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- W2940783539 abstract "The Early Cretaceous sedimentary successions in the Jiaodong-Laiyang (Jiaolai) Basin provide valuable information about sediment provenances and tectonic processes. A clear understanding of the provenance development of the Jiaolai Basin along the northern margin of the Sulu orogen and would elucidate the exhumation history of the Sulu orogen during the post-orogenic period. However, the precise age and provenance evolution of the stratigraphy remain ambiguous. Here, we employ multiple provenance proxies – detailed paleocurrent, conglomerate clast counts, detrital composition point counts of sandstone, and detrital zircon U-Pb geochronology – to reconstruct the source-to-sink system of the northern part of the Jiaolai Basin. Visual and statistical analyses of the different proxy results and comparison with the signatures of potential source regions reveal that (1) Wawukuang Formation (Fm) (ca. 123 Ma) was mainly sourced from the Guocheng uplift in both the Haiyang and Laiyang regions; (2) Linsishan to Zhifengzhuang Fm (ca. 121 Ma), the Laiyang region was mainly fed by the Jiaobei terrane, while in the Haiyang region, the Guocheng uplift and Sulu orogen were primary sources; (3) Shuinan to Longwangzhuang Fm, the Haiyang and Laiyang regions were linked as a single basin fed by the Jiaobei terrane and Sulu orogen; and (4) Qugezhuang Fm (ca. 114 Ma) was mainly sourced from Early Cretaceous plutons in the Sulu orogen and Jiaobei terrane. Based on the inflection point in the proportion of ages of the ultrahigh-pressure metamorphic (UHP) rocks between the Wawukuang and Linsishan Fms, we conclude that the Sulu belt experienced a rapid uplift that resulted in the exposure and erosion of the Jurassic plutons and UHP rocks during ca. 123–121 Ma. In addition, our results show that the denudation processes of the Mesozoic plutons in the Sulu orogen have an obvious temporal sequence: Jurassic plutons first, followed by Cretaceous plutons." @default.
- W2940783539 created "2019-05-03" @default.
- W2940783539 creator A5000198702 @default.
- W2940783539 creator A5016832522 @default.
- W2940783539 creator A5022306333 @default.
- W2940783539 creator A5034027998 @default.
- W2940783539 creator A5055021528 @default.
- W2940783539 creator A5077981606 @default.
- W2940783539 creator A5089899777 @default.
- W2940783539 date "2019-03-01" @default.
- W2940783539 modified "2023-10-03" @default.
- W2940783539 title "Source-to-sink system reconstruction in the northern Jiaolai Basin, eastern China, by multiproxy provenance methods and implications for exhumation of the Sulu orogen" @default.
- W2940783539 cites W1190805272 @default.
- W2940783539 cites W1501081354 @default.
- W2940783539 cites W1580944979 @default.
- W2940783539 cites W1675179255 @default.
- W2940783539 cites W1865561194 @default.
- W2940783539 cites W1898205903 @default.
- W2940783539 cites W1950684065 @default.
- W2940783539 cites W1952095301 @default.
- W2940783539 cites W1957801980 @default.
- W2940783539 cites W1968732925 @default.
- W2940783539 cites W1970079865 @default.
- W2940783539 cites W1970754144 @default.
- W2940783539 cites W1979287378 @default.
- W2940783539 cites W1979854640 @default.
- W2940783539 cites W1980640006 @default.
- W2940783539 cites W1981601242 @default.
- W2940783539 cites W1982960360 @default.
- W2940783539 cites W1983489918 @default.
- W2940783539 cites W1985885839 @default.
- W2940783539 cites W1986702090 @default.
- W2940783539 cites W1989749215 @default.
- W2940783539 cites W1992154287 @default.
- W2940783539 cites W1995387126 @default.
- W2940783539 cites W1996654215 @default.
- W2940783539 cites W1997092735 @default.
- W2940783539 cites W1999573334 @default.
- W2940783539 cites W2009732140 @default.
- W2940783539 cites W2009983465 @default.
- W2940783539 cites W2012863359 @default.
- W2940783539 cites W2015222366 @default.
- W2940783539 cites W2016261729 @default.
- W2940783539 cites W2021508582 @default.
- W2940783539 cites W2031100276 @default.
- W2940783539 cites W2031783355 @default.
- W2940783539 cites W2035980939 @default.
- W2940783539 cites W2048230691 @default.
- W2940783539 cites W2049211279 @default.
- W2940783539 cites W2051636030 @default.
- W2940783539 cites W2052448030 @default.
- W2940783539 cites W2054616290 @default.
- W2940783539 cites W2054911647 @default.
- W2940783539 cites W2058193023 @default.
- W2940783539 cites W2061390528 @default.
- W2940783539 cites W2072751350 @default.
- W2940783539 cites W2075694434 @default.
- W2940783539 cites W2077089229 @default.
- W2940783539 cites W2077112971 @default.
- W2940783539 cites W2077532807 @default.
- W2940783539 cites W2080339133 @default.
- W2940783539 cites W2089048002 @default.
- W2940783539 cites W2089643323 @default.
- W2940783539 cites W2091735058 @default.
- W2940783539 cites W2093299383 @default.
- W2940783539 cites W2093684540 @default.
- W2940783539 cites W2093820708 @default.
- W2940783539 cites W2094090764 @default.
- W2940783539 cites W2097123550 @default.
- W2940783539 cites W2122490144 @default.
- W2940783539 cites W2156586683 @default.
- W2940783539 cites W2159139134 @default.
- W2940783539 cites W2161617180 @default.
- W2940783539 cites W2183427072 @default.
- W2940783539 cites W2195287487 @default.
- W2940783539 cites W2251914726 @default.
- W2940783539 cites W2255386200 @default.
- W2940783539 cites W2264408069 @default.
- W2940783539 cites W2281252973 @default.
- W2940783539 cites W2318795195 @default.
- W2940783539 cites W2321022920 @default.
- W2940783539 cites W2325604355 @default.
- W2940783539 cites W2331165338 @default.
- W2940783539 cites W2346302770 @default.
- W2940783539 cites W2369645039 @default.
- W2940783539 cites W2396913702 @default.
- W2940783539 cites W2514585848 @default.
- W2940783539 cites W2530142661 @default.
- W2940783539 cites W2544359449 @default.
- W2940783539 cites W2565505752 @default.
- W2940783539 cites W2605130328 @default.
- W2940783539 cites W2611939562 @default.
- W2940783539 cites W2620963156 @default.
- W2940783539 cites W2696898621 @default.
- W2940783539 cites W2796600848 @default.
- W2940783539 cites W4249068219 @default.
- W2940783539 cites W637959080 @default.
- W2940783539 doi "https://doi.org/10.1016/j.tecto.2019.01.009" @default.