彬县-铜川地区延长组油页岩晚白垩世以来的抬升剥蚀与冷却历史

于强; 任战利; 朱增伍; 陶霓; 王宝江; 李长春

doi:10.3799/dqkx.2018.596

Volume 43 Issue 6

Jun. 2018

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Article Navigation > Earth Science > 2018 > 43(6): 1839-1849

Yu Qiang, Ren Zhanli, Zhu Zengwu, Tao Ni, Wang Baojiang, Li Changchun, 2018. Exhumation, Cooling and Erosion History of Triassic Oil Shale since Late Cretaceous, Binxian-Tongchuan Area of Ordos Basin. Earth Science, 43(6): 1839-1849. doi: 10.3799/dqkx.2018.596

Citation:

Yu Qiang, Ren Zhanli, Zhu Zengwu, Tao Ni, Wang Baojiang, Li Changchun, 2018. Exhumation, Cooling and Erosion History of Triassic Oil Shale since Late Cretaceous, Binxian-Tongchuan Area of Ordos Basin. Earth Science, 43(6): 1839-1849. doi: 10.3799/dqkx.2018.596

Citation:

Yu Qiang, Ren Zhanli, Zhu Zengwu, Tao Ni, Wang Baojiang, Li Changchun, 2018. Exhumation, Cooling and Erosion History of Triassic Oil Shale since Late Cretaceous, Binxian-Tongchuan Area of Ordos Basin. Earth Science, 43(6): 1839-1849. doi: 10.3799/dqkx.2018.596

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Exhumation, Cooling and Erosion History of Triassic Oil Shale since Late Cretaceous, Binxian-Tongchuan Area of Ordos Basin

doi: 10.3799/dqkx.2018.596

Yu Qiang^{1,2
,},
Ren Zhanli^3,4,
Zhu Zengwu⁵,
Tao Ni^1,2,
Wang Baojiang⁶,
Li Changchun⁵

1.
School of Earth Science and Resources, Chang'an University, Xi'an 710054, China
2.
The Laboratory of Mineralization and Dynamics, Chang'an University, Xi'an 710054, China
3.
Department of Geology, Northwest University, Xi'an 710069, China
4.
State Key Laboratory of Continental Dynamics, Northwest University, Xi'an 710069, China
5.
Shanxi Geological Survey Center, Xi'an 710068, China
6.
Research Institute of Yanchang Petroleum(Group) Company Limited, Shanxi, Xi'an 710075, China

Received Date: 2018-01-04
Publish Date: 2018-06-15

Abstract

Abstract

The recovery of exhumation history of oil shale with the method of geothermometer and thermochronology has scientific significance for the study of thermal background of oil shale mineralization and its reformation. Based on the theory of tectonothermal evolution, the paleogeotemperature, the exhumation-related cooling and the erosion of the Triassic oil shale since Late Cretaceous in the Binxian area and the Tongchuan area were recovered with the fission track data from the well Yongcan1 and the (U-Th)/He data from the drilling well ZK900, respectively. The tectonothermal evolution difference of the two areas are discussed. The average (U-Th)/He ages of the Chang6, Chang9 and Chang10 samples are 43.83 Ma, 31.87 Ma, and 22.88 Ma respectively. Three stages of exhumation-cooling since Late Cretaceous of the Tongchuan area were recovered:97-40 Ma, fast exhumation; 40-8 Ma, slow exhumation, and 8 Ma to the present, extremely fast exhumation, respectively. The erosion thickness and exhumation rate are 600 m, 10.5 m/Ma and 10 m, 0.3 m/Ma and 1 290 m, 161.3 m/Ma, respectively. The paleotemperature and cooling rate are 100-60 ℃, 0.70 ℃/Ma and 60-50 ℃, 0.22 ℃/Ma and 50-25 ℃, 2.90 ℃/Ma, respectively. Three stages of exhumation-cooling since Late Cretaceous of the Triassic in the Binxian area were recovered:97-40 Ma, increasing exhumation-cooling (130-75 ℃), cooling rate of 0.96 ℃/Ma, exhumation rate of 14.4 m/Ma, erosion thickness of 820 m; 40-8 Ma with little changed as 75-70 ℃, exhumation rate/cooling rate, 0.16 ℃/Ma and 1.9 m/Ma, erosion thickness of 60 m; 8 Ma to the present with sharp cooling as 70-31 ℃, exhumation rate of 125 m/Ma, cooling rate of 4.88 ℃/Ma, erosion thickness of 1 000 m, respectively. There are three stages for the exhumation-cooling history of the oil shale (Triassic in the Binxian-Tongchuan area). The Eocene (40 Ma) and the Late Miocene (8 Ma) are the critical moments for the cooling of the oil shale during its mineralization. More attention should be paid to the differences of exhumation, cooling, erosion between Binxian area and Tongchuan area when discussing the mineralization of the oil shale and its reformation in the Ordos basin.
- thermochronology,
- Ordos basin,
- (U-Th)/He,
- Weibei uplift,
- oil shale,
- fission track,
- tectonic,
- petroleum geology

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References(35)

References

Cao, K., Wang, G.C., Liu, C., et al., 2009.Thermochronological Evidence of the Cenozoic Differential Uplift Processes of the West Kunlun and Its Adjacent Area.Earth Science, 34(6):895-906 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX200906004.htm

Farley, K.A., 2000.Helium Diffusion from Apatite:General Behavior as Illustrated by Durango Fluorapatite.Journal of Geophysical Research:Solid Earth, 105(B2):2903-2914. https://doi.org/10.1029/1999jb900348

Hu, S.B., He, L.J., Zhu, C.Q., et al., 2008.Method System of Thermal Reconstruction for Marine Basins.Oil & Gas Geology, 29(5):607-613(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYYT200805013.htm

Li, S.Z., Liu, X., Suo, Y.H., et al., 2009.Triassic Folding and Thrusting in the Eastern Block of the North China Craton and the Dabie-Sulu Orogen and Its Geodynamics.Acta Petrologica Sinica, 25(9):2031-2049 (in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-ysxb200909001.htm

Qiu, N.S., Wang, J.Y., Mei, Q.H., et al., 2010.Constraints of (U-Th)/He Ages on Early Paleozoic Tectonothermal Evolution of the Tarim Basin, China.Science China:Earth Science, 40(12):1669-1683(in Chinese). http://kns.cnki.net/KCMS/detail/detail.aspx?filename=jdxg201007005&dbname=CJFD&dbcode=CJFQ

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). http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-DQWX503.008.htm

Ren, Z.L., Cui, J.P., Guo, K., et al., 2015.Fission-Track Analysis of Uplift Times and Processes of the Weibei Uplift in the Ordos Basin.Chinese Science Bulletin, 60(14):1298-1309 (in Chinese). doi: 10.1360/N972014-00617

Ren, Z.L., Zhang, S., Gao, S.L., et al., 2006.Research on Region of Maturation Anomaly and Formation Time in Ordos Basin.Acta Geologica Sinica, 80(5):674-684(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE200605008.htm

Shen, C.B., Mei, L.F., Fan, Y.F., et al., 2005.Advances and Prospects of Apatite Fission Track Thermochronology.Geological Science and Technology Information, 24(2):57-63(in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-dzkq200502014.htm

Tao, N., Li, Z.X., Danišík, M., et al., 2017.Thermochronological Record of Middle-Late Jurassic Magmatic Reheating to Eocene Rift-Related Rapid Cooling in the SE South China Block.Gondwana Research, 46:191-203. http://dx.doi.org/10.1016/j.gr.2017.03.003

Wang, F., Luo, Q.H., Li, Q., et al., 2002. Cooling Event around 30 Ma in the Northern Edge of the Qaidam Basin:Constraints from ⁴⁰Ar/³⁹Ar and Fission Track Thermochronology.Geological Review, 48(Suppl.):88-96(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-KYDH200104005.htm

Wang, J.Q., Liu, C.Y., Yan, J.P., et al., 2010.Development Time and Evolution Characteristics of Weibei Uplift in the South of Ordos Basin.Journal of Lanzhou University (Natural Sciences), 46(4):22-29 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-LDZK201004006.htm

Wolf, R.A., Farley, K.A., Kass, D.M., 1998.Modeling of the Temperature Sensitivity of the Apatite (U-Th)/He Thermochronometer.Chemical Geology, 148(1-2):105-114. https://doi.org/10.1016/s0009-2541(98)00024-2

Xiao, H., Li, J.X., Han, W., et al., 2013.The Tectonic Uplift Time and Evolution Characteristics of Weibei Uplift in the South Edge of Ordos Basin.Jouranl of Xi'an University of Scinece and Technology, 33 (5):576-582, 593(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-XKXB201305014.htm

Yu, Q., 2009. The Thermal Evolution History of Ordos Basin Mesozoic and Its Relationship with Various Energy Mineral Deposit(Dissertation). Northwest University, Xi'an, 33-41 (in Chinese with English abstract).

Yu, Q., Ren, Z.L., Li, R.X., et al., 2017.Paleogeotemperature and Maturity Evolutionary History of the Source Rocks in the Ordos Basin.Geological Journal, 52(S1):97-118. https://doi.org/10.1002/gj.3069

Yu, Q., Ren, Z.L., Ni, J., et al., 2012.The Thermal Evolution History of Mesozoic, Fuxian Exploratory Area of Ordos Basin.Journal of Northwest University (Natural Science Edition), 42(5):801-805(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-XBDZ201205020.htm

Yu, Q., Ren, Z.L., Wang, B.J., et al., 2018.Geothermal Field and Deep Thermal Structure of the Tianshan-Altun Region.Geological Journal. https://doi.org/10.1002/gj.3202

Yuan, W.M., Wang, S.C., Wang, L.F., 2001.Apatite and Zircon Fission Track Study on the Mineralization Age and Its Thermal History of Nanliang Gold Deposit, Eastern Hebei, China.Acta Mineralogica Sinica, 21(2):225-230(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-KWXB200102020.htm

Zhou, X., He, S., Chen, Z.Y., et al., 2016.Characteristics and Controlling Factors of Source Rocks in Yanchang Formation Sequence Framework, Ordos Basin.Earth Science, 41(6):1055-1066(in Chinese with English abstract). https://doi.org/10.3799/dqkx.2016.087

曹凯, 王国灿, 刘超, 等, 2009.西昆仑及邻区新生代差异隆升的热年代学证据.地球科学, 34(6):895-906. http://www.earth-science.net/WebPage/Article.aspx?id=1904

胡圣标, 何丽娟, 朱传庆, 等, 2008.海相盆地热史恢复方法体系.石油与天然气地质, 29(5):607-613. doi: 10.11743/ogg20080509

李三忠, 刘鑫, 索艳慧, 等, 2009.华北克拉通东部地块和大别-苏鲁造山带印支期褶皱-逆冲构造与动力学背景.岩石学报, 25(9):2031-2049. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200909001.htm

邱楠生, 汪集暘, 梅庆华, 等, 2010.(U-Th)/He年龄约束下的塔里木盆地早古生代构造-热演化.中国科学:地球科学, 40(12):1669-1683. http://mall.cnki.net/magazine/Article/JDXK201012005.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. http://mall.cnki.net/magazine/Article/DQWX503.008.htm

任战利, 崔军平, 郭科, 等, 2015.鄂尔多斯盆地渭北隆起抬升期次及过程的裂变径迹分析.科学通报, 60(14):1298-1309. http://www.oalib.com/paper/4267625

任战利, 张盛, 高胜利, 等, 2006.鄂尔多斯盆地热演化程度异常分布区及形成时期探讨.地质学报, 80(5):674-684. http://mall.cnki.net/magazine/Article/DZXE200605008.htm

沈传波, 梅廉夫, 凡元芳, 等, 2005.磷灰石裂变径迹热年代学研究的进展与展望.地质科技情报, 24(2):57-63. http://mall.cnki.net/magazine/article/DZKQ200502014.htm

王非, 罗清华, 李齐, 等, 2002.柴达木盆地北缘30 Ma前的快速冷却事件及构造意义——⁴⁰Ar/³⁹Ar及FT热年代学制约.地质论评, 48(增刊):88-96. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dzlp2002s1016&dbname=CJFD&dbcode=CJFQ

王建强, 刘池洋, 闫建萍, 等, 2010.鄂尔多斯盆地南部渭北隆起发育时限及其演化.兰州大学学报(自然科学版), 46(4):22-29. http://or.nsfc.gov.cn/handle/00001903-5/53650

肖晖, 李建新, 韩伟, 等, 2013.鄂尔多斯盆地南缘渭北隆起中新生代构造抬升及演化.西安科技大学学报, 33(5):576-582, 593. http://www.cnki.com.cn/Article/CJFDTOTAL-XKXB201305014.htm

于强, 2009. 鄂尔多斯盆地南部中生界热演化史及其与多种能源关系研究(硕士学位论文). 西安: 西北大学, 33-41.

于强, 任战利, 倪军, 等, 2012.鄂尔多斯盆地富县地区中生界热演化史探讨.西北大学学报(自然科学版), 42(5):801-805. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xbdxxb201205020

袁万明, 王世成, 王兰芬, 2001.裂变径迹分析法研究河北南梁金矿床成矿时代及其热历史.矿物学报, 21(2):225-230. http://www.cnki.com.cn/Article/CJFDTOTAL-KWXB200102020.htm

周翔, 何生, 陈召佑, 等, 2016.鄂尔多斯盆地南部延长组层序地层格架中烃源岩特征及控制因素.地球科学, 41(6):1055-1066. https://doi.org/10.3799/dqkx.2016.087

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Exhumation, Cooling and Erosion History of Triassic Oil Shale since Late Cretaceous, Binxian-Tongchuan Area of Ordos Basin

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