鄂尔多斯盆地多种能源矿产分布及其构造背景

邓军; 王庆飞; 高帮飞; 徐浩; 周应华

Volume 31 Issue 3

May 2006

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Article Navigation > Earth Science > 2006 > 31(3): 330-336

DENG Jun, WANG Qing-fei, GAO Bang-fei, XU Hao, ZHOU Ying-hua, 2006. Distribution and Tectonic Background of Various Energy Resources in Ordos Basin. Earth Science, 31(3): 330-336.

Citation:

DENG Jun, WANG Qing-fei, GAO Bang-fei, XU Hao, ZHOU Ying-hua, 2006. Distribution and Tectonic Background of Various Energy Resources in Ordos Basin. Earth Science, 31(3): 330-336.

DENG Jun, WANG Qing-fei, GAO Bang-fei, XU Hao, ZHOU Ying-hua, 2006. Distribution and Tectonic Background of Various Energy Resources in Ordos Basin. Earth Science, 31(3): 330-336.

Citation:

DENG Jun, WANG Qing-fei, GAO Bang-fei, XU Hao, ZHOU Ying-hua, 2006. Distribution and Tectonic Background of Various Energy Resources in Ordos Basin. Earth Science, 31(3): 330-336.

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Distribution and Tectonic Background of Various Energy Resources in Ordos Basin

DENG Jun^{1, 2
,},
WANG Qing-fei^{1, 2},
GAO Bang-fei^{1, 2},
XU Hao^{1, 2},
ZHOU Ying-hua^{1, 2}

1.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China
2.
Key Laboratory of Lithosphere Tectonics and Lithoprobing Technology of Ministry of Education, China University of Geosciences, Beijing 100083, China

Publish Date: 2006-05-25

Abstract

Abstract

The formation process of the various energy resources coexisting system and its regional tectonic background in Ordos basin are analyzed by introducing the "metallogenic system" theory in this paper. The Mesozoic is the important transition period of the regional tectonic regime, during which the orogeny is outstanding around the basin and three rectothermal events took place in the basin. The transition of the tectonic regime induces the occurrence of various accumulating processes of the inorganic and organic fluids, for example, the organic fluid in the basin is activated by the recto-thermal events and the inorganic fluid flowing towards the basin is produced due to the orogeny. The reciprocity between the inorganic and organic fluids happens during their transporting. The existence of the organic fluid produces the redox barrier, which causes the mutation of the physicochemical parameters of the inorganic fluid and the precipitation of the uranium element at the interface. The mutation and interface effects are obvious in the formation of the various energy resources.
- Ordos basin,
- various energy resources,
- orogeny,
- interface mineralization

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References(46)

References

Brian, J.D., Bradley, D.R., 2002. Mesozoic contractional deformation in the middle of the Asian tectonic collage: The intraplate western Ordos fold-thrust belt, China. EPSL, 205: 13-24. doi: 10.1016/S0012-821X(02)01026-9

Dang, B., 2003. The tectonic and sedimentary evolution and its relationship to gas accumulation of Lower Paleozoic in Ordos basin(Dissertation). Northwest University, Xi'an, 43-77(in Chinese with English abstract).

Gao, J. Y., Wang, Y.X., Qiu, Y.Z., et al., 2001. Islandsocean structural evolution of mid-western continent in Inner Mongolia. Geotectonica et Metallogenia, 25(4): 397-404(in Chinese with English abstract).

Guo, J.J., Zhang, G.W., Lu S.N., et al., 1995. Neoproterozoic continental block collage of China and Rodinia supercontinent. Geological Journal of China Universities, 5(2): 148-156(in Chinese with English abstract).

Li, J., Luo, X., Shan, X.Q., et al., 2005. Natural gas accumulation in the Upper Paleozoic of Ordos basin, China. Petroleum Exploration and Development, 32(4): 54-59(in Chinese with English abstract).

Li, S.L., Ouyang, Z.Y., 1998. Tectonic framework and evolution of Xing'anling-Mongolian orogenic belt(XMOB) and its adjacent region. Marine Geology & Quaternary Geology, 18(3): 45-54(in Chinese).

Liu, S.F., 1998. The coupling mechanism of basin and orogen in the western Ordos basin and adjacent regions of China. Journal of Asian Earth Sciences, 16(4): 369-383. doi: 10.1016/S0743-9547(98)00020-8

Ren, Z.L., 1995. Thermal history of Ordos basin assessed by apatite fission track analysis. Chinese Journal of Geophysics, 38(3): 339-349(in Chinese with English abstract).

Sun, S.H., Li, X.M., Gong, G.L., et al., 1997. Study on the tectonic thermal events of Ordos basin. Chinese Science Bulletin, 42(3): 306-308(in Chinese). doi: 10.1360/csb1997-42-3-306

Sun, Y., Li, Z.Y., Xiao, X.J., et al., 2004. Relationship between oil-gas trap and uranium metallogenesis at northern Ordos basin. Uranium Geology, 20(6): 337-343 (in Chinese with English abstract).

Tang, D.Z., Yang, Q., Pan, Z.G., 1992. The simulation of geological thermal history and coal metamorphic evolution in Hedong coalfield. Geoscience, 6(3): 328-337(in Chinese with English abstract).

Wang, C.Y., Guo, Y.H., Jiang, B., et al., 2004. Sequence stratigraphic division of Jurassic Yan'an Formation in West Ordos basin. Journal of China University of Mining & Technology, 33(1): 15-18(in Chinese with English abstract).

Wang, L.Z., Dai, T.M., Peng, P.A., 2005.40Ar/39Ar dating of diagenetic illites and its application in timing gas emplacement in gas reservoirs. Earth Science-Journal of China University of Geosciences, 30(1): 78-82(in Chinese with English abstract).

Wang, S.M., 1996. Coal accumulating and coal resource evaluation of Ordos basin. China Coal Industry Publishing House, Beijing, 1-437(in Chinese).

Wei, Y.P., Wang, Y., 2004. Comparison of enrichment patterns of various energy resources in Ordos basin. Oil & Gas Geology, 25(4): 385-392(in Chinese with English abstract).

Xia, Y.L., Lin, J.R., Liu, H.B., et al., 2003. Research on geochronology of sandstone-hosted uranium oreformation in major uranium productive basins, northern China. Uranium Geology, 19(3): 129-136(in Chinese with English abstract).

Xiao, X. J., Li, Z. Y., Fang, X. H., et al., 2004. The evidences and significances of epithermal mineralization fluid in the Dongsheng sandstone type uranium deposit. Bulletin of Mineralogy, Petrology and Geochemistry, 23(4): 301-304(in Chinese with English abstract).

Yang, J.J., 2002. Tectonic evolution and oil and gas distribution in the Ordos basin. Petroleum Industry Press, Beijing, 23-27, 51-52, 210(in Chinese).

Yin, H.F., Wu, S.B., Du, Y.S., et al., 1999. South China defined as part of Tethyan archipelagic ocean system. Earth Science-Journal of China University of Geosciences, 24(1): 1-12(in Chinese with English abstract).

Zhai, Y.S., Deng, J., Li, X.B., 1999. Essentials of metallogeny. Geological Pubilishing House, Beijing, 287(in Chinese).

Zhai, Y.S., Deng, J., Tang, Z.L., et al., 2002. Metallogenic systems of paleocontinental margin. Geological Publishing House, Beijing, 416(in Chinese).

Zhang, G.W., Zhang, B.R., Yuan, X.C., et al., 2001. Qinling orogenic belt and continental dynamics. Science Press, Beijing, 1-855(in Chinese).

Zhang, H., Bai, Q.Z., Zhang, X.W., et al., 1995. Formation of the Ordos basin and its coal-forming tectonic environment. Geology and Exploration of Coal Field, 23 (3): 1-9(in Chinese with English abstract).

Zhang, K., 1989. Tectonics and resourses of Ordos fault block. Shaanxi Science and Technology Press, Xi'an, 1-394(in Chinese).

党, 2003. 鄂尔多斯盆地构造沉积演化与下古生界天然气聚集关系研究(博士学位论文). 西北大学, 西安.

高计元, 王一先, 裘愉卓, 等, 2001. 内蒙古中西部多岛海构造演化. 大地构造与成矿学, 25(4): 397-404. doi: 10.3969/j.issn.1001-1552.2001.04.006

郭进京, 张国伟, 陆松年, 等, 1995. 中国新元古代大陆拼合与Rodinia超大陆. 高校地质学报, 5(2): 148-156. https://www.cnki.com.cn/Article/CJFDTOTAL-GXDX902.002.htm

李剑, 罗霞, 单秀琴, 等, 2005. 鄂尔多斯盆地上古生界天然气成藏特征. 石油勘探与开发, 32(4): 54-59. doi: 10.3321/j.issn:1000-0747.2005.04.009

李双林, 欧阳自远, 1998. 兴蒙造山带及邻区的构造格局与构造演化. 海洋地质与第四纪地质, 18(3): 45-54. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ803.006.htm

任战利, 1995. 利用磷灰石裂变径迹法研究鄂尔多斯盆地地热史. 地球物理学报, 38(3): 339-349. doi: 10.3321/j.issn:0001-5733.1995.03.009

孙少华, 李小明, 龚革联, 等, 1997. 鄂尔多斯盆地构造热事件研究. 科学通报, 42(3): 306-308. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB199703024.htm

孙晔, 李子颖, 肖新建, 等, 2004. 油气圈闭与鄂尔多斯盆地北部铀成矿关系探讨. 铀矿地质, 20(6): 337-343. doi: 10.3969/j.issn.1000-0658.2004.06.003

汤达祯, 杨起, 潘治贵, 1992. 河东煤田地史-热史模拟与煤变质演化. 现代地质, 6(3): 328-337. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ199203010.htm

王超勇, 郭英海, 姜波, 等, 2004. 鄂尔多斯盆地西缘延安组层序地层划分. 中国矿业大学学报, 33(1): 15-18. https://www.cnki.com.cn/Article/CJFDTOTAL-ZGKD200401003.htm

王龙樟, 戴橦谟, 彭平安, 2005. 自生伊利石40Ar/39Ar法定年技术及气藏成藏期的确定. 地球科学———中国地质大学学报, 30(1): 78-82. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200501010.htm

王双明, 1996. 鄂尔多斯盆地聚煤规律及煤炭资源评价. 北京: 煤炭工业出版社, 1-437.

魏永佩, 王毅, 2004. 鄂尔多斯盆地多种能源矿产富集规律的比较. 石油与天然气地质, 25(4): 385-392. doi: 10.3321/j.issn:0253-9985.2004.04.006

夏毓亮, 林锦荣, 刘汉彬, 等, 2003. 中国北方主要产铀盆地砂岩型铀矿成矿年代学研究. 铀矿地质, 19(3): 129-136. doi: 10.3969/j.issn.1000-0658.2003.03.001

肖新建, 李子颖, 方锡珩, 等, 2004. 东胜砂岩型铀矿床低温热液流体的证据及意义. 矿物岩石地球化学通报. 23(4): 301-304. doi: 10.3969/j.issn.1007-2802.2004.04.004

杨俊杰, 2002. 鄂尔多斯盆地构造演化与油气分布规律. 北京: 石油工业出版社, 23-27, 51-52, 210.

殷鸿福, 吴顺宝, 杜远生, 等, 1999. 华南是特提斯多岛洋体系的一部分. 地球科学———中国地质大学学报, 24(1): 1-12. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX901.000.htm

翟裕生, 邓军, 李小波, 1999. 区域成矿学. 北京: 地质出版社, 287.

翟裕生, 邓军, 汤中立, 等, 2002. 古陆边缘成矿系统. 北京: 地质出版社, 416.

张国伟, 张本仁, 袁学诚, 等, 2001. 秦岭造山带与大陆动力学. 北京: 科学出版社, 1-855.

张泓, 白清昭, 张笑薇, 等, 1995. 鄂尔多斯聚煤盆地的形成及构造环境. 煤田地质与勘探, 23(3): 1-9. https://www.cnki.com.cn/Article/CJFDTOTAL-MDKT503.000.htm

张抗, 1989. 鄂尔多斯断块构造和资源. 西安: 陕西科学技术出版社, 394.

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