Institute of Geomechanics, Chinese Academy of Geological SciencesHost
Advanced Search
Previous Article Next Article
2023 Vol. 29, No. 5
Article Contents
Article navigation > Journal of Geomechanics > 2023 > 29(5): 599-617
Next Article Previous Article

TIAN Zhaoyang, CHEN Hong, LIU Xinshe, GONG Wangbin, ZHAO Weibo, KANG Rui. 2023. Fission track ages and Mesozoic tectonic uplift in the Niushoushan-Luoshan area on the western edge of the Ordos Basin. Journal of Geomechanics, 29(5): 599-617. doi: 10.12090/j.issn.1006-6616.2023030
Citation: TIAN Zhaoyang, CHEN Hong, LIU Xinshe, GONG Wangbin, ZHAO Weibo, KANG Rui. 2023. Fission track ages and Mesozoic tectonic uplift in the Niushoushan-Luoshan area on the western edge of the Ordos Basin. Journal of Geomechanics, 29(5): 599-617. doi: 10.12090/j.issn.1006-6616.2023030
shu

Fission track ages and Mesozoic tectonic uplift in the Niushoushan-Luoshan area on the western edge of the Ordos Basin

  • 1.

    School of Earth Sciences and Resources, China University of Geosciences (Beijing), Beijing 100083, China

  • 2.

    Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

  • 3.

    Reasearch Center of Polar Geosciences, China Geological Survey, Beijing 100081, China

  • 4.

    Institute of Exploration and Development, Changqing Oilfield Company, PetroChina, Xi'an 710018, Shaanxi, China

  • 5.

    Key Laboratory of Paleomagnetism and Tectonic Reconstruction of Ministry of Natural Resources, Beijing 100081, China

    • Fund Project: This research is financially supported by the Geological Survey Project of the China Geological Survey (Grant No.DD20221644), the Fund of the National Natural Science Foundation of China (Grant No.41472195) and the Prospective and Fundamental Science and Technology Project of PetoChina (Grant No.2021DJ2101)
More Information
Received Date:  07 March 2023
Revised Date:  21 June 2023
Publish Date:  28 October 2023
    Abstract

  • The western margin of the Ordos Basin and its adjacent regions have undergone a complex tectonic evolution from the Mesozoic to the Cenozoic era. However, the question of tectonic uplift since the Cenozoic era remains a topic of contention, and the regional thermal evolution history necessitates precise chronological evidence. Situated close to the thrust belt within the western margin of the Ordos Basin, the Niushoushan-Luoshan area holds pivotal significance in unraveling the Mesozoic tectonic events within the basin's confines. Through a meticulous exploration employing apatite fission track (AFT) analysis and thermal history simulation, this study delineates the Mesozoic uplift sequence and its temporal confines in the Niushoushan-Luoshan area. The results reveal that the Mesozoic uplift within this region predominantly occurred during the Middle Jurassic period (170 Ma) to the end of the Early Cretaceous (110 Ma). Furthermore, we observe a slightly earlier onset of uplift in the Luoshan area (170 Ma) compared to the Niushoushan area (160 Ma). This uplift is primarily attributed to the north-eastward extrusion of the Qilian orogenic belt. Combining our findings with existing research, we propose that the Cenozoic uplift in the western margin of the Ordos Basin and its adjacent areas started during the Late Triassic, comprising two distinct phases: the first phase unfolding from the Late Triassic (220 Ma) to the end of the Early Jurassic (185 Ma), and the second phase occurring from the Middle Jurassic (175 Ma) to the end of the Early Cretaceous (110 Ma); the uplift in the Niushoushan-Luoshan area is part of the second phase of uplift along the western margin of the Ordos Basin. The two Cenozoic tectonic uplift phases along the western margin of the Ordos Basin display characteristics of north-to-south and southwest-to-northeast propagation, respectively. It is inferred to be associated with the Late Triassic collision between the North China and South China blocks, as well as the movement of the Lhasa Block converging toward the northeast during the Middle to Late Jurassic.

    • FullText(HTML)
  • 加载中
    • References
  • BAI D L, 2021. Characteristics and genetic mechanisms of intraplate tectonic deformation in the western Ordos Basin[D]. Beijing: China University of Petroleum. (in Chinese with English abstract)

    Google Scholar

    CHEN G, SUN J B, ZHOU L F, et al., 2007. Fission-track-age records of the Mesozoic tectonic-events in the southwest margin of the Ordos Basin, China[J]. Science in China Series D: Earth Sciences, 50(S2): 133-143. doi: 10.1007/s11430-007-6025-y

    CrossRef Google Scholar

    CHEN H, HU J M, GONG W B, et al., 2013. Cenozoic deformation and evolution of the Niushou Shan-Luo Shan fault zone in the northeast margin of the Tibet Plateau[J]. Earth Science Frontiers, 20(4): 18-35. (in Chinese with English abstract)

    Google Scholar

    CHEN H, HU J M, GONG W B, et al., 2015. Characteristics and transition mechanism of late Cenozoic structural deformation within the Niushoushan-Luoshan fault zone at the northeastern margin of the Tibetan Plateau[J]. Journal of Asian Earth Sciences, 114: 73-88. doi: 10.1016/j.jseaes.2015.06.034

    CrossRef Google Scholar

    CHENG L Y, TANG X Y, LI Y, 2021. Research progress of factors affecting apatite fission track annealing[J]. Journal of Geomechanics, 27(1): 127-134. (in Chinese with English abstract)

    Google Scholar

    DARBY B J, RITTS B D, 2002. Mesozoic contractional deformation in the middle of the Asian tectonic collage: the intraplate Western Ordos fold-thrust belt, China[J]. Earth and Planetary Science Letters, 205(1-2): 13-24. doi: 10.1016/S0012-821X(02)01026-9

    CrossRef Google Scholar

    DONG S W, ZHANG Y Q, LONG C X, et al., 2007. Jurassic tectonic revolution in China and new interpretation of the Yanshan Movement[J]. Acta Geologica Sinica, 81(11): 1449-1461. (in Chinese with English abstract) doi: 10.3321/j.issn:0001-5717.2007.11.001

    CrossRef Google Scholar

    DONG S W, ZHANG Y Q, CHEN X H, et al., 2008. The formation and deformational characteristics of East Asia multi-direction convergent tectonic system in Late Jurassic[J]. Acta Geoscientica Sinica, 29(3): 306-317. (in Chinese with English abstract)

    Google Scholar

    DONG S W, ZHANG Y Q, LI H L, et al., 2019. The Yanshan orogeny and late Mesozoic multi-plate convergence in East Asia: Commemorating 90th years of the "Yanshan Orogeny"[J]. Science China Earth Sciences, 61(12): 1888-1909.

    Google Scholar

    DONG Y P, LIU X M, ZHANG G W, et al., 2012. Triassic diorites and granitoids in the Foping area: Constraints on the conversion from subduction to collision in the Qinling orogen, China[J]. Journal of Asian Earth Sciences, 47: 123-142. doi: 10.1016/j.jseaes.2011.06.005

    CrossRef Google Scholar

    DUVALL A R, CLARK M K, KIRBY E, et al., 2013. Low-temperature thermochronometry along the Kunlun and Haiyuan Faults, NE Tibetan Plateau: Evidence for kinematic change during late-stage orogenesis[J]. Tectonics, 32(5): 1190-1211. doi: 10.1002/tect.20072

    CrossRef Google Scholar

    GALLAGHER K, 2012. Transdimensional inverse thermal history modeling for quantitative thermochronology[J]. Journal of Geophysical Research: Solid Earth, 117(B2): B02408.

    Google Scholar

    GAO F, WANG Y J, LIU S S, et al., 2000. Thermal history study in the west of the Ordos Basin using Apatite Fission Track analysis[J]. Geotectonica Et Metallogenia, 24(1): 87-91. (in Chinese with English abstract)

    Google Scholar

    GAO S H, 2014. Mesozoic and Cenozoic tectonic evolution of the transverse structure in the middle of west margin of Ordos Basin and its significance to oil and gas accumulation[D]. Xi'an: Northwest University. (in Chinese with English abstract)

    Google Scholar

    GE X H, 1989. The history of formation of intraplate orogenic belts in the north China paleoplate[J]. Geological Review, 35(3): 254-261. (in Chinese with English abstract)

    Google Scholar

    GONG W B, SHI W, CHEN H, et al., 2016. Quaternary active characteristics of the Liumugao fault in the northern segment of the Niushoushan-Luoshan fault[J]. Journal of Geomechanics, 22(4): 1004-1014. (in Chinese with English abstract)

    Google Scholar

    GREEN P F, 1986. On the thermo-tectonic evolution of northern England: evidence from fission track analysis[J]. Geological Magazine, 123(5): 493-506. doi: 10.1017/S0016756800035081

    CrossRef Google Scholar

    GU Q C, 1996. Stratigraphy(Lithostratic) of Ningxia Hui autonomous region[M]. Wuhan: China University of Geosciences Press. (in Chinese with English abstract)

    Google Scholar

    GUO P, LIU C Y, WANG J Q, et al., 2018. Detrital-zircon geochronology of the Jurassic coal-bearing strata in the western Ordos Basin, North China: Evidences for multi-cycle sedimentation[J]. Geoscience Frontiers, 9(6): 1725-1743. doi: 10.1016/j.gsf.2017.11.003

    CrossRef Google Scholar

    GUO Q Y, 2010. Tectonic evolution at the western margin of Ordos Basin with respect to metallogenesis of sandstone type uranium deposits[D]. Beijing: China University of Geosciences (Beijing). (in Chinese with English abstract)

    Google Scholar

    GUO R H, LI S Z, SUO Y H, et al., 2017. Indentation of North China Block into Greater South China Block and Indosinian Orocline[J]. Earth Science Frontiers, 24(4): 171-184. (in Chinese with English abstract)

    Google Scholar

    HE P J, SONG C H, WANG Y D, et al., 2017. Cenozoic exhumation in the Qilian Shan, northeastern Tibetan Plateau: Evidence from detrital fission track thermochronology in the Jiuquan Basin[J]. Journal of Geophysical Research: Solid Earth, 122(8): 6910-6927. doi: 10.1002/2017JB014216

    CrossRef Google Scholar

    HE Z J, LI J Y, NIU B G, et al., 1998. A Late Jurassic intense thrusting-uplifting event in the Yanshan-Yinshan area, Northern China, and its sedimentary response[J]. Geological Review, 44(4): 407-418. (in Chinese with English abstract)

    Google Scholar

    HURFORD A J, GREEN P F, 1982. A users' guide to fission track dating calibration[J]. Earth and Planetary Science Letters, 59(2): 343-354. doi: 10.1016/0012-821X(82)90136-4

    CrossRef Google Scholar

    KETCHAM R A, 2005. Forward and inverse modeling of low-temperature thermochronometry data[J]. Reviews in Mineralogy and Geochemistry, 58(1): 275-314. doi: 10.2138/rmg.2005.58.11

    CrossRef Google Scholar

    KETCHAM R A, CARTER A, DONELICK R A, et al., 2007a. Improved measurement of fission-track annealing in apatite using c-axis projection[J]. American Mineralogist, 92(5-6): 789-798. doi: 10.2138/am.2007.2280

    CrossRef Google Scholar

    KETCHAM R A, CARTER A, DONELICK R A, et al., 2007b. Improved modeling of fission-track annealing in apatite[J]. American Mineralogist, 92(5-6): 799-810. doi: 10.2138/am.2007.2281

    CrossRef Google Scholar

    KOHN B P, GREEN P F, 2002. Low temperature thermochronology: from tectonics to landscape evolution[J]. Tectonophysics, 349(1-4): 1-4. doi: 10.1016/S0040-1951(02)00042-2

    CrossRef Google Scholar

    KOU L L, LI Z H, DONG X P, et al., 2021. The age sequence of the detrital zircons from the Guanyindian section in Longde, the northeastern margin of the Tibetan Plateau, and its geological significance[J]. Journal of Geomechanics, 27(6): 1051-1064. (in Chinese with English abstract)

    Google Scholar

    LEI Q Y, ZHANG P Z, ZHENG W J, et al., 2016. Dextral strike-slip of Sanguankou-Niushoushan fault zone and extension of arc tectonic belt in the northeastern margin of the Tibet Plateau[J]. Science China Earth Sciences, 59(5): 1025-1040. doi: 10.1007/s11430-016-5272-1

    CrossRef Google Scholar

    LI B, 2019. Thrust structure and its effect on hydrocarbon in the western margin of Ordos Basin[D]. Xi'an: Northwest University. (in Chinese with English abstract)

    Google Scholar

    LI F Q, ZHANG S Z, LI J, et al., 2022. Definition of Mid-Late Jurassic Peripheral Foreland Basin in the northern margin of Lhasa Block[J]. Earth Science, 47(2): 387-404. (in Chinese with English abstract)

    Google Scholar

    LI S Z, SUO Y H, ZHOU J, et al., 2022. Tectonic evolution of the South China Ocean-Continent Connection Zone: Transition and mechanism of the Tethyan to the Pacific tectonic domains[J]. Journal of Geomechanics, 28(5): 683-704. (in Chinese with English abstract)

    Google Scholar

    LI Y H, DU X X, LI T X, 2022. Characterization of the Holocene extensional structures in the Wuwei Basin, northeastern margin of the Tibetan Plateau, and their formation mechanism[J]. Journal of Geomechanics, 28(3): 353-366. (in Chinese with English abstract)

    Google Scholar

    LIANG W T, ZHANG G W, LU R K, et al., 2013. Extrusion tectonics inferred from fabric study of the Guanzizhen ophiolitic mélange belt in the West Qinling orogen, Central China[J]. Journal of Asian Earth Sciences, 78: 345-357. doi: 10.1016/j.jseaes.2013.07.006

    CrossRef Google Scholar

    LIN X B, CHEN H L, WYRWOLL K H, et al., 2011. The uplift history of the Haiyuan-Liupan Shan region northeast of the present Tibetan Plateau: Integrated constraint from stratigraphy and thermochronology[J]. The Journal of Geology, 119(4): 372-393. doi: 10.1086/660190

    CrossRef Google Scholar

    LIU C Y, ZHAO H G, WANG F, et al., 2005. Attributes of the Mesozoic structure on the west margin of the Ordos Basin[J]. Acta Geologica Sinica, 79(6): 737-747. (in Chinese with English abstract)

    Google Scholar

    LIU J H, 2009. Apatite Fission Track (AFT) Analysis of the Cenozoic Extensional Exhumation and Uplift of the Helan Shan and the Qinling Mountains, and Frictional Heating along Active Faults[D]. Beijing: Institute of Geology, China Earthquake Administrator. (in Chinese with English abstract)

    Google Scholar

    MA J H, HE D F, 2019. Meso-Cenozoic tectonic events in the Helanshan Tectonic Belt and its adjacent areas: Constraints from unconformity and fission track data[J]. Acta Petrologica Sinica, 35(4): 1121-1142. (in Chinese with English abstract) doi: 10.18654/1000-0569/2019.04.10

    CrossRef Google Scholar

    MA X H, XING L S, YANG Z Y, et al., 1993. Paleomagnetic study since Late Paleozoic in The Ordos Basin[J]. Acta Geophysica Sinica, 36(1): 68-79. (in Chinese with English abstract)

    Google Scholar

    MA Y S, 2003. The neotectonic activity and the evaluation of geological hazards risk in the upper reaches of the Yellow River[M]. Beijing: Geology Press, 1-278. (in Chinese with English abstract)

    Google Scholar

    MENG Q R, ZHANG G W, 1999. Timing of collision of the North and South China blocks: controversy and reconciliation[J]. Geology, 27(2): 123-126. doi: 10.1130/0091-7613(1999)027<0123:TOCOTN>2.3.CO;2

    CrossRef Google Scholar

    MIN W, CHAI Z Z, WANG P, et al., 1993. The study on the paleoearthquakes on the eastern piedmont fault of the Luoshan mountains in Holocene[J]. Plateau Earthquake Research, 5(4): 97-102. (in Chinese with English abstract)

    Google Scholar

    OUYANG Z J, CHEN H D, FENG J P, 2012. Structural characters and evolution of the mid-south section at the west margin of Ordos Basin[J]. Geoscience, 26(4): 691-695. (in Chinese with English abstract)

    Google Scholar

    PENG H, WANG J Q, ZATTIN M, et al., 2018. Late Triassic-Early Jurassic uplifting in Eastern Qilian Mountain and its geological significance: Evidence from apatite fission track thermochronology[J]. Earth Science, 43(6): 1983-1996. (in Chinese with English abstract)

    Google Scholar

    PENG H, WANG J Q, LIU C Y, et al., 2019. Thermochronological constraints on the Meso-Cenozoic tectonic evolution of the Haiyuan-Liupanshan region, northeastern Tibetan Plateau[J]. Journal of Asian Earth Sciences, 183: 103966. doi: 10.1016/j.jseaes.2019.103966

    CrossRef Google Scholar

    PENG H, 2020. Fission-track thermochronological analysis and its geological significance in the southwestern Ordos Block and its surroundings[D]. Xi'an: Northwest University. (in Chinese with English abstract)

    Google Scholar

    PENG H, LIU X Y, LIU C Y, et al., 2022. Spatial-temporal evolution and the dynamic background of the translation of Mid-Late Mesozoic tectonic regimes of the southwest Ordos basin margin[J]. Acta Geologica Sinica, 96(2): 387-402. (in Chinese with English abstract)

    Google Scholar

    REN J S, JIANG C F, ZHANG Z K, et al., 1980. Geotectonic evolution of China[M]. Beijing: Science Press, 10-65. (in Chinese with English abstract)

    Google Scholar

    REN W J, ZHANG Q L, ZHANG J, et al., 1999. The plate tectonic formation of the Central Paleo Uplift in The Ordos Basin[J]. Geotectonica et Metallogenia, 23(2): 191-196. (in Chinese with English abstract)

    Google Scholar

    RUAN Z, LUO Z, YU B S, et al., 2021. Middle-Late Triassic basin prototype and tectonic paleographic response in the Ordos Basin[J]. Earth Science Frontiers, 28(1): 12-32. (in Chinese with English abstract)

    Google Scholar

    SONG L J, MU Q H, LI A R, et al., 2013. Fission-track thermal evolution history in the formation age of Yaoshan Formation[J]. Coal Geology & Exploration, 41(4): 1-4. (in Chinese with English abstract)

    Google Scholar

    SONG Y G, FANG X M, LI J J, et al., 2001. The Late Cenozoic uplift of the Liupan Shan, China[J]. Science in China Series D: Earth Sciences, 44(S1): 176-184. doi: 10.1007/BF02911985

    CrossRef Google Scholar

    SONG Y G, QIAN L B, LI Y, 2013. Fission track evidence of tectonic uplift in Liupanshan area since cretaceous[C]//Proceedings of the First National Youth Geological Congress. Fuzhou: 121-124. (in Chinese)

    Google Scholar

    TANG X Y, GUO Z M, 1992. The study and petroleum prospect of thrust nappe in the west margin of Shanxi-Gansu-Ningxia Basin[M]. Xi'an: Northwest University Press. (in Chinese with English abstract)

    Google Scholar

    WANG J Q, JIA N, LIU C Y, et al., 2011. Fabric analysis of Yijun gravels of Lower Cretaceous in the southwestern Ordos Basin[J]. Acta Sedimentologica Sinica, 29(2): 226-234. (in Chinese with English abstract)

    Google Scholar

    WANG J Q, LIU C Y, ZHAO H G, et al., 2020. Uplift and exhumation events and thermochronological constraints at the end of Triassic in southwestern Ordos Basin[J]. Acta Petrologica Sinica, 36(4): 1199-1212. (in Chinese with English abstract) doi: 10.18654/1000-0569/2020.04.14

    CrossRef Google Scholar

    WANG Q, ZHANG P Z, FREYMUELLER J T, et al., 2001. Present-day crustal deformation in China constrained by global positioning system measurements[J]. Science, 294(5542): 574-577. doi: 10.1126/science.1063647

    CrossRef Google Scholar

    WANG W T, ZHANG P Z, KIRBY E, et al., 2011. A revised chronology for Tertiary sedimentation in the Sikouzi basin: Implications for the tectonic evolution of the northeastern corner of the Tibetan Plateau[J]. Tectonophysics, 505(1-4): 100-114. doi: 10.1016/j.tecto.2011.04.006

    CrossRef Google Scholar

    WANG W T, ZHANG P Z, LEI Q Y, 2013. Deformational characteristics of the Niushoushan-Luoshan fault zone and its tectonic implications[J]. Seismology and Geology, 35(2): 195-207. (in Chinese with English abstract)

    Google Scholar

    WANG W T, ZHANG P Z, ZHENG D W, et al., 2014. Late Cenozoic tectonic deformation of the Haiyuan fault zone in the northeastern margin of the Tibetan Plateau[J]. Earth Science Frontiers, 21(4): 266-274. (in Chinese with English abstract)

    Google Scholar

    XU L Q, LI S Z, GUO L L, et al., 2016. Impaction of the Tan-Lu Fault Zone on uplift of the Luxi Rise: Constraints from apatite fission track thermochronology[J]. Acta Petrologica Sinica, 32(4): 1153-1170. (in Chinese with English abstract)

    Google Scholar

    YANG Z Y, BESSE J, 2000. Early Triassic paleomagnetic results from southern part of the Sichuan Basin and its tectonic implications[J]. Chinese Journal of Geology, 35(1): 77-82. (in Chinese with English abstract)

    Google Scholar

    YUAN W M, BAO Z K, DONG J Q, et al., 2007. Zircon and apatite fission track analyses on mineralization ages and tectonic activities of Tuwu-Yandong porphyry copper deposit in northern Xinjiang, China[J]. Science in China Series D: Earth Sciences, 50(12): 1787-1795. doi: 10.1007/s11430-007-0130-9

    CrossRef Google Scholar

    ZHANG H, JIN X L, LI G H, et al., 2008. Original features and palaeogeographic evolution during the Jurassic-Cretaceous in Ordos Basin[J]. Journal of Palaeogeography, 10(1): 1-11. (in Chinese with English abstract)

    Google Scholar

    ZHANG J, MA Z J, REN W J, 2000. The mechanism of the difference between the northern part and the southern part of the fold and thrust belt on the Western edge of The Ordos Basin, China[J]. Geotectonica et Metallogenia, 24(2): 124-133. (in Chinese with English abstract)

    Google Scholar

    ZHANG J, MA Z J, REN W J, 2004. Tectonic characteristics of the western Ordos thrust-fold belt and the causes for its north-south segmentation[J]. Acta Geologica Sinica, 78(5): 600-611. (in Chinese with English abstract)

    Google Scholar

    ZHANG L, LIU C Y, HE X Y, 2019. Discovery of kilometer-scale uplift and exhumation related to the Late Indosinian movement in the northern Ordos Basin, North China[J]. Acta Geologica Sinica-English Edition, 93(1): 231-232. doi: 10.1111/1755-6724.13793

    CrossRef Google Scholar

    ZHANG P Z, SHEN Z K, WANG M, et al., 2004. Continuous deformation of the Tibetan plateau from global positioning system data[J]. Geology, 32(9): 809-812. doi: 10.1130/G20554.1

    CrossRef Google Scholar

    ZHANG S H, LIU C Y, YANG M H, et al., 2018. Latest Triassic to Early Jurassic thrusting and exhumation in the southern Ordos Basin, North China: Evidence from LA-ICP-MS-based apatite fission track thermochronology[J]. Acta Geologica Sinica-English Edition, 92(4): 1334-1348. doi: 10.1111/1755-6724.13630

    CrossRef Google Scholar

    ZHANG W J, MENG X X, HU J M, et al., 1994. Tectonic characteristics and orogenic process of the junction of the Qilian-North Qinling orogenic belt[M]. Xi'an: Northwest University Press, 1-150. (in Chinese t).

    Google Scholar

    ZHANG Y Q, LIAO C Z, 2006. Transition of the Late Mesozoic-Cenozoic tectonic regimes and modification of the Ordos basin[J]. Geology in China, 33(1): 28-40. (in Chinese with English abstract)

    Google Scholar

    ZHANG Z C, WANG X S, 2004. The issues of application for the fission track dating and its geological significance[J]. Acta Scicentiarum Naturalum Universitis Pekinesis, 40(6): 898-905. (in Chinese with English abstract)

    Google Scholar

    ZHAO H G, 2003. Structural characteristics and the evolution in western Ordos Basin[D]. Xi'an: Northwest University. (in Chinese with English abstract)

    Google Scholar

    ZHAO H G, LIU C Y, WANG F, et al., 2007a. Uplift and evolution of Helan Mountain[J]. Science in China Series D: Earth Sciences, 50(S2): 217-226. doi: 10.1007/s11430-007-6010-5

    CrossRef Google Scholar

    ZHAO H G, LIU C Y, YAO Y M, et al., 2007b. Differential uplift in the west margin of Ordos Basin since Mesozoic from the fission track evidence[J]. Journal of Northwest University(Natural Science Edition), 37(3): 470-474. (in Chinese with English abstract)

    Google Scholar

    ZHAO X C, LIU C Y, WANG J Q, et al., 2016. Mesozoic-Cenozoic tectonic uplift events of Xiangshan Mountain in northern North-South Tectonic Belt, China[J]. Acta Petrologica Sinica, 32(7): 2124-2136. (in Chinese with English abstract)

    Google Scholar

    ZHAO X C, 2017. Mesozoic tectonic evolution and late reformation of the Northern North-South Tectonic Belt, China[D]. Xi'an: Northwest University. (in Chinese with English abstract)

    Google Scholar

    ZHAO Y, GAO H L, ZHANG S H, et al., 2022. A brief century review of the "Yanshan Movement" and its founder[J]. Acta Geologica Sinica, 96(5): 1510-1523. (in Chinese with English abstract)

    Google Scholar

    ZHENG D W, ZHANG P Z, WAN J L, et al., 2006. Rapid exhumation at ~8 Ma on the Liupan Shan thrust fault from apatite fission-track thermochronology: Implications for growth of the northeastern Tibetan Plateau margin[J]. Earth and Planetary Science Letters, 248(1-2): 198-208. doi: 10.1016/j.epsl.2006.05.023

    CrossRef Google Scholar

    ZHU G S, 2015. Analysis of Meso-Cenozic structural characteristics and prediction of favorable oil and gas zone in Liupanshan Basin[D]. Xi'an: Chang'an University. (in Chinese with English abstract)

    Google Scholar

    白东来, 2021. 鄂尔多斯盆地西缘板内构造变形特征及其成因机制[D]. 北京: 中国石油大学(北京).

    Google Scholar

    陈刚, 孙建博, 周立发, 等, 2007. 鄂尔多斯盆地西南缘中生代构造事件的裂变径迹年龄记录[J]. 中国科学(D辑: 地球科学), 37(S1): 110-118.

    Google Scholar

    陈虹, 胡健民, 公王斌, 等, 2013. 青藏高原东北缘牛首山-罗山断裂带新生代构造变形与演化[J]. 地学前缘, 20(4): 18-35.

    Google Scholar

    程璐瑶, 唐晓音, 李毅, 2021. 磷灰石裂变径迹退火影响因素研究进展[J]. 地质力学学报, 27(1): 127-134.

    Google Scholar

    董树文, 张岳桥, 龙长兴, 等, 2007. 中国侏罗纪构造变革与燕山运动新诠释[J]. 地质学报, 81(11): 1449-1461.

    Google Scholar

    董树文, 张岳桥, 陈宣华, 等, 2008. 晚侏罗世东亚多向汇聚构造体系的形成与变形特征[J]. 地球学报, 29(3): 306-317.

    Google Scholar

    董树文, 张岳桥, 李海龙, 等, 2019. "燕山运动"与东亚大陆晚中生代多板块汇聚构造: 纪念"燕山运动"90周年[J]. 中国科学: 地球科学, 49(6): 913-938.

    Google Scholar

    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[J]. 大地构造与成矿学, 24(1): 87-91.

    Google Scholar

    高少华, 2014. 鄂尔多斯盆地西缘中部横向构造带中新生代演化改造及其油气意义[D]. 西安: 西北大学.

    Google Scholar

    葛肖虹, 1989. 华北板内造山带的形成史[J]. 地质论评, 35(3): 254-261.

    Google Scholar

    公王斌, 施炜, 陈虹, 等, 2016. 牛首山-罗山断裂带北段柳木高断裂第四纪活动特征[J]. 地质力学学报, 22(4): 1004-1014.

    Google Scholar

    顾其昌, 1996. 宁夏回族自治区岩石地层[M]. 武汉: 中国地质大学出版社.

    Google Scholar

    郭庆银, 2010. 鄂尔多斯盆地西缘构造演化与砂岩型铀矿成矿作用[D]. 北京: 中国地质大学(北京).

    Google Scholar

    郭润华, 李三忠, 索艳慧, 等, 2017. 华北地块揳入大华南地块和印支期弯山构造[J]. 地学前缘, 24(4): 171-184.

    Google Scholar

    和政军, 李锦轶, 牛宝贵, 等, 1998. 燕山—阴山地区晚侏罗世强烈推覆—隆升事件及沉积响应[J]. 地质论评, 44(4): 407-418.

    Google Scholar

    寇琳琳, 李振宏, 董晓朋, 等, 2021. 青藏高原东北缘隆德观音店剖面碎屑锆石年龄序列及地质意义[J]. 地质力学学报, 27(6): 1051-1064.

    Google Scholar

    雷启云, 张培震, 郑文俊, 等, 2016. 青藏高原东北缘三关口-牛首山断裂的右旋走滑与弧形构造带扩展[J]. 中国科学: 地球科学, 46(5): 691-705.

    Google Scholar

    李斌, 2019. 鄂尔多斯盆地西部冲断带构造与控油气因素研究[D]. 西安: 西北大学.

    Google Scholar

    李奋其, 张士贞, 李俊, 等, 2022. 拉萨地块北缘中晚侏罗世周缘前陆盆地的厘定[J]. 地球科学, 47(2): 387-404.

    Google Scholar

    李三忠, 索艳慧, 周洁, 等, 2022. 华南洋陆过渡带构造演化: 特提斯构造域向太平洋构造域的转换过程与机制[J]. 地质力学学报, 28(5): 683-704.

    Google Scholar

    李艺豪, 杜星星, 李天秀, 2022. 青藏高原东北缘武威盆地内部全新世伸展构造特征及其成因机制[J]. 地质力学学报, 28(3): 353-366.

    Google Scholar

    刘池洋, 赵红格, 王锋, 等, 2005. 鄂尔多斯盆地西缘(部)中生代构造属性[J]. 地质学报, 79(6): 737-747.

    Google Scholar

    刘建辉, 2009. 贺兰山、秦岭山脉新生代伸展隆升及断层摩擦生热磷灰石裂变径迹分析[D]. 北京: 中国地震局地质研究所.

    Google Scholar

    马静辉, 何登发, 2019. 贺兰山构造带及邻区中—新生代构造事件: 来自不整合面和裂变径迹的约束[J]. 岩石学报, 35(4): 1121-1142.

    Google Scholar

    马醒华, 邢历生, 杨振宇, 等, 1993. 鄂尔多斯盆地晚古生代以来古地磁研究[J]. 地球物理学报, 36(1): 68-79.

    Google Scholar

    马寅生, 2003. 黄河上游新构造活动与地质灾害风险评价[M]. 北京: 地质出版社, 1-278.

    Google Scholar

    闵伟, 柴炽章, 王萍, 等, 1993. 罗山东麓断裂全新世古地震研究[J]. 高原地震, 5(4): 97-102.

    Google Scholar

    欧阳征健, 陈洪德, 冯娟萍, 2012. 鄂尔多斯盆地西缘中南段构造特征与演化[J]. 现代地质, 26(4): 691-695.

    Google Scholar

    彭恒, 王建强, ZATTIN M, 等, 2018. 晚三叠世—早侏罗世祁连山东部隆升的裂变径迹年代学证据及地质意义[J]. 地球科学, 43(6): 1983-1996.

    Google Scholar

    彭恒, 2020. 鄂尔多斯地块西南邻区裂变径迹热年代学分析及地质意义[D]. 西安: 西北大学.

    Google Scholar

    彭恒, 刘显阳, 刘池洋, 等, 2022. 鄂尔多斯盆地西南缘中生代中晚期构造体制转化过程及其动力学背景[J]. 地质学报, 96(2): 387-402.

    Google Scholar

    任纪舜, 姜春发, 张正坤, 等, 1980. 中国大地构造及其演化[M]. 北京: 科学出版社, 10-65.

    Google Scholar

    任文军, 张庆龙, 张进, 等, 1999. 鄂尔多斯盆地中央古隆起板块构造成因初步研究[J]. 大地构造与成矿学, 23(2): 191-196.

    Google Scholar

    阮壮, 罗忠, 于炳松, 等, 2021. 鄂尔多斯盆地中—晚三叠世盆地原型及构造古地理响应[J]. 地学前缘, 28(1): 12-32.

    Google Scholar

    宋立军, 牟秋环, 李爱荣, 等, 2013. 宁夏固原炭山窑山组形成时代的裂变径迹热史约束[J]. 煤田地质与勘探, 41(4): 1-4.

    Google Scholar

    宋友桂, 方小敏, 李吉均, 等, 2001. 晚新生代六盘山隆升过程初探[J]. 中国科学: D辑, 31(增刊): 142-148.

    Google Scholar

    宋友桂, 千琳勃, 李云, 2013. 白垩纪以来六盘山地区构造隆升的裂变径迹证据[C]//第一届全国青年地质大会论文集. 福州: 121-124.

    Google Scholar

    汤锡元, 郭忠铭, 1992. 陕甘宁盆地西缘逆冲推覆构造及油气勘探[M]. 西安: 西北大学出版社.

    Google Scholar

    王建强, 贾楠, 刘池洋, 等, 2011. 鄂尔多斯盆地西南部下白垩统宜君组砾岩砾组分析及其意义[J]. 沉积学报, 29(2): 226-234.

    Google Scholar

    王建强, 刘池洋, 赵红格, 等, 2020. 鄂尔多斯盆地西南部三叠纪末抬升剥蚀事件及热年代学记录[J]. 岩石学报, 36(4): 1199-1212.

    Google Scholar

    王伟涛, 张培震, 雷启云, 2013. 牛首山-罗山断裂带的变形特征及其构造意义[J]. 地震地质, 35(2): 195-207.

    Google Scholar

    王伟涛, 张培震, 郑德文, 等, 2014. 青藏高原东北缘海原断裂带晚新生代构造变形[J]. 地学前缘, 21(4): 266-274.

    Google Scholar

    许立青, 李三忠, 郭玲莉, 等, 2016. 郯庐断裂带对鲁西隆升过程的影响: 磷灰石裂变径迹证据[J]. 岩石学报, 32(4): 1153-1170.

    Google Scholar

    杨振宇, BESSE J, 2000. 四川盆地南缘早三叠世古地磁结果及其构造意义[J]. 地质科学, 35(1): 77-82.

    Google Scholar

    袁万明, 保增宽, 董金泉, 等, 2007. 新疆土屋—延东斑岩铜矿区成矿时代与构造活动的裂变径迹分析[J]. 中国科学D辑: 地球科学, 37(10): 1330-1337.

    Google Scholar

    张泓, 晋香兰, 李贵红, 等, 2008. 鄂尔多斯盆地侏罗纪—白垩纪原始面貌与古地理演化[J]. 古地理学报, 10(1): 1-11.

    Google Scholar

    张进, 马宗晋, 任文军, 2000. 鄂尔多斯盆地西缘逆冲带南北差异的形成机制[J]. 大地构造与成矿学, 24(2): 124-133.

    Google Scholar

    张进, 马宗晋, 任文军, 2004. 鄂尔多斯西缘逆冲褶皱带构造特征及其南北差异的形成机制[J]. 地质学报, 78(5): 600-611.

    Google Scholar

    张维吉, 孟宪恂, 胡建民, 等, 1994. 祁连山-北秦岭造山带接合部位构造特征与造山过程[M]. 西安: 西北大学出版社, 1-150.

    Google Scholar

    张岳桥, 廖昌珍, 2006. 晚中生代—新生代构造体制转换与鄂尔多斯盆地改造[J]. 中国地质, 33(1): 28-40.

    Google Scholar

    张志诚, 王雪松, 2004. 裂变径迹定年资料应用中的问题及其地质意义[J]. 北京大学学报(自然科学版), 40(6): 898-905.

    Google Scholar

    赵红格, 2003. 鄂尔多斯盆地西部构造特征及演化[D]. 西安: 西北大学.

    Google Scholar

    赵红格, 刘池洋, 王锋, 等, 2007a. 贺兰山隆升时限及其演化[J]. 中国科学D辑: 地球科学, 37(S1): 185-192.

    Google Scholar

    赵红格, 刘池洋, 姚亚明, 等, 2007b. 鄂尔多斯盆地西缘差异抬升的裂变径迹证据[J]. 西北大学学报(自然科学版), 37(3): 470-474.

    Google Scholar

    赵晓辰, 刘池洋, 王建强, 等, 2016. 南北构造带北部香山地区中—新生代构造抬升事件[J]. 岩石学报, 32(7): 2124-2136.

    Google Scholar

    赵晓辰, 2017. 中国南北构造带北部中生代构造演化与后期改造[D]. 西安: 西北大学.

    Google Scholar

    赵越, 高海龙, 张拴宏, 等, 2022. 回眸燕山运动: 致敬"燕山运动"的创建者和中国地质学会的奠基人翁文灏[J]. 地质学报, 96(5): 1510-1523.

    Google Scholar

    朱国胜, 2015. 六盘山盆地中新生代构造特征分析及有利油气区预测[D]. 西安: 长安大学.

    Google Scholar

    • Relative Articles
  • Cited by
  • Supplements
    • Proportional views
  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Figures(10)

Tables(3)

Export Citation
PDF
XML

Article Metrics

Article views(502) PDF downloads(31) Cited by(0)

Access History

Other Articles By Authors

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    版权所有：中国地质调查局发展研究中心 copyright @2020