Fig.1 White line indicates the location of Himachal Pradesh. Figure made with GeoMapApp (www.geomapapp.org) / CC BY / CC BY (Ryan et al., 2009).[ 1]
The geology of Himachal Pradesh is dominated by Precambrian rocks that were assembled and deformed during the India-Asia collision and the subsequent Himalayan orogeny . The Northern Indian State Himachal Pradesh is located in the Western Himalaya (Fig. 1). It has a rugged terrain, with elevation ranging from 320m to 6975m.[ 2] Rock materials in the region are largely from the Indian craton ,[ 3] and their ages range from the Paleoproterozoic to the present day.[ 4] It is generally agreed that the Indian craton collided with Asia 50-60 million years ago (Ma).[ 5] [ 6] [ 7] Rock sequences were thrust and folded immensely during the collision.[ 3] The area has also been shaped by focused orographic precipitation , glaciation and rapid erosion .[ 8] [ 9]
^ Ryan, William B. F.; Carbotte, Suzanne M. ; Coplan, Justin O.; O'Hara, Suzanne; Melkonian, Andrew; Arko, Robert; Weissel, Rose Anne; Ferrini, Vicki; Goodwillie, Andrew; Nitsche, Frank; Bonczkowski, Juliet (March 2009). "Global Multi-Resolution Topography synthesis" . Geochemistry, Geophysics, Geosystems . 10 (3): n/a. Bibcode :2009GGG....10.3014R . doi :10.1029/2008gc002332 . ISSN 1525-2027 .
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^ a b Webb, A. Alexander G.; Yin, An; Harrison, T. Mark; Célérier, Julien; Gehrels, George E.; Manning, Craig E.; Grove, Marty (2011-08-01). "Cenozoic tectonic history of the Himachal Himalaya (northwestern India) and its constraints on the formation mechanism of the Himalayan orogen" . Geosphere . 7 (4): 1013–1061. doi :10.1130/GES00627.1 .
^ Yin, An (2006-05-01). "Cenozoic tectonic evolution of the Himalayan orogen as constrained by along-strike variation of structural geometry, exhumation history, and foreland sedimentation" . Earth-Science Reviews . 76 (1): 1–131. Bibcode :2006ESRv...76....1Y . doi :10.1016/j.earscirev.2005.05.004 . ISSN 0012-8252 .
^ Hodges, K. V. (2000-03-01). "Tectonics of the Himalaya and southern Tibet from two perspectives" . GSA Bulletin . 112 (3): 324–350. Bibcode :2000GSAB..112..324H . doi :10.1130/0016-7606(2000)112<324:TOTHAS>2.0.CO;2 . ISSN 0016-7606 .
^ Wu, F.-Y.; Ji, W.-Q.; Wang, J.-G.; Liu, C.-Z.; Chung, S.-L.; Clift, P. D. (2014-02-01). "Zircon U-Pb and Hf isotopic constraints on the onset time of India-Asia collision" . American Journal of Science . 314 (2): 548–579. Bibcode :2014AmJS..314..548W . doi :10.2475/02.2014.04 . ISSN 0002-9599 . S2CID 130337662 .
^ Colleps, C.L.; McKenzie, N.R.; Horton, B.K.; Webb, A.A.G.; Ng, Y.W.; Singh, B.P. (March 2020). "Sediment provenance of pre- and post-collisional Cretaceous–Paleogene strata from the frontal Himalaya of northwest India" . Earth and Planetary Science Letters . 534 : 116079. Bibcode :2020E&PSL.53416079C . doi :10.1016/j.epsl.2020.116079 . ISSN 0012-821X . S2CID 213962032 .
^ THIEDE, R (May 2004). "Climatic control on rapid exhumation along the Southern Himalayan Front" . Earth and Planetary Science Letters . doi :10.1016/s0012-821x(04)00198-0 . ISSN 0012-821X .
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