Skip to main content
Log in

Influences of Tibetan Plateau uplift on provenance evolution of the paleo-Pearl River

  • Original Article
  • Published:
Chinese Journal of Geochemistry Aims and scope Submit manuscript

Abstract

A comparative analysis of the geochemical characteristics of sediments from the Oligocene Zhuhai Formation (32–23.8 Ma), the Miocene Zhujiang Formation (23.8–16.5 Ma), and the Hanjiang Formation (16.5–10.5 Ma) and a comprehensive analysis of the geochemical characteristics of rocks surrounding the paleo-Pearl River drainage contribute to understanding the influences of the Tibetan Plateau uplift on provenance evolution of the paleo-Pearl River. The results show that the geochemical characteristics of sediments from the Oligocene Zhuhai Formation are very different from the geochemical characteristics of sediments from the Miocene Zhujiang and Hanjiang Formations. The ∑ rare earth elements (REE) of mudstone is relatively high in the Zhuhai Formation, 204.07–293.88 ppm (average 240.46 ppm), and low in the Zhujiang and Hanjiang Formations, 181.32–236.73 ppm (average 203.83 ppm) and 166.84–236.65 ppm (average 199.04 ppm), respectively. The chemical index of alteration (CIA) for these samples has a similar trend to the ∑ REE: the CIA of the Zhuhai Formation is relatively high and the CIA of the Zhujiang and Hanjiang Formations is relatively low. The uplift of the Tibetan Plateau is crucial to the westward expansion of the paleo-Pearl River drainage.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5

Similar content being viewed by others

References

  • Allegre CT (1978) Quantitative models of trace planet. Earth Plant Sci Lett 38:1–25

    Article  Google Scholar 

  • Burbank DW (1992) Causes of recent Himalaya uplift deduced from deposit patterns in the Ganges basin. Nature 357:680–682

    Article  Google Scholar 

  • Chen S, Pei C (1993) Geology and geochemistry of source rocks of the eastern Pearl River Mouth Basin, South China Sea. J Southeast Asian Earth Sci 81:393–406

    Google Scholar 

  • Chen L, Liu J, Zhou X, Wang P (1999) Impact of uplift of Qinghai-Xizang Plateau and change of land-ocean distribution on climate over Asia. Quat Sci 4:314–329 (in Chinese with English abstract)

    Google Scholar 

  • Chen C, Shi H, Xu S, Chen X (2003) The conditions of hydrocarbon accumulation of the tertiary petroleum system in the Pearl River Mouth Basin. Science Press, Beijing, pp 1–27 (in Chinese)

    Google Scholar 

  • Chen F, Li Q, Wang X, Li X (2006) Zircon age and Sr–Nd–Hf isotopic composition of migmatite in the eastern Tengchong block, western Yunnan. Acta Petrol Sin 22:439–448 (in Chinese with English abstract)

    Google Scholar 

  • Clift P, Lee JI, Clark M (2002) Erosinal response of South China to arc rifting and monsoonal strengthening a record from the South China Sea. Mar Geol 184:207–226

    Article  Google Scholar 

  • Condie KC, Noll JPD, Conway CM (1992) Geochemical and detrital mode evidence for two sources of Early Proterozoic sedimentary rocks from the Tonto Basin Supergroup, central Arizona. Sediment Geol 77:51–76

    Article  Google Scholar 

  • Cullers Rl (1995) The controls on the major and trace elements evolution of shales, siltstones and sandstones of Ordorvician to tertiary age in the Wet Mountains region, Colorado, USA. Chem Geol 123:107–131

    Article  Google Scholar 

  • Dai S, Yang S, Cai A (2007) Variation of sediment discharge of the Pear l River Basin from 1955 to 2005. Acta Geogr Sin 62:545–554 (in Chinese with English abstract)

    Google Scholar 

  • Darbyshire DPF, Sewell RJ (1997) Nd and Sr isotope geochemistry of plutonic rocks from Hong Kong implications for granite petrogenesis regional structure and crustal evolution. Chem Geol 143:81–93

    Article  Google Scholar 

  • Deniel C, Vidal P, Femandez A, Le Fort P, Pencat J-J (1987) Isotopic study of the Manaslu granite inferences on the age and source of Himalayan leucogranites. Contrib Miner Petrol 96:78–92

    Article  Google Scholar 

  • England PC, Houseman GA (1988) The mechanics of the Tibet Plateau. Philos Trans R Soc Lond 73:523–532

    Google Scholar 

  • Fedo CM, Nesbitt HW, Young GM (1995) Unravelling the effects of potassium metasomatism in sedimentary rocks and paleosoles, with implications for paleoweathing conditions and provenance. Geology 23:921–924

    Article  Google Scholar 

  • Ge X (2003) Mesozoic magmatism in Hainan Island (SE China) and its tectonic significance: geochronology, geochemistry and Sr-Nd isotope evidences. Doctor’s Degree Dissertation, Institute of Geochemistry, Chinese Academy of Science, Guangzhou, p 29 (in Chinese with English abstract)

  • Girty GH, Ridge DL, Knaack C (1996) Provenance and depositional setting of paleozoic chert and argillite, Sierra Nevada, California. J Sediment Res 66:107–118

    Google Scholar 

  • Gu XX, Liu JM, Zheng MH, Tang JX, Qi L (2002) Provenance and tectonic setting of the Proterozoic turbidites in Hunan, South China: geochemical evidence. J Sediment Res 72:393–407

    Article  Google Scholar 

  • Hao F, Sun Y, Li S, Zhang Q (1995) Overpressure retardation of organic-matter maturation and petroleum generation—a case study from the Yinggehai and Qiongdongnan Basins, South China Sea. AAPG Bull 79:551–562

    Google Scholar 

  • Hao F, Li S, Gong Z, Yang J (2000) Thermal regime, inter-reservoir compositional heterogeneities, and reservoir-filling history of the Dongfang gas field, Yinggehai Basin, South China Sea: evidence for episodic fluid injections in overpressured basins. AAPG Bull 84:607–626

    Google Scholar 

  • Jin J, Li Z, Chen X, Ling Z, Cao X, Wang S (2011) Paleoclimatic significance of geochemical elements from Takermohur desert, Xinjiang since Late Holocene. Acta Sedimentol Sin 29:336–343 (in Chinese with English abstract)

    Google Scholar 

  • Kazuo A, Asaniko T (1992) Two phase uplift of higher Himalayas since 17 Ma. Geology 20:391–394

    Article  Google Scholar 

  • Kent-Corson ML, Ritts BD, Zhuang GS, Bovet PM, Graham SA, Chamberlain CP (2009) Stable isotopic constraints on the tectonic, topographic, and climatic evolution of the northern margin of the Tibetan Plateau. Earth Planet Sci Lett 282:158–166

    Article  Google Scholar 

  • Li X, Liu Y, Tu X, Hu G, Zeng W (2002) Precise determination of chemical compositions in silicate rocks using ICP-AES and ICP-MS: a comparative study of sample digestion techniques of alkali fusion and acid dissolution. Geochimica 31:289–294

    Google Scholar 

  • Li XH, Wei GJ, Shao L (2003) Geochemical and Nd isotopic variations in sediments of the South China Sea: a response to Cenozoic tectonism in SE Asia. Earth Planet Sci Lett 211:207–220

    Article  Google Scholar 

  • Li Q, Zheng F, Liu C (2007a) Stratigraphic events across the Oligocene/Miocene boundary. Mar Geol Quat Geol 27:57–64 (in Chinese with English abstract)

    Google Scholar 

  • Li Q, Zhao Q, Zhong G, Jian Z, Tian J (2007b) Deepwater ventilation and stratification in the Neogene South China Sea. J China Univ Geosci 18:95–108 (English edition)

    Article  Google Scholar 

  • Li Y, Zheng R, Gao B, Hu X, Dai Z (2011) Characteristics of the detrital response to Oligocene/Miocene geological events in Baiyun Sag, Pearl River Mouth Basin. Geoscience 25:476–481 (in Chinese with English abstract)

    Google Scholar 

  • Li Y, Zheng R, Yang B, Zhu G, Gao B, Hu X (2013) Deep-water Depositional Features of Miocene Zhujiang Formation in Baiyun Sag, Pearl River Mouth Basin. Acta Geol Sin 87:197–210 (English Edition)

    Article  Google Scholar 

  • Liu S, Chi X, Li C, Yang R (2001) The summarizing for the forming and uplifted mechanism of Qinghai-Tibet Plateau. World Geol 20:105–112 (in Chinese with English abstract)

    Google Scholar 

  • Liu Z, Christophe C, Wei H, Zhong C, Alain T, Chen J (2007) Clay minerals in surface sediments of the Pearl River drainage basin and their contribution to the South China Sea. Chin Sci Bull 52:1101–1111

    Article  Google Scholar 

  • Liu D, Fang X, Song C, Dai S, Zhang T, Zhang W, Miao Y, Liu Y, Wang J (2010) Stratigraphic and paleomagnetic evidence of mid-Pleistocene rapid deformation and uplift of the NE Tibetan Plateau. Tectonophysics 486:108–119

    Article  Google Scholar 

  • Liu B, Pang X, Yan C, Liu J, Lian S, He M, Shen J (2011) Evolution of the Oligocene-Miocene shelf slope-break zone in the Baiyun deep-water area of the Pearl River Mouth Basin and its significance in oil–gas exploration. Acta Pet Sin 32:234–242 (in Chinese with English abstract)

    Google Scholar 

  • Miao Y, Meng Q, Fang X, Yan X, Wu F, Song C (2011) Origin and development of Artemisia (Asteraceae) in Asia and its implications for the uplift history of the Tibetan Plateau: a review. Quat Int 236:3–12

    Article  Google Scholar 

  • Nesbitt HWM, Young GM (1982) Early Proterozoic climates and plate motions inferred from major element chemistry of lutites. Nature 299:715–717

    Article  Google Scholar 

  • Pan Y (1999) Formation and uplifting of the Qinghai-Tibet Plateau. Earth Sci Front 6:153–163 (in Chinese with English abstract)

    Google Scholar 

  • Pang X, Chen C, Shi H, Yu S, Shao L, He M, Shen J (2005) Response between relative sea-level change and the Pearl River deep-water fan system in the South China Sea. Earth Sci Front 12:167–177 (in Chinese with English abstract)

    Google Scholar 

  • Pang X, Chen C, Shao L, Wang C, Zhu M (2007) Baiyun movement, a great tectonic event on the Oligocene–Miocene boundary in the northern South China Sea and its implications. Geol Rev 53:145–150 (in Chinese with English abstract)

    Google Scholar 

  • Peng D, Pang X, Chen C, Yu S, Ye B, Gan J, Wu C, Huang X (2005) From shallow-water shelf to deep-water slope—the study on deep-water fan systems in South China Sea. Acta Sedimentol Sin 23:1–11 (in Chinese with English abstract)

    Google Scholar 

  • Qin C, Shi H, Zhang Z, Gao P, Xu H, Qu L, Liu D (2011) Sedimentary characteristics and hydrocarbon exploration potential along the SQ21.0 sequence shelf-break zone on Panyu low-uplift and the north slope of Baiyun Sag, Pearl River Mouth Basin. China Offshore Oil Gas 23:14–18 (in Chinese with English abstract)

    Google Scholar 

  • Qu X, Hou Z, Khin Z, Mo X, Xu W, Xin H (2009) A large-scale copper ore-forming event accompanying rapid uplift of the southern Tibetan Plateau: evidence from zircon SHRIMP U-Pb dating and LA ICP-MS analysis. Ore Geol Rev 36:52–64

    Article  Google Scholar 

  • Ruddiman WF, Prell WL, Raymo ME (1989) Late Cenozoic uplift in south Asia and the American west: rationale for general circulation modeling experiments. J Geophys Res 94:379–391

    Google Scholar 

  • Rudnick RL, Gao S (2003) Composition of the continental crust. In: Holland HD, Turekian KK (eds) Treatise on geochemistry. Elsevier Pergamon, Oxford, pp 1–64

    Chapter  Google Scholar 

  • Shao L, Pang X, Chen C, Shi H, Li Q, Qiao P (2007) Terminal Oligocene sedimentary environments and abrupt provenance change event in the northern South China Sea. Geol China 34:1022–1031 (in Chinese with English abstract)

    Google Scholar 

  • Shao L, Pang X, Qiao P, Chen C, Li Q, Miao W (2008) Sedimentary filling of the Pearl River Mouth Basin and its response to the evolution of the Pearl River. Acta Sedimentol Sin 26:179–185 (in Chinese with English abstract)

    Google Scholar 

  • Shen J, Wang SM, Wang Y, Qiang XK, Xiao HF, Xiao XY (2010) Uplift events of the Qinghai-Tibetan Plateau and environmental evolution of the southwest monsoon since 2.7 Ma, recorded in a long lake sediment core from Heqing, China. Quat Int 218:67–73

    Article  Google Scholar 

  • Song C, Fang X, Li J, Gao J, Zhao Z, Fan M (2001) Tectonic uplift and sedimentary evolution of the Jiuxi Basin in the northern margin of the Tibetan Plateau since 13 Ma BP. Sci China (Ser D) 44(Supp.):192–202

    Article  Google Scholar 

  • Sun SS, McDonough WF (1989) Chemical and isotopic systematics of oceanic basalts; implications for mantle composition and processes. In: Saunders AD, Norry MJ (eds) Magmatism in the ocean basins, vol 42. Geological Society of London Special Publication, London, pp 313–345

    Google Scholar 

  • Taylor SR, Mclennan SM (1985) The continental crust, its composition and evolution. Blackwell, Oxford, pp 1–32

    Google Scholar 

  • Vervoort JD, Patchett PJ, Soderlund U, Baker M (2004) Isotopic composition of Yb and the determination of Lu concentrations and Lu/Hf ratios by isotopic dilution using MC-ICP-MS. Geochem Geophys Geosyst (G3) 5:Q11002. doi:10.1029/2004GC000721

    Google Scholar 

  • Wang C, Ding X (1998) The new researching progress of Tibet Plateau uplift. Adv Earth Sci 13:526–532 (in Chinese with English abstract)

    Google Scholar 

  • Wang G, Wang C, Zeng Y (1999) Sedimentary evidence of the westernYunnan Plateau uplift since Miocene. Bull Miner Petrol Geochem 18:167–170 (in Chinese with English abstract)

    Google Scholar 

  • Wang G, Wang C, Zeng Y, Zhao X (2000) The uplift of the western Yunnan Plateau and the sedimentary response of the Yinggehai Basin. Acta Sediment Sin 18:234–240 (in Chinese with English abstract)

    Google Scholar 

  • Wang G, Chu F, Wang C (2004) Paleoelevation reconstruction of Red River drainage areas in western Yunnan Plateau since Miocene. J Chengdu Univ Technol 31:119–124 (in Chinese with English abstract)

    Google Scholar 

  • Wang Z, Chen X, Zhang L, Li Y (2006) Spatio-temporal change characteristics of precipitation in the Pearl River Basin in recent 40 years. J China Hydrol 26:71–75 (in Chinese with English abstract)

    Google Scholar 

  • Wang C, Dai J, Liu Z, Zhu L, Li Y, Jia G (2009) The uplift history of the Tibetan Plateau and Himalaya and its study approaches and techniques: a review. Earth Sci Front 16:1–30 (in Chinese with English abstract)

    Google Scholar 

  • Wang G, Cao K, Zhang K, Wang A, Liu C, Meng Y, Xu Y (2011) Spatio-temporal framework of tectonic uplift stages of the Tibetan Plateau in Cenozoic. Sci China 54:29–44

    Article  Google Scholar 

  • Wang Y, Zheng J, Zhang W, Li S, Liu X, Yang X, Liu Y (2012a) Cenozoic uplift of the Tibetan Plateau: evidence from the tectonic-sedimentary evolution of the western Qaidam Basin. Geosci Front 3:175–187

    Article  Google Scholar 

  • Wang Y, Wang Y, Xu Q, Li D, Zhuo H, Zhou W (2012b) The early-middle Miocene submarine fan system in the Pearl River Mouth Basin, South China Sea. Pet Sci 9:1–9

    Article  Google Scholar 

  • Xu Z, Cheng R, Shen Y, Wang L, Zhang L (2012) Sedimentary records of the climatic transition from warm and humid to dry and hot during Late Triassic Early Jurassic in southwestern Fujian. J China Univ Min Technol 41:783–792 (in Chinese with English abstract)

    Google Scholar 

  • Yang S, Jiang S, Ling H, Xia X, Sun M, Wang D (2007) Sr–Nd isotopic compositions of the Changjiang sediments: implications for tracing sediment sources. Sci China (Ser D) 50:1556–1565

    Article  Google Scholar 

  • Zhang Z, Wang F (2003) Sr, Nd and Pb isotopic characteristics of Emeishan Basalt province and discussion on their source region. Earth Sci 28:432–439 (in Chinese with English abstract)

    Google Scholar 

  • Zhang Y, Dong S, Yang N (2009) Active faulting pattern, present-day tectonic stress field and block kinematics in the east Tibetan Plateau. Acta Geol Sin 83:694–712 (English edition)

    Article  Google Scholar 

  • Zhang Z, Qin C, Gao P, Qu L, Liu D, Xu H, Xu L, Zhou F (2011) Geological characteristics and exploration potentials of the shelf break zone on the north slope of the Baiyun Depression, Pearl River Mouth Basin. Nat Gas Ind 31:39–44 (in Chinese with English abstract)

    Google Scholar 

  • Zhong D, Ding L (1996) Rising process of the Qinghai-Xizang (Tibet) Plateau and its mechanism. Sci China (Ser D). 26:35–45 (in Chinese with English abstract)

    Google Scholar 

  • Zhou D, Yao B (2009) Tectonics and sedimentary basins of the South China Sea: challenges and progresses. J Earth Sci 20:1–12

    Article  Google Scholar 

  • Zhu D, Pan G, Mo X, Duan L, Liao Z, Wang L (2003) Sr–Nd–Pb isotopic variations of the Cenozoic volcanic rocks from the Qingha-i Xizang Plateau and its adjacent areas. Sediment Geol Tethyan Geol 23:1–11 (in Chinese with English abstract)

    Google Scholar 

  • Zhu W, Zhang G, Gao L (2008) Geological characteristics and exploration objectives of hydrocarbons in the northern continental margin basin of South China Sea. Acta Pet Sin 19:1–9 (in Chinese with English abstract)

    Google Scholar 

Download references

Acknowledgments

This work was supported by the National Major Scientific and Technological Special Project during the Twelfth Five-year Plan Period (Grant No. 2011ZX05023-002). The authors appreciate the help of Professor Shao Lei and State Key Laboratory of Marine Geology (Tongji University) with the geochemical analysis, and Du Jiayuan, Liu Daoli with project support.

Author information

Authors and Affiliations

Authors

Corresponding authors

Correspondence to Ye Yu or Changmin Zhang.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Yu, Y., Zhang, C., Li, S. et al. Influences of Tibetan Plateau uplift on provenance evolution of the paleo-Pearl River. Chin. J. Geochem. 34, 208–218 (2015). https://doi.org/10.1007/s11631-015-0032-z

Download citation

  • Received:

  • Revised:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s11631-015-0032-z

Keywords

Navigation