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• W3199763105 abstract "Abstract Understanding the processes and mechanisms responsible for exhumation are essential for determining the evolution of landscapes. Our knowledge of these issues in continental convergent margins is still incomplete despite decades of research. Here, we present a record of exhumation rates obtained from thermochronology across the collision zone of the Himalayan‐Tibetan orogen, which has been carved by the dextral Karakoram fault (KF) along its western margin. Our thermochronology results across the KF suggest that transpression controlled exhumation from ∼10 to 8 Ma. Exhumation rates at the margin of the Tibetan plateau, in the SE Karakoram range, to the north of the KF are twice as high as the Ladakh range, to the south of the KF, since at least middle Miocene. We hypothesize that rapid exhumation of the Tibetan margin was in response to topographic uplift and subsequent erosion due to the convective removal of the lower lithosphere, triggered by the rollback of the subducting Indian lower crust during the Oligocene‐Miocene in an early phase. Our thermochronology results document an additional two‐fold increase in the exhumation rates of the Tibetan margin since the late Mio‐Pliocene. We propose that the underthrusting of the Indian Plate below Tibet during the late Mio‐Pliocene was responsible for this additional increase of exhumation rates of the Tibetan margin in the late phase. These exhumation rates are in good agreement with the topographic slope, relief, and channel steepness data of these regions. Thus, the coupling of tectonics and topography dictated the exhumation patterns since late Mio‐Pliocene." @default.
• W3199763105 created "2021-09-27" @default.
• W3199763105 creator A5015630682 @default.
• W3199763105 creator A5018066782 @default.
• W3199763105 creator A5034501717 @default.
• W3199763105 creator A5086165333 @default.
• W3199763105 date "2021-10-01" @default.
• W3199763105 modified "2023-10-10" @default.
• W3199763105 title "Tectonic Control Over Shallow Crustal Exhumation Across the India‐Asia Convergent Margin" @default.
• W3199763105 cites W1520954582 @default.
• W3199763105 cites W1521156282 @default.
• W3199763105 cites W1527871403 @default.
• W3199763105 cites W1533315712 @default.
• W3199763105 cites W1561132610 @default.
• W3199763105 cites W1571565806 @default.
• W3199763105 cites W1612049120 @default.
• W3199763105 cites W1613362835 @default.
• W3199763105 cites W1623701821 @default.
• W3199763105 cites W1658256170 @default.
• W3199763105 cites W1660674569 @default.
• W3199763105 cites W1685716106 @default.
• W3199763105 cites W173402686 @default.
• W3199763105 cites W1769452332 @default.
• W3199763105 cites W1846174530 @default.
• W3199763105 cites W1883962991 @default.
• W3199763105 cites W1963598772 @default.
• W3199763105 cites W1965732067 @default.
• W3199763105 cites W1966431820 @default.
• W3199763105 cites W1968955406 @default.
• W3199763105 cites W1969894116 @default.
• W3199763105 cites W1970268065 @default.
• W3199763105 cites W1973926757 @default.
• W3199763105 cites W1974467019 @default.
• W3199763105 cites W1976166881 @default.
• W3199763105 cites W1976467450 @default.
• W3199763105 cites W1977442136 @default.
• W3199763105 cites W1977755373 @default.
• W3199763105 cites W1978640446 @default.
• W3199763105 cites W1978787042 @default.
• W3199763105 cites W1981369543 @default.
• W3199763105 cites W1986228949 @default.
• W3199763105 cites W1987562178 @default.
• W3199763105 cites W1990103216 @default.
• W3199763105 cites W1993519551 @default.
• W3199763105 cites W1996284045 @default.
• W3199763105 cites W1996994351 @default.
• W3199763105 cites W1998585045 @default.
• W3199763105 cites W1999757103 @default.
• W3199763105 cites W2005110508 @default.
• W3199763105 cites W2007382743 @default.
• W3199763105 cites W2009851579 @default.
• W3199763105 cites W2011055705 @default.
• W3199763105 cites W2016056728 @default.
• W3199763105 cites W2016643944 @default.
• W3199763105 cites W2016904677 @default.
• W3199763105 cites W2019916967 @default.
• W3199763105 cites W2020527814 @default.
• W3199763105 cites W2022909854 @default.
• W3199763105 cites W2024005564 @default.
• W3199763105 cites W2024259689 @default.
• W3199763105 cites W2024305702 @default.
• W3199763105 cites W2024462757 @default.
• W3199763105 cites W2025441790 @default.
• W3199763105 cites W2028243111 @default.
• W3199763105 cites W2028759234 @default.
• W3199763105 cites W2030642484 @default.
• W3199763105 cites W2031242600 @default.
• W3199763105 cites W2033045898 @default.
• W3199763105 cites W2033121371 @default.
• W3199763105 cites W2033265152 @default.
• W3199763105 cites W2034459516 @default.
• W3199763105 cites W2035621835 @default.
• W3199763105 cites W2035737599 @default.
• W3199763105 cites W2036709818 @default.
• W3199763105 cites W2036936972 @default.
• W3199763105 cites W2037405321 @default.
• W3199763105 cites W2038367331 @default.
• W3199763105 cites W2040368577 @default.
• W3199763105 cites W2040714581 @default.
• W3199763105 cites W2041837766 @default.
• W3199763105 cites W2043117138 @default.
• W3199763105 cites W2043624522 @default.
• W3199763105 cites W2045699793 @default.
• W3199763105 cites W2048084754 @default.
• W3199763105 cites W2049397443 @default.
• W3199763105 cites W2049946327 @default.
• W3199763105 cites W2050487135 @default.
• W3199763105 cites W2053952273 @default.
• W3199763105 cites W2055356153 @default.
• W3199763105 cites W2055457776 @default.
• W3199763105 cites W2056398906 @default.
• W3199763105 cites W2060839143 @default.
• W3199763105 cites W2061335808 @default.
• W3199763105 cites W2062011476 @default.
• W3199763105 cites W2062032100 @default.
• W3199763105 cites W2062393489 @default.
• W3199763105 cites W2063215451 @default.
• W3199763105 cites W2063307255 @default.
• W3199763105 cites W2064288238 @default.
• W3199763105 cites W2064814762 @default.

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