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- aggregation classification "A1".
- aggregation creator B453629.
- aggregation creator B453630.
- aggregation creator B453631.
- aggregation creator B453632.
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- aggregation date "2011".
- aggregation format "application/pdf".
- aggregation hasFormat 2067694.bibtex.
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- aggregation isPartOf urn:issn:0278-7407.
- aggregation language "eng".
- aggregation rights "I have transferred the copyright for this publication to the publisher".
- aggregation subject "Earth and Environmental Sciences".
- aggregation title "Tectonic history of the Kyrgyz South Tien Shan (Atbashi-Inylchek) suture zone: the role of inherited structures during deformation-propagation".
- aggregation abstract "Multimethod chronology was applied on intrusives bordering the Kyrgyz South Tien Shan suture (STSs) to decipher the timing of (1) formation and amalgamation of the suturing units and (2) intracontinental deformation that built the bordering mountain ranges. Zircon U/Pb data indicate similarities between the Tien Shan and Tarim Precambrian crust. Caledonian (similar to 440-410 Ma) and Hercynian (similar to 310-280 Ma) zircon U/Pb ages were found at the edge of the STSs, related to subduction and closure of the Turkestan Ocean and the formation of the suture itself. Permian-Triassic (similar to 280-210 Ma) titanite fission track and zircon (U-Th)/He data record the first signs of exhumation when the STSs evolved into a shear zone and the adjacent Tarim basin started to subside. Low-temperature thermochronological (apatite fission track, zircon and apatite (U-Th)/He) analyses reveal three distinct cooling phases, becoming younger toward the STSs center: (1) Jurassic-Cretaceous cooling ages provide evidence that a Mesozoic South Tien Shan orogen formed as a response to the Cimmerian orogeny; (2) Early Paleogene (similar to 60-45 Ma) data indicate a renewed pulse of STSs reactivation during the Early Cenozoic; (3) Neogene ages constrain the onset of the modern Tien Shan mountain building to the Late Oligocene (similar to 30-25 Ma), which intensified during the Miocene (similar to 10-8 Ma) and Pliocene (similar to 3-2 Ma). The Cenozoic signals may reflect renewed responses to collisions at the southern Eurasian border (i.e., the Kohistan-Dras and India-Eurasia collisions). This progressive rejuvenation of the STSs demonstrates that deformation has not migrated steadily into the forelands, but was focused on pre-existing basement structures.".
- aggregation authorList BK789455.
- aggregation volume "30".
- aggregation aggregates 2067698.
- aggregation isDescribedBy 2067694.
- aggregation similarTo 2011TC002949.
- aggregation similarTo LU-2067694.