Matches in SemOpenAlex for { <https://semopenalex.org/work/W2274700917> ?p ?o ?g. }
- W2274700917 endingPage "15" @default.
- W2274700917 startingPage "1" @default.
- W2274700917 abstract "The Qinling–Dabie–Sulu orogen is the most prominent Phanerozoic orogenic belt in China. The discovery of ultra-high pressure (UHP) minerals in zircon inclusions suggests that the crust was subducted to deeper than 120 km into the mantle and then exhumed to shallow crustal. Recently, low temperature thermochronology has been applied to constrain the final exhumation of Dabie Shan, while there are few studies describing the Cenozoic exhumation history of the Sulu belt. Here we report some (U–Th)/He ages for various lithologies from Sulu Orogenic belt and its northern part-Jiaobei terrane. The single grain He ages range between 18 and 154 Ma, and most of the samples having large intra-sample age scattering. Several reasons such as invisible U/Th-rich inclusions, grain size effect, slow cooling rate, and zonation of parent nuclide or radiation damage effect may account for this dispersion. For all samples, the pattern of the single grain age data exhibits a peak at ~ 45 Ma which is consistent with the borehole fission-track age pattern in adjacent Hefei Basin. Both (U–Th)/He and fission track ages of the Sulu area suggest an enhanced exhumation/cooling in Early-Middle Eocene in the southern part of Tan-Lu fault zone. This enhanced cooling event coincides with rapid subsidence of North China Basin and rapid uplift of its surrounding reliefs, which indicates basin-mountain coupling. This Eocene event is widespread in central China and could be far-field consequence of India–Asia collision. The convergence rate between Pacific Plate and Eurasia decreased substantially during early Tertiary and reached a minimum in Eocene (~ 30–40 mm/yr) while at the same time the collision between India and Asia was completed. Therefore, the Cenozoic exhumation history of the Sulu Orogenic Belt was a combined result of far-field effect of India–Asia collision and declined subduction rate of the Pacific Plate under Eurasia." @default.
- W2274700917 created "2016-06-24" @default.
- W2274700917 creator A5019647097 @default.
- W2274700917 creator A5022159758 @default.
- W2274700917 creator A5024618200 @default.
- W2274700917 creator A5048768379 @default.
- W2274700917 creator A5057808345 @default.
- W2274700917 creator A5058568334 @default.
- W2274700917 creator A5068218473 @default.
- W2274700917 creator A5086529957 @default.
- W2274700917 date "2016-03-01" @default.
- W2274700917 modified "2023-10-17" @default.
- W2274700917 title "Cenozoic exhumation history of Sulu terrane: Implications from (U–Th)/He thermochrology" @default.
- W2274700917 cites W118755439 @default.
- W2274700917 cites W120028556 @default.
- W2274700917 cites W1523733318 @default.
- W2274700917 cites W1580944979 @default.
- W2274700917 cites W161046653 @default.
- W2274700917 cites W1950684065 @default.
- W2274700917 cites W1957801980 @default.
- W2274700917 cites W1964236143 @default.
- W2274700917 cites W1965443852 @default.
- W2274700917 cites W1967389310 @default.
- W2274700917 cites W1968732925 @default.
- W2274700917 cites W1970079865 @default.
- W2274700917 cites W1970773451 @default.
- W2274700917 cites W1972673996 @default.
- W2274700917 cites W1973844707 @default.
- W2274700917 cites W1976467450 @default.
- W2274700917 cites W1977134448 @default.
- W2274700917 cites W1979476030 @default.
- W2274700917 cites W1981601242 @default.
- W2274700917 cites W1983483408 @default.
- W2274700917 cites W1989610583 @default.
- W2274700917 cites W1989749215 @default.
- W2274700917 cites W1991132092 @default.
- W2274700917 cites W1994209198 @default.
- W2274700917 cites W1994566257 @default.
- W2274700917 cites W1995676444 @default.
- W2274700917 cites W1997092735 @default.
- W2274700917 cites W1998742488 @default.
- W2274700917 cites W2002325302 @default.
- W2274700917 cites W2008892826 @default.
- W2274700917 cites W2009148447 @default.
- W2274700917 cites W2011084451 @default.
- W2274700917 cites W2024090073 @default.
- W2274700917 cites W2028015325 @default.
- W2274700917 cites W2028642961 @default.
- W2274700917 cites W2029970729 @default.
- W2274700917 cites W2031100276 @default.
- W2274700917 cites W2031783355 @default.
- W2274700917 cites W2032001189 @default.
- W2274700917 cites W2034276226 @default.
- W2274700917 cites W2034683722 @default.
- W2274700917 cites W2035003573 @default.
- W2274700917 cites W2037129994 @default.
- W2274700917 cites W2037313368 @default.
- W2274700917 cites W2037950492 @default.
- W2274700917 cites W2038984337 @default.
- W2274700917 cites W2039293130 @default.
- W2274700917 cites W2039681041 @default.
- W2274700917 cites W2040063319 @default.
- W2274700917 cites W2040089183 @default.
- W2274700917 cites W2041774199 @default.
- W2274700917 cites W2042911974 @default.
- W2274700917 cites W2043657636 @default.
- W2274700917 cites W2043708004 @default.
- W2274700917 cites W2048779068 @default.
- W2274700917 cites W2048894507 @default.
- W2274700917 cites W2049826542 @default.
- W2274700917 cites W2051636030 @default.
- W2274700917 cites W2053177516 @default.
- W2274700917 cites W2053422899 @default.
- W2274700917 cites W2054421038 @default.
- W2274700917 cites W2055122293 @default.
- W2274700917 cites W2057162185 @default.
- W2274700917 cites W2058193023 @default.
- W2274700917 cites W2058261858 @default.
- W2274700917 cites W2059653811 @default.
- W2274700917 cites W2063006645 @default.
- W2274700917 cites W2063754919 @default.
- W2274700917 cites W2064449403 @default.
- W2274700917 cites W2065984657 @default.
- W2274700917 cites W2067181219 @default.
- W2274700917 cites W2067480884 @default.
- W2274700917 cites W2068138879 @default.
- W2274700917 cites W2071917865 @default.
- W2274700917 cites W2074841195 @default.
- W2274700917 cites W2075497999 @default.
- W2274700917 cites W2077089229 @default.
- W2274700917 cites W2077428740 @default.
- W2274700917 cites W2077532807 @default.
- W2274700917 cites W2077986876 @default.
- W2274700917 cites W2078261567 @default.
- W2274700917 cites W2083260737 @default.
- W2274700917 cites W2083841543 @default.
- W2274700917 cites W2084045184 @default.
- W2274700917 cites W2086891553 @default.