如何定量评估构造和气候对造山带地貌演化的贡献？

曹凯; 王国灿

doi:10.3799/dqkx.2022.831

如何定量评估构造和气候对造山带地貌演化的贡献？

doi: 10.3799/dqkx.2022.831

曹凯,
王国灿

中国地质大学地球科学学院, 湖北武汉 430074

详细信息

作者简介:
曹凯(1984-)，副教授，主要从事构造地貌学和构造热年代学的教学与科研工作.E-mail：kai.cao@cug.edu.cn

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出版历程
- 刊出日期: 2022-10-25

How to Evaluate Quantitatively the Contribution of Tectonics and Climate to the Topography Evolution of the Mountains?

摘要

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图 1 构造、气候和地表过程相互作用概念图(据Willett et al., 2006修改)

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图 2 造山带地貌演化的3种代表性模型

a. Davis的地貌“侵蚀循环”理论；b. Penck修正的“侵蚀循环”理论；c. Hack的地貌“动态平衡”理论.据Burbank and Anderson(2011)修改.F_A和F_E分别为构造和侵蚀通量(Stolar et al., 2007)，侵蚀引起沉积通量

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参考文献(25)

[1]	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. Nature, 411(6833): 62-66. https://doi.org/10.1038/35075035
[2]	Antonelli, A., Kissling, W. D., Flantua, S. G. A., et al., 2018. Geological and Climatic Influences on Mountain Biodiversity. Nature Geoscience, 11(10): 718-725. https://doi.org/10.1038/s41561-018-0236-z
[3]	Beaumont, C., Jamieson, R. A., Nguyen, M. H., et al., 2001. Himalayan Tectonics Explained by Extrusion of a Low-Viscosity Crustal Channel Coupled to Focused Surface Denudation. Nature, 414(6865): 738-742. https://doi.org/10.1038/414738a
[4]	Boos, W. R., Kuang, Z. M., 2010. Dominant Control of the South Asian Monsoon by Orographic Insulation Versus Plateau Heating. Nature, 463(7278): 218-222. https://doi.org/10.1038/nature08707
[5]	Burbank, D. W., Anderson, R. S., 2011. Tectonic Geomorphology. Wiley-Blackwell, New Jersey, 480.
[6]	Cawood, P. A., Kröner, A., Collins, W. J., et al., 2009. Accretionary Orogens through Earth History. Geological Society, London, Special Publications, 318(1): 1-36. https://doi.org/10.1144/sp318.1
[7]	Davis, W. M., 1899. The Geographical Cycle. The Geographical Journal, 14(5): 481-504. doi: 10.2307/1774538
[8]	Ding, W. N., Ree, R. H., Spicer, R. A., et al., 2020. Ancient Orogenic and Monsoon-Driven Assembly of the World's Richest Temperate Alpine Flora. Science, 369(6503): 578-581. https://doi.org/10.1126/science.abb4484
[9]	Egholm, D. L., Knudsen, M. F., Sandiford, M., 2013. Lifespan of Mountain Ranges Scaled by Feedbacks between Landsliding and Erosion by Rivers. Nature, 498(7455): 475-478. https://doi.org/10.1038/nature12218
[10]	Elsen, P. R., Tingley, M. W., 2015. Global Mountain Topography and the Fate of Montane Species under Climate Change. Nature Climate Change, 5(8): 772-776. https://doi.org/10.1038/nclimate2656
[11]	Guo, Z. T., Ruddiman, W. F., Hao, Q. Z., et al., 2002. Onset of Asian Desertification by 22 Myr ago Inferred from Loess Deposits in China. Nature, 416(6877): 159-163. https://doi.org/10.1038/416159a
[12]	Hack, J. T., 1973. Stream-Profile Analysis and Stream-Gradient Index. Journal of Research of the U. S. Geological Survey, 1(4): 421-429.
[13]	Hack, J. T., 1975. Dynamic Equilibrium and Landscape Evolution. Theories of Landform Development: Publications in Geomorphology, 91-102. http://geomorphology.sese.asu.edu/Papers/Hack_1975.pdf
[14]	Hoorn, C., Wesselingh, F. P., ter Steege, H., et al., 2010. Amazonia through Time: Andean Uplift, Climate Change, Landscape Evolution, and Biodiversity. Science, 330(6006): 927-931. https://doi.org/10.1126/science.1194585
[15]	Kooi, H., Beaumont, C., 1996. Large-Scale Geomorphology: Classical Concepts Reconciled and Integrated with Contemporary Ideas via a Surface Processes Model. Journal of Geophysical Research: Solid Earth, 101(B2): 3361-3386. https://doi.org/10.1029/95jb01861
[16]	Körner, C., Jetz, W., Paulsen, J., et al., 2017. A Global Inventory of Mountains for Bio-Geographical Applications. Alpine Botany, 127(1): 1-15. https://doi.org/10.1007/s00035-016-0182-6
[17]	Molnar, P., England, P., 1990. Late Cenozoic Uplift of Mountain Ranges and Global Climate Change: Chicken or Egg? Nature, 346(6279): 29-34. https://doi.org/10.1038/346029a0
[18]	Molnar, P., Tapponnier, P., 1975. Cenozoic Tectonics of Asia: Effects of a Continental Collision. Science, 189(4201): 419-426. doi: 10.1126/science.189.4201.419
[19]	Pazzaglia, F. J., Brandon, M. T., 2001. A Fluvial Record of Long-Term Steady-State Uplift and Erosion across the Cascadia Forearc High, Western Washington State. American Journal of Science, 301(4/5): 385-431. https://doi.org/10.2475/ajs.301.4-5.385
[20]	Penck, W., 1954. Morphological Analysis of Landforms. Soil Science, 77(1): 80.
[21]	Stolar, D. B., Willett, S. D., Montgomery, D. R., 2007. Characterization of Topographic Steady State in Taiwan. Earth and Planetary Science Letters, 261(3/4): 421-431. https://doi.org/10.1016/j.epsl.2007.07.045
[22]	Summerfield, M. A., 2000. Geomorphology and Global Tectonics. John Wiley & Sons Inc, 386.
[23]	Willett, S. D., 1999. Orogeny and Orography: The Effects of Erosion on the Structure of Mountain Belts. Journal of Geophysical Research: Solid Earth, 104(B12): 28957-28981. https://doi.org/10.1029/1999jb900248
[24]	Willett, S. D., Hovius, N., Brandon, M. T., et al., 2006. Introduction. Tectonics, Climate, and Landscape Evolution. Geological Society of America, Boulder, 398. https://doi.org/10.1130/2006.2398(00)
[25]	Wolf, S. G., Huismans, R. S., Braun, J., et al., 2022. Topography of Mountain Belts Controlled by Rheology and Surface Processes. Nature, 606(7914): 516-521. https://doi.org/10.1038/s41586-022-04700-6