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Heavy mineral assemblage characteristics and the Cenozoic paleogeographic evolution in southwestern Qaidam Basin

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Abstract

Based on the analysis of heavy mineral assemblages in Cenozoic southwestern Qaidam Basin, we found that different areas have variable heavy mineral assemblage characteristics, which suggested that there were two source areas—the Altyn Mountains and the Qimen Tagh-East Kunlun Mountains. In Ganchaigou-Shizigou-Huatugou (Area A), which was mainly source from the Altyn Mountains, its heavy minerals were mainly composed of zircon, Ti-oxides, and wollastonite in the Paleocene-early Eocene and mainly of unstable minerals, especially amphibole, in the middle Eocene-Oligene. Since the late Oligocene-Miocene, the heavy minerals were still mainly unstable minerals, but the content of epidote increased and the content of amphibole decreased. In Qigequan-Hongliuquan (Area B), which was the mixed source from the Altyn Mountains and the Qimen Tagh-East Kunlun Mountains, its heavy minerals were mainly garnet, epidote, and amphibole. The source of Lücaotan-Dongchaishan-Kunbei (Area C) was mainly from the Qimen Tagh-East Kunlun Mountains, heavy minerals in the sediments in Area C were mainly zircon and Ti-oxides in Paleogene and garnet, epidote, and amphibole in Neogene. In Yuejin-Youshashan (Area D), where the stable minerals and unstable minerals were present simultaneously, the heavy mineral assemblages was controlled by multi-direction source. The variation of heavy mineral assemblages in southwestern Qaidam Basin shows that Altyn Mountains was of low-lying topographic relief in Paleocene-early Eocene, and the rapid uplift of Altyn Mountains started from the middle Eocene. In Paleogene, the Altyn Tagh Fault had a slow strike-slip velocity, but the strike-slip velocity increased greatly since the late Oligocene, leading to a strike-slip displacement above 300 km since Neogene. Meanwhile, the Qimen Tagh-East Kunlun fault zone was under a stable tectonic stage in Paleogene with the Qimen Tagh Mountain being low-lying hills; since the late Oligocene, the fault zone started to activate and the Qimen Tagh Mountain began to uplift rapidly.

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References

  • Andò S, Garzanti E, Padoan M, et al. 2012. Corrosion of heavy minerals during weathering and diagenesis: A catalog for optical analysis. Sediment Geol, 280: 165–178

    Article  Google Scholar 

  • Burchfiel B C, Deng Q D, Molnar P, et al. 1989. Intracrustal detachment within zones of continental deformation. Geology, 17: 748–752

    Article  Google Scholar 

  • Chen W P, Chen C Y, Nábelek J L. 1999. Present-day deformation of the Qaidam basin with implications for intra-continental tectonics. Tectonophysics, 305: 165–181

    Article  Google Scholar 

  • Chen Z L, Gong H L, Li L, et al. 2006. Cenozoic uplifting and exhumation process of the Altyn Tagh Mountains (in Chinese). Earth Sci Front, 13: 91–102

    Google Scholar 

  • China Geological Survey, Chengdu Institute of Geology and Mineral Resources. 2004. Geological Map of Tibetan Plateau and Its Adjacent (in Chinese). Chengdu: Chengdu Cartographic Publishing House

    Google Scholar 

  • Darby B J, Ritts B D, Yue Y J, et al. 2005. Did the Altyn Tagh fault extend beyond the Tibetan Plateau? Earth Planet Sci Lett, 240: 425–435

    Article  Google Scholar 

  • DeCelles P G, Robinson D M, Zandt G. 2002. Implications of shortening in the Himalayan fold-thrust belt for uplift of the Tibetan Plateau. Tectonics, 21: 1062

    Article  Google Scholar 

  • Dupont-Nivet G, Butler R F, Yin A, et al. 2002. Paleomagnetism indicates no Neogene rotation of the Qaidam Basin in northern Tibet during Indo-Asian collision. Geology, 30: 263–266

    Article  Google Scholar 

  • Dupont-Nivet G, Robinson D, Butler R F, et al. 2004. Concentration of crustal displacement along a weak Altyn Tagh fault: Evidence from paleomagnetism of the northern Tibetan Plateau. Tectonics, 23: TC1020

    Article  Google Scholar 

  • Fang X M, Zhang W L, Meng Q Q, et al. 2007. High-resolution magnetostratigraphy of the Neogene Huaitoutala section in the eastern Qaidam Basin on the NE Tibetan Plateau, Qinghai Province, China and its implication on tectonic uplift of the NE Tibetan Plateau. Earth Planet Sci Lett, 258: 293–306

    Article  Google Scholar 

  • Fu L, Guan P, Jian X, et al. 2012. Sedimentary genetic types of coarse fragment of Paleogene Lulehe formation in Qaidam Basin and Time limit of the Tibetan Plateau uplift (in Chinese). Nat Gas Geosci, 23: 833–840

    Google Scholar 

  • Garzanti E, Resentini A, Vezzoli G, et al. 2012. Forward compositional modeling of Alpine orogenic sediments. Sediment Geol, 280: 149–164

    Article  Google Scholar 

  • Garzanti E, Vermeesch P, Andò S, et al. 2013. Provenance and recycling of Arabian desert sand. Earth-Sci Rev, 120: 1–19

    Article  Google Scholar 

  • Harrison T M, Copeland P, Kind W S F, et al. 1992. Raising Tibet. Science, 255: 1663–1670

    Article  Google Scholar 

  • Hubert J F. 1962. A zircon-tourmaline-rutile maturity index and the interdependence of the composition of heavy mineral assemblages with the gross composition and texture of sandstones. J Sediment Res, 32: 440–450

    Google Scholar 

  • Hui B, Yin H S, Xia G Q, et al. 2011. Characteristics of Cenozoic sedimentary evolution in western Qaidam Basin (in Chinese). Geol Chin, 38: 1274–1281

    Google Scholar 

  • Jiang H C, Yu B S, Wang L D, et al. 2003. Analysis on depositional facies of the lower Ganchaigou formation in Hongliuquan-Shizigou Area, Western Qaidam Basin (in Chinese). Acta Sediment Sin, 21: 391–397

    Google Scholar 

  • Jolivet M, Brunel M, Seward D, et al. 2001. Mesozoic and Cenozoic tectonics of the northern edge of the Tibetan plateau: Fission-track constraints. Tectonophysics, 343: 111–134

    Article  Google Scholar 

  • Jolivet M, Brunel M, Seward D, et al. 2003. Neogene extension and volcanism in the Kunlun Fault Zone, northern Tibet: New constraints on the age of the Kunlun Fault. Tectonics, 22: 1052

    Article  Google Scholar 

  • Kapp P, Yin A, Manning G E, et al. 2003. Tectonic evolution of the Mesozoic blueschist-bearing Qiangtang metamorphic belt, central Tibet. Tectonics, 22: 1043

    Google Scholar 

  • Liu Q M, Chen K Y, Wang J, et al. 2011. The Provenance analysis of the Quaternary heavy minerals in Sanhu depression, Qaidam Basin (in Chinese). Geoscience, 25: 315–321

    Google Scholar 

  • Liu Y J, Neubauer F, Ge X H, et al. 2007. Geochronology of the Altun Fault Zone and rising of the Altun Mountains (in Chinese). Chin J Geol, 42: 134–146

    Google Scholar 

  • Liu Z H, Wan C B, Yang J G, et al. 2005. Cenozoic structural features and deformation regularities of the northern Qaidam Basin, China (in Chinese). Chin J Geol, 40: 404–414

    Google Scholar 

  • Liu Z H, Wu G Y, Yang M D, et al. 2006. Sedimentary features of the Cenozoic in the western Qaidam Basin: Response to strike-slipping of the Altun fault (in Chinese). Chin J Geol, 41: 344–354

    Google Scholar 

  • Lü B F, Zhang Y Q, Yang S Y. 2011. Characteristics of structural system and its implication for formation dynamics in Qaidam Basin (in Chinese). Geol Rev, 57: 167–174

    Google Scholar 

  • Ma D D, Shou J F, Hu Y, et al. 2005. Analysis of the main controlling factors on the formation of clastic reservoirs in the southwestern area of the Qaidam Basin (in Chinese). Acta Sediment Sin, 23: 589–595

    Google Scholar 

  • Mange M A, Maurer H F W. 1992. Heavy Minerals in Color. London: Chapman and Hall. 147

    Book  Google Scholar 

  • Morton A C. 1985. A new approach to provenance studies: Electron microprobe analysis of detrital garnets from Middle Jurassic sandstones of the northern North Sea. Sedimentology, 32: 553–566

    Article  Google Scholar 

  • Morton A C, Hallsworth C. 1994. Identifying provenance-specific features of detrital heavy mineral assemblages in sandstones. Sediment Geol, 90: 241–256

    Article  Google Scholar 

  • Morton A C, Hallsworth C R. 1999. Processes controlling the composition of heavy mineral assemblages in sandstones. Sediment Geol, 124: 3–29

    Article  Google Scholar 

  • Owens T J, Zandt G. 1997. Implications of crustal property variations for models of Tibetan plateau evolution. Nature, 387: 37–43

    Article  Google Scholar 

  • Pettijohn F J. 1957. Sedimentary Rocks. 2nd ed. New York: Harper & Brothers. 718

    Google Scholar 

  • Pettijohn F J, Potter P E, Siever R. 1987. Sand and Sandstone. 2nd ed. New York: Springer. 553

    Book  Google Scholar 

  • Ren S M, Ge X H, Yang Z Y, et al. 2006. Application of 36Cl-dating to the last rapid uplift of the Tibet Plateau (in Chinese). Acta Geol Sin, 80: 1110–1117

    Google Scholar 

  • Rieser A B, Neubauer F, Liu Y J, et al. 2005. Sandstone provenance of north-western sectors of the intracontinental Cenozoic Qaidam basin, western China: Tectonic vs. climatic control. Sediment Geol, 177: 1–18

    Article  Google Scholar 

  • Rieser A B, Bojar A V, Neubauer F, et al. 2009. Monitoring Cenozoic climate evolution of northeastern Tibet: Stable isotope constraints from the western Qaidam Basin, China. Int J Earth Sci, 98: 1063–1075

    Article  Google Scholar 

  • Ritts B D, Biffi U. 2000. Magnitude of post-Middle Jurassic (Bajocian) displacement on the central Altyn Tagh Fault system, northwest China. Geol Soc Am Bull, 112: 61–74

    Article  Google Scholar 

  • Royden L H, Burchfiel B C, van der Hilst R D. 2008. The geological evolution of the Tibetan Plateau. Science, 321: 1054–1058

    Article  Google Scholar 

  • Song B W, Zhang K X, Lu J F, et al. 2013. The middle Eocene to early Miocene integrated sedimentary record in the Qaidam Basin and its implications for paleoclimate and early Tibetan Plateau uplift. Can J Earth Sci, 50: 183–196

    Article  Google Scholar 

  • China National Petroleum Corporation. 1997. The Method of Separation and Examination of Heavy Minerals for Sedimentary Rock (in Chinese). SY/T6336-1997

    Google Scholar 

  • Sun Z M, Yang Z Y, Pei J L, et al. 2005. Magnetostratigraphy of Paleogene sediments from northern Qaidam Basin, China: Implications for tectonic uplift and block rotation in northern Tibetan plateau. Earth Planet Sci Lett, 237: 635–646

    Article  Google Scholar 

  • Tapponnier P, Xu Z Q, Roger F, et al. 2001. Oblique stepwise rise and growth of the Tibet Plateau. Science, 294: 1671–1677

    Article  Google Scholar 

  • Wang C S, Li X H. 2003. Sedimentary Basin: From Principles to Analyses (in Chinese). Beijing: Higher Education Press. 378

    Google Scholar 

  • Wang C S, Gao R, Yin A, et al. 2011. A mid-crustal strain-transfer model for continental deformation: A new perspective from high-resolution deep seismic-reflection profiling across NE Tibet. Earth Planet Sci Lett, 306: 279–288

    Article  Google Scholar 

  • Wang J G, Hu X M. 2008. Applications of geochemistry and geochronology of accessory minerals in sandstone to provenance analysis (in Chinese). Geol Rev, 54: 670–678

    Google Scholar 

  • Wang Y Q, Gong Q S, Xia Z Y, et al. 2012. Provenance analysis of Oligocene sediments in western Qaidam Basin (in Chinese). Geol Chin, 39: 426–435

    Google Scholar 

  • Weltje G J, von Eynatten H. 2004. Quantitative provenance analysis of sediments: Review and outlook. Sediment Geol, 171: 1–11

    Article  Google Scholar 

  • Wu C, Yan C F, Li H B, et al. 2013. Cenozoic tectonic evolution of the western Qaidam Basin and its constrain on the growth of the northern Tibetan Plateau (in Chinese). Acta Petrol Sin, 29: 2211–2222

    Google Scholar 

  • Wu C D, Lin C S, Shen Y P, et al. 2005. Composition of sandstone and heavy minerals implies the provenance of Kuqa Depression in Jurassic, Tarim Basin, China. Prog Nat Sci, 15: 633–640

    Article  Google Scholar 

  • Wu L, Xiao A C, Wang L Q, et al. 2012. EW-trending uplifts along the southern side of the central segment of the Altyn Tagh Fault, NW China: Insight into the rising mechanism of the Altyn Mountain during the Cenozoic. Sci China Earth Sci, 55: 926–939

    Article  Google Scholar 

  • Wu L, Gong Q L, Tan S H. 2013. When did Cenozoic left-slip along the Altyn Tagh Fault initiate? (in Chinese). Acta Petrol Sin, 29: 2837–2850

    Google Scholar 

  • Xiao A C, Wu L, Li H G, et al. 2013. Tectonic processes of the Cenozoic Altyn Tagh Fault and its coupling with the Qaidam Basin, NW China (in Chinese). Acta Petrol Sin, 29: 2826–2836

    Google Scholar 

  • Xu Y J, Du Y S, Yang J H. 2007. Prospects of sediment provenance analysis (in Chinese). Geol Sci Tech Info, 26: 26–32

    Google Scholar 

  • Yin A, Harrison T M. 2000. Geologic evolution of the Himalayan-Tibetan orogen. Ann Rev Earth Planet Sci, 28: 211–280

    Article  Google Scholar 

  • 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. Geol Soc Am Bull, 114: 1257–1295

    Article  Google Scholar 

  • Yin A, Dang Y Q, Zhang M, et al. 2007. Cenozoic tectonic evolution of Qaidam basin and its surrounding regions (Part 2): Wedge tectonics in southern Qaidam basin and the Eastern Kunlun Range. In: Sears J W, Harms T A, Evenchick C A, eds. Whence the Mountains? Inquiries into the Evolution of Orogenic Systems: A Volume in Honor of Raymond A. Geol Soc Am Spec Pap, 433: 369–390

    Google Scholar 

  • Yin A, Dang Y Q, Wang L C, et al. 2008a. Cenozoic tectonic evolution of Qaidam basin and its surrounding regions (Part 1): The southern Qilian Shan-Nan Shan thrust belt and northern Qaidan Basin. Geol Soc Am Bull, 120: 813–846

    Article  Google Scholar 

  • Yin A, Dang Y Q, Zhang M, et al. 2008b. Cenozoic tectonic evolution of the Qaidam basin and its surrounding regions (Part 3): Structural geology, sedimentation, and regional tectonic reconstruction. Geol Soc Am Bull, 120: 847–876

    Article  Google Scholar 

  • Yin C M, Li W M, Andrea R, et al. 2007. Cenozoic climate changes in the Qaidam Basin, wertern China: Evidenced from carbon and oxygen stable isotope (in Chinese). J Jilin Univ (Earth Sci Ed), 37: 901–907

    Google Scholar 

  • Yu X J, Huang B C, Guan S W, et al. 2014. Anisotropy of magnetic susceptibility of Eocene and Miocene sediments in the Qaidam Basin, Northwest China: Implication for Cenozoic tectonic transition and depocenter migration. Geochem Geophys Geosyst, 15: 2095–2108

    Article  Google Scholar 

  • Yuan S H, Liu Y J, Ge X H, et al. 2008. Uplift period of the northern margin of the Qinghai-Tibet Plateau: evidences from the Altyn Mountains and Qaidan Basin (in Chinese). Acta Petrol Mineral, 27: 413–421

    Google Scholar 

  • Yue Y J, Ritts B D, Graham S A, et al. 2003. Slowing extrusion tectonics: lowered estimate of post-Early Miocene slip rate for the Altyn Tagh Fault. Earth Planet Sci Lett, 217: 111–122

    Article  Google Scholar 

  • Yue Y J, Graham S A, Ritts B D, et al. 2005. Detrital zircon provenance evidence for large-scale extrusion along the Altyn Tagh Fault. Tectonophysics, 406: 165–178

    Article  Google Scholar 

  • Zhang K X, Wang G C, Xu Y D, et al. 2013. Sedimentary evolution of the Qinghai-Tibet Plateau in Cenozoic and its response to the uplift of the plateau. Acta Geol Sin, 87: 555–575

    Article  Google Scholar 

  • Zhao J F, Chen X H, Du Y B. 2004. The Tertiary sedimentary evolution of the Qaidam Basin, Northern China (in Chinese). Petrol Explor Dev, 31: 41–44

    Google Scholar 

  • Zhu L P, Helmberger D V. 1998. Moho offset across the northern margin of the Tibetan Plateau. Science, 281: 1170–1172

    Article  Google Scholar 

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Authors and Affiliations

  1. Key Laboratory of Orogenic Belts and Crustal Evolution, MOE, Peking University, Beijing, 100871, China

    LinLin Li, ZhaoJie Guo, MingZhen Wang, YaNan Fang & ChenChen Zhang

  2. Institute of Oil & Gas, Peking University, Beijing, 100871, China

    ZhaoJie Guo & ChenChen Zhang

  3. PetroChina Research Institute of Petroleum Exploration & Development, Beijing, 100083, China

    ShuWei Guan

  4. Research Institute of Exploration and Development, PetroChina Qinghai Oilfield Company, Dunhuang, 736202, China

    SuPing Zhou

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Li, L., Guo, Z., Guan, S. et al. Heavy mineral assemblage characteristics and the Cenozoic paleogeographic evolution in southwestern Qaidam Basin. Sci. China Earth Sci. 58, 859–875 (2015). https://doi.org/10.1007/s11430-014-5050-x

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