Matches in SemOpenAlex for { <https://semopenalex.org/work/W2996263438> ?p ?o ?g. }
- W2996263438 endingPage "228310" @default.
- W2996263438 startingPage "228310" @default.
- W2996263438 abstract "The Cenozoic India-Asia collision reactivated several ancient thrust belts in the interior of the Asian continent, including the West and East Kunlun ranges in central Tibet, and the Tian Shan and Qilian Shan further north. Both basin sedimentary records and thermochronological data show that the uplift of the South Tian Shan and Qilian Shan at the north occurred earlier than that of the West and East Kunlun ranges at the south. Diachronous continental deformation and initiation of uplift during orogeny are contrary to the general notion that the stress transfer in response to the India-Asia collision should propagate sequentially from south to north. Here we systematically conducted 2D thermo-mechanical simulations to investigate possible factors for this diachronous deformation pattern. The results show that a hotter Tian Shan lithosphere, with Moho temperature >100 °C hotter than that of the proto-southern Asia, leads to an earlier and higher uplift of the Tian Shan. Additionally, a faster convergence rate of the India-Asia collision results in a more efficient transfer of boundary force into the upper plate's interior, giving rise to a larger amount of uplift in the Tian Shan. We conclude that intra-continental ranges with weaker lithosphere, such as the Tian Shan or Qilian Shan, uplift earlier than stronger regions, such as the West and East Kunlun ranges. Faster convergence rates amplify this situation. Our results imply that the unique diachronous growth of the Tibetan plateau arises from its complex pre-collisional history, which includes collided arc-continent terranes with hotter and weaker lithosphere that respond to the effects of far-field stress transfer." @default.
- W2996263438 created "2019-12-26" @default.
- W2996263438 creator A5000882772 @default.
- W2996263438 creator A5011273231 @default.
- W2996263438 creator A5015664275 @default.
- W2996263438 creator A5040214967 @default.
- W2996263438 creator A5060883640 @default.
- W2996263438 creator A5084860196 @default.
- W2996263438 creator A5089357549 @default.
- W2996263438 creator A5091418610 @default.
- W2996263438 date "2020-01-01" @default.
- W2996263438 modified "2023-10-17" @default.
- W2996263438 title "Diachronous uplift in intra-continental orogeny: 2D thermo-mechanical modeling of the India-Asia collision" @default.
- W2996263438 cites W1540907122 @default.
- W2996263438 cites W1607805073 @default.
- W2996263438 cites W1635932458 @default.
- W2996263438 cites W1658256170 @default.
- W2996263438 cites W1667867793 @default.
- W2996263438 cites W1861597417 @default.
- W2996263438 cites W1964042891 @default.
- W2996263438 cites W1969077938 @default.
- W2996263438 cites W1972705099 @default.
- W2996263438 cites W1973623325 @default.
- W2996263438 cites W1975821545 @default.
- W2996263438 cites W1979790521 @default.
- W2996263438 cites W1983483408 @default.
- W2996263438 cites W1987224960 @default.
- W2996263438 cites W1988085376 @default.
- W2996263438 cites W1988918961 @default.
- W2996263438 cites W1988979328 @default.
- W2996263438 cites W1991702933 @default.
- W2996263438 cites W1992516451 @default.
- W2996263438 cites W1993869084 @default.
- W2996263438 cites W1995043866 @default.
- W2996263438 cites W1996923801 @default.
- W2996263438 cites W1997744066 @default.
- W2996263438 cites W1998028544 @default.
- W2996263438 cites W1999146909 @default.
- W2996263438 cites W1999147128 @default.
- W2996263438 cites W2002325302 @default.
- W2996263438 cites W2002637732 @default.
- W2996263438 cites W2004538247 @default.
- W2996263438 cites W2005769501 @default.
- W2996263438 cites W2012452556 @default.
- W2996263438 cites W2013651167 @default.
- W2996263438 cites W2015665518 @default.
- W2996263438 cites W2015673335 @default.
- W2996263438 cites W2016461253 @default.
- W2996263438 cites W2017178470 @default.
- W2996263438 cites W2017649324 @default.
- W2996263438 cites W2017720481 @default.
- W2996263438 cites W2019671752 @default.
- W2996263438 cites W2019748000 @default.
- W2996263438 cites W2019797998 @default.
- W2996263438 cites W2021065582 @default.
- W2996263438 cites W2025964703 @default.
- W2996263438 cites W2027864691 @default.
- W2996263438 cites W2027934726 @default.
- W2996263438 cites W2028427335 @default.
- W2996263438 cites W2032149561 @default.
- W2996263438 cites W2034927575 @default.
- W2996263438 cites W2035621835 @default.
- W2996263438 cites W2035711153 @default.
- W2996263438 cites W2040200942 @default.
- W2996263438 cites W2041774199 @default.
- W2996263438 cites W2042324412 @default.
- W2996263438 cites W2044919273 @default.
- W2996263438 cites W2048075532 @default.
- W2996263438 cites W2051992811 @default.
- W2996263438 cites W2053211094 @default.
- W2996263438 cites W2053616931 @default.
- W2996263438 cites W2054101690 @default.
- W2996263438 cites W2054668730 @default.
- W2996263438 cites W2059927626 @default.
- W2996263438 cites W2061906159 @default.
- W2996263438 cites W2068157565 @default.
- W2996263438 cites W2068691195 @default.
- W2996263438 cites W2069277652 @default.
- W2996263438 cites W2070253566 @default.
- W2996263438 cites W2071487482 @default.
- W2996263438 cites W2071604291 @default.
- W2996263438 cites W2072812220 @default.
- W2996263438 cites W2076182220 @default.
- W2996263438 cites W2076314199 @default.
- W2996263438 cites W2080848572 @default.
- W2996263438 cites W2082558157 @default.
- W2996263438 cites W2087510706 @default.
- W2996263438 cites W2088988148 @default.
- W2996263438 cites W2093671367 @default.
- W2996263438 cites W2094074034 @default.
- W2996263438 cites W2098362516 @default.
- W2996263438 cites W2099670382 @default.
- W2996263438 cites W2103789938 @default.
- W2996263438 cites W2103796536 @default.
- W2996263438 cites W2110491183 @default.
- W2996263438 cites W2110499187 @default.
- W2996263438 cites W2110706788 @default.
- W2996263438 cites W2111492115 @default.