with English abstract).
[13]	McNeil B,Shaw H F,Rankin A H.1998.The timing in the Rotliegend sandstones of the southern North Sea:a petrological and fluid inclusion study of cements.J.Petroleum Geology,21 (3):311～328.
[14]	Ren Zhanli.1995.Application of apatite fission track analysis method to the study of thermal history of the Ordos Basin.Chinese Journal of Geophysics,38(2):235～247.
[15]	Sachsenhofer R F,Privalov V A,Zhykalyak M V,Bueker C,Panova E A,Rainer T,Shymanovskyya V A,Stephenson R.2002.Donets Basin(Ukraine/Russia):coalification and thermal history.International Journal of Coal Geology,49:3～55.
[16]	Su Chunqian,Yang Xingke,Liu Jiqing,Zhang Zhongyi.2004.A study of foreland basins in the light of Triassic-Jurassic strata of the Helan Mountain.Acta Petrologica et Mineralogical,23(4):318～326(in Chinese with English abstract).
[17]	Wu Chuanrong,Zhang Hui,Li Yuanlu,Li Xiaoyan,Wang Chengsheng.1995.Research on Coal Petrology Properties and Metamorphism of Early-Mid Jurassic Coal in Northwest China.Beijing:China Coal Industry Publishing House,78～97,128～157(in Chinese).
[18]	Zhang Hong,He Zonglian,Jin Xianglan,Zhang Peihe,Meng Zhaoping.2005.Tectonic evolution and coal accumulation of the Ordos coal basin.Beijing:Geological Publishing House,17 ～ 24 (in Chinese).
[19]	Zhang Hui,Wu Chuanrong,Li Xiaoyan,Yan Shu.1994.A study of the inclusion in quartz veins with coal measures and coal metamorphism at Rujigou Area.Coal Geology & Exploration,22(3):23 ～ 26 (in Chinese with English abstract).
[20]	高山林,李芳,李天斌,吕昌国,陆彦俊.2003.汝箕沟晚中生代玄武岩的确定与煤变质作用关系简论.煤田地质与勘探,31(3):8～10.
[21]	刘池洋,赵红格,王峰,陈洪.2005.鄂尔多斯盆地西缘(部)中生代构造属性.地质学报,79(6):738～747.
[22]	宁夏回族自治区地质矿产局.1990.宁夏回族自治区区域地质志.北京:地质出版社,145～171.
[23]	潘治贵,兰庆余,陈基娘,等.1992.热水煤田煤的热水变质特征.北京:地质出版社,61～77.
[24]	谭勇杰.1989.煤变质古地温恢复方法探讨.煤田地质与勘探,(2):30～36.
[25]	杨起.1996.中国煤变质作用.北京:煤炭工业出版社,44～58.
[26]	张泓,何宗莲,晋香兰,张培河,孟昭平.2005.鄂尔多斯盆地构造演化与成煤作用.北京:地质出版社,17～24.
[27]	张慧,吴传荣,李小彦.1995.西北中生代煤系岩脉发育特征与煤变质关系.煤炭学报,20(2):218～222.
[28]	Gao Shanlin,Li Fang,Li Tianbing,Lu Changguo,Lu Yanjun.2003.Discussion of the relationship between coal metamorphism and the Late Mesozoic basin in Rujigou Area.Coal Geology & Exploration,31 (3):8 ～ 10 (in Chinese with English abstract).
[29]	Liu Yiqun,Li Wenhou,Feng Qiao.1997.Palaeotemperatures and diagenetic stage of the upper Triaddic oil sandstones in the eastern Ordos basin.Acta Geologica Sinica,71 (1):65 ～ 74 (in Chinese with English abstract).
[30]	Pan Aifang,He Ying,Ma Runyong.2004.Preliminary study of relation between geochemical field of surface elements and energy minerals in Ordos basin.Oil & Gas Geology,25(6):629～633(in Chinese with English abstract).
[31]	Pan Zhigui,Lan Qingyu,Chen Jiniang,et al.1992.Characteristics of hydrothermal metamorphism of coal in Reshui coalfield.Beijing:Geological Publishing House,61～77(in Chinese).
[32]	Scott M,Charles B.2003.Coalbed methane,cook inlet,south central Alaska:a potential giant gas resourve.AAPG,87(1):1～13.
[33]	Tan Yongjie.1989.Method discussing on comback palaeotemperatures of coal metamorphism.Coal Geology & Exploration,(2):30～ 36(in Chinese with English abstract).
[34]	Yang Qi.1996.The coal metamorphism in China.Beijing:China Coal Industry Publishing House,44 ～ 58 (in Chinese).
[35]	Zhang Hui,Li Xiaoyan.1993.Genetic studies of minerals from coal in Rujigou and their implication.Acta Mineralogica Sinica,13 (4):362～367(in Chinese with English abstract).
[36]	Zhang Hui,Wu Chuanrong,Li Xiaoyan.1995.Coal metamorphism and characteristics of veins in mesozoic coal measures in northwest area.Journal of China Coal Society,20 (2):218 ～ 222 (in Chinese with English abstract).

Full-Text