Abstract
Recent mapping in the Gangdese block has revealed many leucogranites that are similar to those in the High Himalaya. These leucogranites formed at ∼140 Ma as indicated by monazite Th-Pb ion-microprobe dating and cooled at ∼130 Ma as indicated by muscovite40Ar/39Ar dating. In conjunction with previous structural and paleogeographic studies, the new data indicate that the Gangdese block underwent crustal thickening and associated exhumation during ∼140–130 Ma. In this regard, the southern margin of Eurasia continent was comparable to the modern South American Altiplano-Puna plateau, the prime example of active ocean-continent subduction and associated thickened crust. Specifically, the early stages of crustal thickening and uplifting of the Gangdese block may result from subduction of the Neo-Tethyan Ocean. If the Tibetan Plateau would form by accretion of a series of blocks with thickened crust, an elevated topographic plateau similar to the Altiplano-Puna plateau had formed before collision between the Indian and Eurasian plates. Then the Tibetan Plateau would have quickly thickened, uplifted, and begun to extend soon after onset of the collision. Thus, the deformational mechanism of the Tibetan Plateau is not distributed shortening, but rather concentrating deformation within regions of thin crust between the accreted blocks.
Similar content being viewed by others
References
Zhao, W. J., Nelson, K. D., Project INDEPTH team, Deep seismic reflection evidence for continental underthrusting beneath southern Tibet, Nature, 1993, 366: 557–559.
Nelson, K. D., Zhao, W. J., Brown, L. D., et al., Partially molten middle crust beneath Southern Tibet: synthesis of Project INDEPTH results, Science, 1996, 274: 1684–1696.
Hirn, A., Jiang, M., Sapin, M. et al., Scismic anisotropy as an indicator of mantle flow beneath the Himalayas and Tibet. Nature, 1995, 375: 571–574.
Beck, R. A., Burbank, D. W., Sercombe, W. J. et al., Stratigraphic evidence for an early collision between northwest India and Asia, Nature, 1995, 373: 55–58.
Rowley, D. B., Age of initiation of collision between India and Asia: A review of stratigraphic data, Earth and Planetary Science Letters, 1996, 145: 1–13.
Kley, J., Eisbacher, G. H., How Alpine or Himalayan are the Central Andes? Int. Journ. Earth Sciences, 1999, 88: 175–189.
Wigger, P. J., Schmitz, M., Araneda, M. et al., Variation in the crustal structure of the southern Central Andes deduced from seismic refraction investigations (eds. Reutter, K. J., Scheuber, E., Wigger, P. J.), Tectonics of the southern Central Andes, Berlin Heidelberg New York: Springer, 1994, 23–48.
Okaya, N., Tawackoli, S., Giese, P., Area-balanced model of the late Cenozoic tectonic evolution of the central Andean arc and back arc (lat. 20°–22°S), Geology, 1997, 25: 367–370.
Baumont, D., Paul, A., Lithospheric structure of the central Andes based on surface wave dispersion, Journal of Geophysocal Research, 2002, 107, B122371, ESE 18: 1–13.
Murphy, M. A., Yin, A., Harrison, T. M. et al., Did the IndoAsian collision alone create the Tibetan Plateau? Geology, 1997, 25: 719–722.
Zhang, K. J., Zhang, Y. J., Xia, B. D., Did the Indo-Asian collision alone create the Tibetan Plateau?: comment, Geology, 1998, 26: 958–959.
Harrsion, T. M., McKeegan, K. D., Le Fort, P., Detection of inherited monazite in the Manaslu leucogranite by208Pb/232Th ion microprobe dating: crystallization age and tectonic significance, Earth and Planetary Science Letters, 1995, 133: 271–282.
England, P., Le Fort, P., Molnar, P. et al., Heat sources for Tertiary metamorphism and anatexis in the Annapurna-Manaslu region, Central Nepal, Journal of Geophysical Research, 1992, 97: 2107–2128.
Guillot, S., Le Fort, P., Geochemical constrains on the bimodal origin of High Himalayan leucogranite, Lithos., 1995, 35: 221–234.
Xizang Bureau of Geology and Mineral Resources, The Regional Geology of Xigazi and Yadong (Geology Part) Scale 1: 1000000 (in Chinese), Beijing, Geological Publishing House, 1983, 10–314.
Yin An, Harrison, T. M., Geologic evolution of the Himalayan-Tibetan orogen, Annu. Rev. Earth Planet. Sci., 2000, 28: 211–280.
Zhao, Z. J., Li, Y. T., Ye, H. F. et al. Petroleum geology in Qiangtang basin of Tibet Plateau, Beijing: Sciences Press, 2001, 66–123.
Einsele, G., Liu, B., Durr, S. et al., The Xigaze forearc basin: evolution and facies architecture (Cretaceous, Tibet), Sedimentary Geology, 1994, 90: 1–32.
Coulon, C., Maluski, H., Bollinger, C. et al., Mesozoic and Cenozoic volcanic rocks from central and southern Tibet:39Ar-40Ar dating, petrological characteristics and geodynamical significance, Earth and Planetary Science Letters, 1986, 79: 281–302.
Xizang Bureau of Geology and Mineral Resources, The Regional Geology of Xikazi and Yadong (Geology Part) Scale 1: 200000 (in Chinese), Beijing: Geological Publishing House, 1991, 22–148.
Harrison, T. M., Copeland, P., Kidd, W. S. F. et al., Raising Tibet, Science, 1992, 255: 1663–1670.
Coleman, M., Hodges, K., Evidence for Tibetan plateau uplift before 14Myr ago from a new minimum age for east-west extension, Nature, 1995, 374: 49–52.
Blismuk, P. M., Hacker, B. R., Glodny, J. et al., Normal faulting in central Tibet since at least 13.5 Myr ago, Nature, 2001, 412: 628–632.
Harrison, T. M., Grove, M., McKeegan, K. D. et al., Origin and episodic emplacement of the Manaslu intrusive complex, central Himalaya, Journal of Petrology, 1999, 40: 3–19.
Ding, L., Zhong, D. L., Yin An et al., Cenozoic structural and metamorphic evolution of the eastern Himalayan syntaxis (Namche Barwa), Earth and Planetary Science Letters, 2001, 192: 423–438.
Wang, S. S., Constraits of chlorine on40Ar/39Ar dating and calculation of high-precise40Ar/39Ar ages, Sciences Geologica Sinica, 1992, 27: 369–378.
Burchfiel, B. C., Chen, Z., Hodges, K. V. et al., The south Tibetan detachment system, Himalayan orogen: Extension contemporaneous with and parallel to shortening in a collisional mountain belt, Geol. Soc. Am. Special Paper, 1992, 269: 1–41.
Yin An, Rumelhart, P. E., Butler, R. et al., Tectonic history of the Altyn Tagh fault system in northern Tibet inferred from Cenozoic sedimentation, GSA Bulletin, 2002, 114: 1257–1295.
Tapponnier, P., Xu, Z. Q., Roger, F. et al., Oblique stepwise rise and growth of the Tibet Plateau, Science, 2001, 294: 1671–1677.
Author information
Authors and Affiliations
Corresponding author
About this article
Cite this article
Ding, L., Lai, Q. New geological evidence of crustal thickening in the Gangdese block prior to the Indo-Asian collision. Chin. Sci. Bull. 48, 1604–1610 (2003). https://doi.org/10.1007/BF03183969
Received:
Issue Date:
DOI: https://doi.org/10.1007/BF03183969