Late Oligocene-early Miocene unroofing in the Chinese Tian Shan: An early effect of the India-Asia collision

Research Article| June 01, 1994 Late Oligocene-early Miocene unroofing in the Chinese Tian Shan: An early effect of the India-Asia collision Marc S. Hendrix; Marc S. Hendrix 1Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305 Search for other works by this author on: GSW Google Scholar Trevor A. Dumitru; Trevor A. Dumitru 1Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305 Search for other works by this author on: GSW Google Scholar Stephan A. Graham Stephan A. Graham 1Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305 Search for other works by this author on: GSW Google Scholar Author and Article Information Marc S. Hendrix 1Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305 Trevor A. Dumitru 1Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305 Stephan A. Graham 1Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305 Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1994) 22 (6): 487–490. https://doi.org/10.1130/0091-7613(1994)0222.3.CO;2 Article history First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Marc S. Hendrix, Trevor A. Dumitru, Stephan A. Graham; Late Oligocene-early Miocene unroofing in the Chinese Tian Shan: An early effect of the India-Asia collision. Geology 1994;; 22 (6): 487–490. doi: https://doi.org/10.1130/0091-7613(1994)0222.3.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Apatite fission-track data indicate that Mesozoic strata exposed on the northern flank of the Chinese Tian Shan underwent ∼4-5 km of late Cenozoic unroofing, beginning at ∼24 Ma. This age apparently dates initial reactivation of the northern Tian Shan in response to the India-Asia collision, which continues to raise the mountain range today. Numerous studies of the Himalaya and Tibet suggest that a major shift from extrusion-dominated to crustal thickening-dominated tectonics occurred in latest Oligocene-early Miocene time, approximately coincident with the start of unroofing in the Tian Shan. This suggests that Tian Shan unroofing was a distant effect of that shift within the collision zone. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.