FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4286436698> ?p ?o ?g. }

• W4286436698 endingPage "103897" @default.
• W4286436698 startingPage "103897" @default.
• W4286436698 abstract "Rapid denudation and uplift of eastern Tibet have accelerated during the Late Miocene due to lateral lower crustal flow, without a significant contribution from upper crustal shortening. However, growing lines of evidence have revealed that Early Cenozoic faulting controlled enhanced denudation and shortening. Here, we report 51 new zircon and apatite (UTh)/He and apatite fission-track ages from seven granite samples along one primary branch fault (the Yunongxi fault) of the Yalong thrust belt in eastern Tibet. Cooling ages and inverse thermal modeling revealed two pulses of accelerated exhumation during the Late Cretaceous (70–65 Ma) and the Late Eocene–Early Oligocene (40–30 Ma). We suspect that the surface uplift of eastern Tibet, due to the convergence rate acceleration between India and Eurasia, triggered the first cooling stage. A synchronous out-of-pace Early Cenozoic cooling pattern across the Yunongxi fault was further identified and could be due to fault initiation at ca. 40–30 Ma. We argue that the Late Eocene–Early Oligocene rapid cooling and exhumation and the associated outward plateau growth were primarily accommodated through upper-crust faulting along the Yalong–Longmen Shan thrust belt. This deformation pulse was the first-stage response of fault activity to the India–Eurasia collision in eastern Tibet. More extensive Late Miocene deformation driven by lateral lower crustal flow consequently bypassed these early-stage fault systems and overwhelmed the Late Cretaceous and Late Eocene–Early Oligocene deformation in eastern Tibet." @default.
• W4286436698 created "2022-07-22" @default.
• W4286436698 creator A5007569973 @default.
• W4286436698 creator A5010833233 @default.
• W4286436698 creator A5016981787 @default.
• W4286436698 creator A5018863416 @default.
• W4286436698 creator A5025526333 @default.
• W4286436698 creator A5041985756 @default.
• W4286436698 creator A5055359924 @default.
• W4286436698 creator A5070049908 @default.
• W4286436698 creator A5091543149 @default.
• W4286436698 date "2022-09-01" @default.
• W4286436698 modified "2023-10-18" @default.
• W4286436698 title "Late Cretaceous–Early Cenozoic exhumation across the Yalong thrust belt in eastern Tibet and its implications for outward plateau growth" @default.
• W4286436698 cites W1511845621 @default.
• W4286436698 cites W1514116682 @default.
• W4286436698 cites W1528695685 @default.
• W4286436698 cites W1592988921 @default.
• W4286436698 cites W1597063492 @default.
• W4286436698 cites W1608334880 @default.
• W4286436698 cites W1612050563 @default.
• W4286436698 cites W1658256170 @default.
• W4286436698 cites W1803908422 @default.
• W4286436698 cites W1905764703 @default.
• W4286436698 cites W1905885784 @default.
• W4286436698 cites W1946512236 @default.
• W4286436698 cites W1949804026 @default.
• W4286436698 cites W1968771872 @default.
• W4286436698 cites W1969599221 @default.
• W4286436698 cites W1974467019 @default.
• W4286436698 cites W1974469836 @default.
• W4286436698 cites W1975635298 @default.
• W4286436698 cites W1979867347 @default.
• W4286436698 cites W1983483408 @default.
• W4286436698 cites W1991149963 @default.
• W4286436698 cites W2002325302 @default.
• W4286436698 cites W2011834231 @default.
• W4286436698 cites W2018092557 @default.
• W4286436698 cites W2018693288 @default.
• W4286436698 cites W2026142722 @default.
• W4286436698 cites W2029683395 @default.
• W4286436698 cites W2033837022 @default.
• W4286436698 cites W2037898567 @default.
• W4286436698 cites W2038907414 @default.
• W4286436698 cites W2040177180 @default.
• W4286436698 cites W2041455558 @default.
• W4286436698 cites W2041774199 @default.
• W4286436698 cites W2042730394 @default.
• W4286436698 cites W2049109006 @default.
• W4286436698 cites W2054359522 @default.
• W4286436698 cites W2058958898 @default.
• W4286436698 cites W2068157565 @default.
• W4286436698 cites W2073350342 @default.
• W4286436698 cites W2079237883 @default.
• W4286436698 cites W2079335235 @default.
• W4286436698 cites W2080719977 @default.
• W4286436698 cites W2087665583 @default.
• W4286436698 cites W2087932839 @default.
• W4286436698 cites W2102402389 @default.
• W4286436698 cites W2103018800 @default.
• W4286436698 cites W2103294084 @default.
• W4286436698 cites W2108237083 @default.
• W4286436698 cites W2115518283 @default.
• W4286436698 cites W2116926271 @default.
• W4286436698 cites W2121076941 @default.
• W4286436698 cites W2121412830 @default.
• W4286436698 cites W2122084771 @default.
• W4286436698 cites W2123464034 @default.
• W4286436698 cites W2123779550 @default.
• W4286436698 cites W2123919931 @default.
• W4286436698 cites W2128610717 @default.
• W4286436698 cites W2145180142 @default.
• W4286436698 cites W2145347294 @default.
• W4286436698 cites W2148691236 @default.
• W4286436698 cites W2149147576 @default.
• W4286436698 cites W2149567728 @default.
• W4286436698 cites W2151546086 @default.
• W4286436698 cites W2153331827 @default.
• W4286436698 cites W2164177118 @default.
• W4286436698 cites W2169799081 @default.
• W4286436698 cites W2170853118 @default.
• W4286436698 cites W2171246464 @default.
• W4286436698 cites W2312320844 @default.
• W4286436698 cites W2417407591 @default.
• W4286436698 cites W2509257985 @default.
• W4286436698 cites W2520226227 @default.
• W4286436698 cites W2587672488 @default.
• W4286436698 cites W2592645024 @default.
• W4286436698 cites W2595137703 @default.
• W4286436698 cites W2603434560 @default.
• W4286436698 cites W2605216192 @default.
• W4286436698 cites W2612691354 @default.
• W4286436698 cites W2614330085 @default.
• W4286436698 cites W2614449567 @default.
• W4286436698 cites W2708550365 @default.
• W4286436698 cites W2766953446 @default.
• W4286436698 cites W2790068644 @default.
• W4286436698 cites W2795372622 @default.

• next