Volume 27 Issue 6
Dec.  2021
Turn off MathJax
Article Contents
KOU Linlin, LI Zhenhong, DONG Xiaopeng, 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. Journal of Geomechanics, 27 (6): 1051-1064. DOI: 10.12090/j.issn.1006-6616.2021.27.06.085
Citation: KOU Linlin, LI Zhenhong, DONG Xiaopeng, 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. Journal of Geomechanics, 27 (6): 1051-1064. DOI: 10.12090/j.issn.1006-6616.2021.27.06.085

The age sequence of the detrital zircons from the Guanyindian section in Longde, the northeastern margin of the Tibetan Plateau, and its geological significance

doi: 10.12090/j.issn.1006-6616.2021.27.06.085
Funds:

the National Natural Science Foundation of China 41972119

the Geological Survey Project of China Geological Survey DD20190018

More Information
  • Received: 2021-04-25
  • Revised: 2021-08-11
  • The precise age of the strata at the northeastern margin of the Tibetan Plateau in the Paleogene-Neogene, and the initial time when the uplift of the Plateau affected its northeastern margin, have always been two main bone contentions among geologists. The Guanyindian section at the northeastern margin of the Tibetan Plateau is our research subject. We gain new insights to the two mentioned issues by using detrital zircon U-Pb dating in combination with the previous results concerning regional paleontological fossil identification and paleomagnetic dating. The dating results show, among the samples from the upper Paleogene Qingshuiying formation at the northeastern margin of the Tibetan Plateau, the youngest peak is 17.8 Ma. Two conclusions are drawn from the research results. Firstly, the deposition age of the Qingshui formation is from the late Oligecene to early Miocene, showing the characteristic of diachronism. Secondly, the northeastward extension and pushing of the uplift of the Tibetan Plateau has begun affecting the west of the Haiyuan-Liupanshan fault zone since the early Miocene with a coupling relationship among tectonics, sedimentation and climate in the area. The research findings provide a new time scale for determining the initial time when the northeastward pushing of the Tibetan Plateau began to affect its northeastern margin.

     

  • loading
  • AN Z S, SUN D H, CHEN M Y, et al., 2000. Red clay sequences in Chinese loess plateau and recorded paleoclimate events of the late tertiary[J]. Quaternary Sciences, 20(5): 435-446. (in Chinese with English abstract) http://www.oalib.com/paper/1572466
    AN Z S, KUTZBACH J E, PRELL W L, et al., 2001. Evolution of Asian monsoons and phased uplift of the Himalaya-Tibetan Plateau since late Miocene times[J]. Nature, 411(6833): 62-66. doi: 10.1038/35075035
    BIAN S, YU Z Q, GONG J F, et al., 2021. Spatiotemporal distribution and geodynamic mechanism of the nearly NS-trending rifts in the Tibetan Plateau[J]. Journal of Geomechanics, 27(2): 178-194. (in Chinese with English abstract) https://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20210203&journal_id=dzlxxb
    BURCHFIEL B C, ZHANG P Z, WANG Y P, et al., 1991. Geology of the Haiyuan fault zone, Ningxia Hui Autonomous Region, China, and its relation to the evolution of the northeastern margin of the Tibetan Plateau[J]. Tectonics, 10(6): 1091-1110. doi: 10.1029/90TC02685
    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) http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY201304004.htm
    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
    CHEN J L, LI H B, WANG H L, et al., 2007. LA-ICPMS zircon U-Pb dating of a quartz diorite pluton from Wangjiacha, the Junction area between the Qinling and Qilian Orogenic belts and its tectonic significance[J]. Journal of Jilin University (Earth Science Edition), 37(3): 423-431. (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-CCDZ200703001.htm
    Research China Seismological Bureau, 1988. Ordos peripheral active faults[M]. Beijing: Seismological Press. (in Chinese)
    CLARK M K, FARLEY K A, ZHENG D W, et al., 2010. Early Cenozoic faulting of the northern Tibetan Plateau margin from apatite (U-Th)/He ages[J]. Earth and Planetary Science Letters, 296(1-2): 78-88. doi: 10.1016/j.epsl.2010.04.051
    CUI J W, LI Z H, LIU F, et al., 2018. Redefinition of the sedimentary time of the Salawusu formation in the Hongsibu basin, Ningxia and its significance[J]. Journal of Geomechanics, 24(2): 283-292. (in Chinese with English abstract) https://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20180215&journal_id=dzlxxb
    DENG Q D, SUNG F, ZHU S L, et al., 1984. Active faulting and tectonics of the Ningxia-Hui autonomous region, China[J]. Journal of Geophysical Research (Solid Earth), 89(B6): 4427-4445. doi: 10.1029/JB089iB06p04427
    DING Z L, XIONG S F, SUN J M, et al., 1999. Pedostratigraphy and paleomagnetism of a~7.0 Ma eolian loess-red clay sequence at Lingtai, Loess Plateau, North-central China and the implications for paleomonsoon evolution[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 152(1-2): 49-66. doi: 10.1016/S0031-0182(99)00034-6
    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
    ENGLAND P, HOUSEMAN G, 1985. Role of lithospheric strength heterogeneities in the Tectonics of Tibet and neighbouring regions[J]. Nature, 315(6017): 297-301. doi: 10.1038/315297a0
    ENKELMANN E, RATSCHBACHER L, JONCKHEERE R, et al., 2006. Cenozoic exhumation and deformation of northeastern Tibet and the Qinling: is Tibetan lower crustal flow diverging around the Sichuan Basin?[J]. GSA Bulletin, 118(5-6): 651-671. doi: 10.1130/B25805.1
    FAN L G, MENG Q R, WU G L, et al., 2019. Paleogene crustal extension in the eastern segment of the NE Tibetan plateau[J]. Earth and Planetary Science Letters, 514: 62-74. doi: 10.1016/j.epsl.2019.02.036
    FANG X M, GARZIONE C, VAN DER VOO R, et al., 2003. Flexural subsidence by 29 Ma on the NE edge of Tibet from the magnetostratigraphy of Linxia Basin, China[J]. Earth and Planetary Science Letters, 210(3-4): 545-560. doi: 10.1016/S0012-821X(03)00142-0
    HU Z C, GAO S, LIU Y S, et al., 2008. Signal enhancement in laser ablation ICP-MS by addition of nitrogen in the central channel gas[J]. Journal of Analytical Atomic Spectrometry, 23(8): 1093-1101. doi: 10.1039/b804760j
    HU Z C, LIU Y S, GAO S, et al., 2012. A "wire" signal smoothing device for laser ablation inductively coupled plasma mass spectrometry analysis[J]. Spectrochimica Acta Part B: Atomic Spectroscopy, 78: 50-57. doi: 10.1016/j.sab.2012.09.007
    HUANG T, LI Z H, LIU F, et al., 2018. The current situation of desertification in the Hongsibu basin, Ningxia, and its main geological controlling factors[J]. Journal of Geomechanics, 24(4): 505-514. (in Chinese with English abstract) https://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20180408&journal_id=dzlxxb
    HUANG X F, FENG S Y, GAO R, et al., 2016. High-resolution crustal structure of the Yinchuan basin revealed by deep seismic reflection profiling: implications for deep processes of basin[J]. Earthquake Science, 29(2): 83-92. doi: 10.1007/s11589-016-0148-1
    JIANG H C, DING Z L, XIONG S F, 2007. Magnetostratigraphy of the Neogene Sikouzi section at Guyuan, Ningxia, China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 243(1-2): 223-234. doi: 10.1016/j.palaeo.2006.07.016
    JIANG H C, DING Z L, 2008. A 20 Ma pollen record of East-Asian summer monsoon evolution from Guyuan, Ningxia, China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 265(1-2): 30-38. doi: 10.1016/j.palaeo.2008.04.016
    JIANG H C, JI J L, GAO L, et al., 2008. Cooling-driven climate change at 12-11 Ma: Multiproxy records from a long fluviolacustrine sequence at Guyuan, Ningxia, China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 265(1-2): 148-158. doi: 10.1016/j.palaeo.2008.05.006
    LI C Y, ZHANG P Z, YIN J H, et al., 2009. Late Quaternary left-lateral slip rate of the Haiyuan fault, northeastern margin of the Tibetan Plateau[J]. Tectonics, 28(5): TC5010. http://www.onacademic.com/detail/journal_1000035647022610_41ad.html
    LI Y, SONG Y G, QIAN L B, et al., 2013. Paleomagnetic and fission-track dating of a Late Cenozoic red earth section in the Liupan Shan and associated tectonic implications[J]. Journal of Earth Science, 24(4): 506-518. doi: 10.1007/s12583-013-0353-y
    LIN A M, HU J M, GONG W B, 2015. Active normal faulting and the seismogenic fault of the 1739 M 8.0 Pingluo earthquake in the intracontinental Yinchuan Graben, China[J]. Journal of Asian Earth Sciences, 114: 155-173. doi: 10.1016/j.jseaes.2015.04.036
    LIN X B, CHEN H L, WYRWOLL K H, et al., 2010. Commencing uplift of the Liupan Shan since 9.5 Ma: Evidences from the Sikouzi section at its east side[J]. Journal of Asian Earth Sciences, 37(4): 350-360. doi: 10.1016/j.jseaes.2009.09.005
    LIU X B, SHI W, HU J M, et al., 2019. Magnetostratigraphy and tectonic implications of Paleogene-Neogene Sediments in the Yinchuan Basin, western North China Craton[J]. Journal of Asian Earth Sciences, 173: 61-69. doi: 10.1016/j.jseaes.2019.01.016
    LIU Y S, HU Z C, GAO S, et al., 2008. In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard[J]. Chemical Geology, 257(1-2): 34-43. doi: 10.1016/j.chemgeo.2008.08.004
    LIU Y S, GAO S, HU Z C, et al., 2010a. Continental and oceanic crust recycling-induced melt-peridotite interactions in the Trans-North China Orogen: U-Pb dating, Hf isotopes and trace elements in zircons from mantle xenoliths[J]. Journal of Petrology, 51(1-2): 537-571. doi: 10.1093/petrology/egp082
    LIU Y S, HU Z C, ZONG K Q, et al., 2010b. Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LA-ICP-MS[J]. Chinese Science Bulletin, 55(15): 1535-1546. doi: 10.1007/s11434-010-3052-4
    LUDWIG K R, 2003. ISOPLOT 3.00: A geochronological toolkit for Microsoft excel[M]. Berkeley, California: Berkeley Geochronology Center: 39.
    MA Y S, 2003. Neotectonic activities and geological disaster risk assessment in the upper Yellow River[M]. Beijing: Geological Publishing House. (in Chinese)
    MEYER B, TAPPONNIER P, BOURJOT L, et al., 1998. Crustal thickening in Gansu-Qinghai, lithospheric mantle subduction, and oblique, strike-slip controlled growth of the Tibet Plateau[J]. Geophysical Journal International, 135(1): 1-47. doi: 10.1046/j.1365-246X.1998.00567.x
    MOLNAR P, TAPPONNIER P, 1975. Cenozoic tectonics of Asia: Effects of a continental collision[J]. Science, 189(4201): 419-426. doi: 10.1126/science.189.4201.419
    Ningxia Hui Autonomous Region Bureau of Geology and Mineral Resources, 1990. Regional geology of Ningxia Hui Autonomous region[M]. Beijing: Geological Publishing House. (in Chinese)
    Ningxia Hui Autonomous Region Geological Survey Institute, 2017. Regional geology of China[M]. Beijing: Geological Publishing House. (in Chinese)
    PEI X Z, SUN R Q, DING S P, et al., 2007. LA-ICP-MS zircon U-Pb dating of the Yanjiadian diorite in the eastern Qilian Mountains and its geological significance[J]. Geology in China, 34(1): 8-16. (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-DIZI200701001.htm
    QIANG X K, LI Z X, POWELL C M, et al., 2001. Magnetostratigraphic record of the Late Miocene onset of the east Asian monsoon, and Pliocene uplift of northern Tibet[J]. Earth and Planetary Science Letters, 187(1-2): 83-93. doi: 10.1016/S0012-821X(01)00281-3
    QIU Z X, YE J, HUO F C, 1988. Description of a kubanochoerus skull from Tongxin, Ningxia[J]. Vertebrata Palasiatica, 26(1): 1-14. (in Chinese with English abstract) http://www.cnki.com.cn/Article/CJFDTotal-GJZD198801001.htm
    QIU Z X, QIU Z D, 1990. Sequencing and staging of late tertiary local mammals in China[J]. Journal of Stratigraphy, 14(4): 241-260. (in Chinese)
    SHEN X H, TIAN Q J, DING G Y, et al., 2001. The late cenozxic stratigraphic sequence and its implication to Tectuic evolution Hejiakouzi Area Ningxzia Hui Autonomus regin[J]. Earthquake Research in China, 17(2): 156-166. (in Chinese with English abstract) http://qikan.cqvip.com/Qikan/Article/Detail?id=1000531762
    SHI W, ZHANG Y Q, MA Y S, 2006. Elevation distribution pattern of red clay beds in the regions east and west of Liupanshan and Neotectonic significance[J]. Marine Geology & Quaternary Geology, 26(5): 123-130. (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-HYDZ200605020.htm
    SHI W, LIU Y, LIU Y, et al., 2013. Cenozoic evolution of the Haiyuan fault zone in the northeast margin of the Tibetan Plateau[J]. Earth Science Frontiers, 20(4): 1-17. (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY201304003.htm
    SHI W, HU J M, CHEN H, et al., 2015. Cenozoic tectonic evolution of the arcuate structures in the Northeast Tibetan Plateau[J]. Acta Geologica Sinica, 89(2): 676-677. doi: 10.1111/1755-6724.12457
    SONG F M, ZHU S L, WANG Y P, et al., 1982. The maximum horizontal displacement in the Haiyuan earthquake of 1920 and the estimation of the earthquake recurrence along the northern marginal fault of the Xihuashan[J]. Seismology and Geology, 5(4): 29-38. (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZDZ198304004.htm
    SUN D H, SHAW J, AN Z S, et al., 1998. Magnetostratigraphy and paleoclimatic interpretation of a continuous 7.2 Ma Late Cenozoic eolian sediments from the Chinese Loess Plateau[J]. Geophysical Research Letters, 25(1): 85-88. doi: 10.1029/97GL03353
    TAPPONNIER P, XU Z Q, ROGER F, et al., 2001. Oblique stepwise rise and growth of the Tibet Plateau[J]. Science, 294(5547): 1671-1677. doi: 10.1126/science.105978
    TIAN Q J, SHEN X H, DING G Y, et al., 2000. Discovery and preliminary study of the Laolongwan tertiary pull-apart basin in the Haiyuan fault zone[J]. Seismology and Geology, 22(3): 329-336. (in Chinese with English abstract) http://en.cnki.com.cn/article_en/cjfdtotal-dzdz200003014.htm
    WANG W T, 2012. Sedimentary evolution of Cenozoic basins in southern Ningxia and its response to tectonic deformation in the northeast corner of Qinghai-Tibet plateau[J]. Recent Developments in World Seismology (10): 40-43. (in Chinese)
    WANG W T, ZHENG D W, PANG J Z, 2013. Provenancial tracing for the Cenozoic Sikouzi section in the northeastern margin of the Tibetan Plateau and its tectonic Implications[J]. Acta Geologica Sinica, 87(10): 1551-1569. (in Chinese with English abstract) http://epub.cnki.net/grid2008/docdown/docdownload.aspx?filename=DZXE201310006&dbcode=CJFD&year=2013&dflag=pdfdown
    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) https://oversea.cnki.net/kcms/detail/detail.aspx?dbcode=CJFD&dbname=CJFD2014&filename=DXQY201404034
    WEI F H, PEI X Z, LI R B, et al., 2012. LA-ICP-MS zircon U-Pb dating of early Paleozoic Huangmenchuan granodiorite in Tianshui area of Gansu province and its tectonic significance[J]. Geological Bulletin of China, 31(9): 1496-1509. (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD201209013.htm
    WIEDENBECK M, ALLÉ P, CORFU F, et al., 1995. Three natural zircon standards for U-Th-Pb, Lu-Hf, trace element and REE analyses[J]. Geostandards Newsletter, 19(1): 1-23. doi: 10.1111/j.1751-908X.1995.tb00147.x
    XU Y, YUE L P, LI J X, et al., 2012. Red clay deposits on the Chinese Loess Plateau during 11.0-2.6 Ma and its implications for long-term evolution of East Asian monsoon[J]. Environmental Earth Sciences, 66(7): 2021-2030. doi: 10.1007/s12665-011-1427-8
    YIN A, RUMELHART P E, BUTLER R, et al., 2002. Tectonic history of the Altyn Tagh fault system in northern Tibet inferred from Cenozoic sedimentation[J]. GSA Bulletin, 114(10): 1257-1295. doi: 10.1130/0016-7606(2002)114<1257:THOTAT>2.0.CO;2
    YU X X, MO X X, ZHAO Z D, et al., 2011. Cenozoic bimodal volcanic rocks of the West Qinling: Implication for the genesis and nature of the rifting of north-south tectonic belt[J]. Acta Petrologica Sinica, 27(7): 2195-2202. http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201107028.htm
    ZHANG J, MA Z J, REN W J, 2005. The Sedimentary characteristics of Cenozoic strata in central and southern Ningxia and their relationships with the development of the Qinghai-Tibetan Plateau[J]. Acta Geologica Sinica, 79(6): 757-773. (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE200506012.htm
    ZHANG J, MA Z J, REN W J, 2006. Discussion on the tectonic setting of deposition of the Eocene Sikouzi formation in Ningxia region[J]. Geological Review, 52(2): 207-214. (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP200602009.htm
    ZHANG J, CUNNINGHAM D, CHENG H Y, 2010. Sedimentary characteristics of Cenozoic strata in central-southern Ningxia, NW China: Implications for the evolution of the NE Qinghai-Tibetan Plateau[J]. Journal of Asian Earth Sciences, 39(6): 740-759. doi: 10.1016/j.jseaes.2010.05.008
    ZHANG J, WANG Y N, ZHANG B H, et al., 2016. Tectonics of the Xining Basin in NW China and its implications for the evolution of the NE Qinghai-Tibetan Plateau[J]. Basin Research, 28(2): 159-182. doi: 10.1111/bre.12104
    ZHANG P Z, BURCHFIEL B C, MOLNAR P, et al., 1991. Amount and style of Late Cenozoic Deformation in the Liupan Shan Area, Ningxia Autonomous Region, China[J]. Tectonics, 10(6): 1111-1129. doi: 10.1029/90TC02686
    ZHANG P Z, ZHENG D W, YIN G M, et al., 2006. Discussion on late Cenozoic growth and rise of northeastern margin of the Tibetan Plateau[J]. Quaternary Sciences, 26(1): 5-13. (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-DSJJ200601001.htm
    ZHENG D W, ZHANG P Z, WAN J L, et al., 2005. Apatite fission track evidence for the thermal history of the Liupanshan basin[J]. Chinese Journal of Geophysics, 48(1): 157-164. (in Chinese with English abstract) http://www.agu.org/WPS/ChineseJGeo/48/48.01/articles/zdw.pdf
    ZHENG W J, ZHANG P Z, YUAN D Y, et al., 2019. Basic characteristics of active tectonics and associated geodynamic processes in continental China[J]. Journal of Geomechanics, 25(5): 699-721. (in Chinese with English abstract) https://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20190506&journal_id=dzlxxb
    ZHOU T X, WANG L, CAO M Z, 1985. Morphotectonic Patterns of Ningxia Hui Autonomous region and its formation and evolution[J]. Acta Geographica Sinica, 40(3): 215-224. (in Chinese with English abstract)
    安芷生, 孙东怀, 陈明扬, 等, 2000. 黄土高原红粘土序列与晚第三纪的气候事件[J]. 第四纪研究, 20(5): 435-446. doi: 10.3321/j.issn:1001-7410.2000.05.004
    卞爽, 于志泉, 龚俊峰, 等, 2021. 青藏高原近南北向裂谷的时空分布特征及动力学机制[J]. 地质力学学报, 27(2): 178-194. https://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20210203&journal_id=dzlxxb
    陈虹, 胡建民, 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. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201304004.htm
    陈隽璐, 李好斌, 王洪亮, 等, 2007. 秦祁结合部位王家岔石英闪长岩体锆石LA-ICP-MS定年及地质意义[J]. 吉林大学学报(地球科学版), 37(3): 423-431. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ200703001.htm
    崔加伟, 李振宏, 刘锋, 等, 2018. 宁夏红寺堡盆地萨拉乌苏组地层时代重新厘定及意义[J]. 地质力学学报, 24(2): 283-292. https://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20180215&journal_id=dzlxxb
    国家地震局, 1988. 鄂尔多斯周缘活动断裂系[M]. 北京: 地震出版社.
    黄婷, 李振宏, 刘锋, 等, 2018. 宁夏红寺堡盆地地表沙漠化现状及其地质主控因素[J]. 地质力学学报, 24(4): 505-514. https://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20180408&journal_id=dzlxxb
    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.
    宁夏回族自治区地质调查院, 2017. 中国区域地质志-宁夏志[M]. 北京: 地质出版社.
    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[M]. 北京: 地质出版社.
    裴先治, 孙仁奇, 丁仨平, 等, 2007. 陇东地区阎家店闪长岩LA-ICP-MS锆石U-Pb测年及其地质意义[J]. 中国地质, 34(1): 8-16. doi: 10.3969/j.issn.1000-3657.2007.01.002
    邱占祥, 叶捷, 霍福臣, 1988. 记宁夏同心发现的库班猪头骨化石[J]. 古脊椎动物学报, 26(1): 1-14. https://www.cnki.com.cn/Article/CJFDTOTAL-GJZD198801000.htm
    邱占祥, 邱铸鼎, 1990. 中国晚第三纪地方哺乳动物群的排序及其分期[J]. 地层学杂志, 14(4): 241-260. https://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ199004000.htm
    申旭辉, 田勤俭, 丁国瑜, 等, 2001. 宁夏贺家口子地区晚新生代地层序列及其构造意义[J]. 中国地震, 17(2): 156-166. doi: 10.3969/j.issn.1001-4683.2001.02.006
    施炜, 张岳桥, 马寅生, 2006. 六盘山两侧晚新生代红黏土高程分布及其新构造意义[J]. 海洋地质与第四纪地质, 26(5): 123-130. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200605020.htm
    施炜, 刘源, 刘洋, 等, 2013. 青藏高原东北缘海原断裂带新生代构造演化[J]. 地学前缘, 20(4): 1-17. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201304003.htm
    宋方敏, 朱世龙, 汪一鹏, 等, 1982. 1920年海原地震中的最大水平位移及西华山北缘断裂地震重复率的估计[J]. 地震地质, 5(4): 29-38. https://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ198304004.htm
    田勤俭, 申旭辉, 丁国瑜, 等, 2000. 海原断裂带内第三纪老龙湾拉分盆地的地质特征[J]. 地震地质, 22(3): 329-336. doi: 10.3969/j.issn.0253-4967.2000.03.013
    王伟涛, 2012. 宁夏南部新生代盆地沉积演化及其对青藏高原东北角构造变形的响应[J]. 国际地震动态(10): 40-43. doi: 10.3969/j.issn.0253-4975.2012.10.010
    王伟涛, 郑德文, 庞建章, 2013. 青藏高原东北缘寺口子剖面碎屑锆石示踪及其构造意义[J]. 地质学报, 87(10): 1551-1569. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201310006.htm
    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. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201404034.htm
    魏方辉, 裴先治, 李瑞保, 等, 2012. 甘肃天水地区早古生代黄门川花岗闪长岩体LA-ICP-MS锆石U-Pb定年及构造意义[J]. 地质通报, 31(9): 1496-1509. doi: 10.3969/j.issn.1671-2552.2012.09.013
    张进, 马宗晋, 任文军, 2005. 宁夏中南部新生界沉积特征及其与青藏高原演化的关系[J]. 地质学报, 79(6): 757-773. doi: 10.3321/j.issn:0001-5717.2005.06.005
    张进, 马宗晋, 任文军, 2006. 试论宁夏地区始新统寺口子组沉积的构造背景[J]. 地质论评, 52(2): 207-214. doi: 10.3321/j.issn:0371-5736.2006.02.009
    张培震, 郑德文, 尹功明, 等, 2006. 有关青藏高原东北缘晚新生代扩展与隆升的讨论[J]. 第四纪研究, 26(1): 5-13. doi: 10.3321/j.issn:1001-7410.2006.01.002
    郑德文, 张培震, 万景林, 等, 2005. 六盘山盆地热历史的裂变径迹证据[J]. 地球物理学报, 48(1): 157-164. doi: 10.3321/j.issn:0001-5733.2005.01.021
    郑文俊, 张培震, 袁道阳, 等, 2019. 中国大陆活动构造基本特征及其对区域动力过程的控制[J]. 地质力学学报, 25(5): 699-721. https://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20190506&journal_id=dzlxxb
    周特先, 王利, 曹明志, 1985. 宁夏构造地貌格局及其形成与发展[J]. 地理学报, 40(3): 215-224. doi: 10.3321/j.issn:0375-5444.1985.03.003
  • 加载中

Catalog

    Figures(8)

    Article Metrics

    Article views (425) PDF downloads(81) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return