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- W3208454664 endingPage "406" @default.
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- W3208454664 abstract "Abstract The uplift history of northeastern Asian continental margin has been the subject of much debate. The Sanjiang Basin is an ideal area to investigate the uplift history of this margin. We present new data from sandstone petrology, whole-rock geochemistry, U–Pb geochronology and Hf isotopy of detrital zircons to trace the provenance of the basin and to unravel the uplift history of the northeastern Asian continental margin. We investigated the chemical and plagioclase indices of alteration and index of compositional variability (CIA, PIA and ICV, respectively) in samples from two formations. The geochemical proxies indicate that source rocks were subjected to an intensified weathering process. Based on the high SiO 2 /Al 2 O 3 values and low K 2 O, we infer that the two basinal strata experienced silicification and insignificant potassium metasomatism. Sandstone petrography is indicative of low degrees of sedimentary sorting, suggesting a proximal deposition. The provenance fingerprints of light rare earth, high-field-strength and transition metal elements indicate that parts of the provenance included recycled sediments, and that first-cycle sediments were derived mainly from felsic rocks with a minor contribution from intermediate and mafic rocks. The combined detrital zircon U–Pb ages and Hf isotopic results constrain the contributions of different source terranes over time. The provenance results, in combination with seismic profile interpretations from the Sanjiang Basin, suggest that the northeastern Asian continental margin experienced at least three stages of uplift, which were driven by subduction initiation of the Paleo-Pacific Ocean during the Jurassic Period, a plate motion change during the Early Cretaceous Epoch, and a shallowing of the slab dip angle during the Late Cretaceous Epoch." @default.
- W3208454664 created "2021-11-08" @default.
- W3208454664 creator A5034001966 @default.
- W3208454664 creator A5046053996 @default.
- W3208454664 creator A5078319373 @default.
- W3208454664 date "2021-11-03" @default.
- W3208454664 modified "2023-10-18" @default.
- W3208454664 title "Provenance and depositional history of the Mesozoic Sanjiang Basin (northeastern China): implications for the uplift history of the northeastern Asian continental margin" @default.
- W3208454664 cites W1100243556 @default.
- W3208454664 cites W1104249897 @default.
- W3208454664 cites W141993106 @default.
- W3208454664 cites W1587780337 @default.
- W3208454664 cites W1852220267 @default.
- W3208454664 cites W1876747383 @default.
- W3208454664 cites W1965536973 @default.
- W3208454664 cites W1967827341 @default.
- W3208454664 cites W1968074090 @default.
- W3208454664 cites W1971733245 @default.
- W3208454664 cites W1977880023 @default.
- W3208454664 cites W1980600502 @default.
- W3208454664 cites W1980640006 @default.
- W3208454664 cites W1984617079 @default.
- W3208454664 cites W1986886630 @default.
- W3208454664 cites W1988627424 @default.
- W3208454664 cites W1989478869 @default.
- W3208454664 cites W1992903217 @default.
- W3208454664 cites W1994233909 @default.
- W3208454664 cites W1999621813 @default.
- W3208454664 cites W2005350578 @default.
- W3208454664 cites W2010781943 @default.
- W3208454664 cites W2011611022 @default.
- W3208454664 cites W2015876559 @default.
- W3208454664 cites W2016223358 @default.
- W3208454664 cites W2016536555 @default.
- W3208454664 cites W2017647068 @default.
- W3208454664 cites W2020139762 @default.
- W3208454664 cites W2022859730 @default.
- W3208454664 cites W2023621032 @default.
- W3208454664 cites W2025069593 @default.
- W3208454664 cites W2029401070 @default.
- W3208454664 cites W2044911516 @default.
- W3208454664 cites W2049340605 @default.
- W3208454664 cites W2050716036 @default.
- W3208454664 cites W2050912197 @default.
- W3208454664 cites W2053587074 @default.
- W3208454664 cites W2062961346 @default.
- W3208454664 cites W2072680255 @default.
- W3208454664 cites W2074114517 @default.
- W3208454664 cites W2074343720 @default.
- W3208454664 cites W2078195267 @default.
- W3208454664 cites W2083645617 @default.
- W3208454664 cites W2084051225 @default.
- W3208454664 cites W2087937118 @default.
- W3208454664 cites W2089096123 @default.
- W3208454664 cites W2093820542 @default.
- W3208454664 cites W2110531414 @default.
- W3208454664 cites W2117879248 @default.
- W3208454664 cites W2118591942 @default.
- W3208454664 cites W2121397859 @default.
- W3208454664 cites W2123600791 @default.
- W3208454664 cites W2123985829 @default.
- W3208454664 cites W2126573066 @default.
- W3208454664 cites W2134490602 @default.
- W3208454664 cites W2137335718 @default.
- W3208454664 cites W2140093647 @default.
- W3208454664 cites W2142031556 @default.
- W3208454664 cites W2161346058 @default.
- W3208454664 cites W2162334444 @default.
- W3208454664 cites W2162898351 @default.
- W3208454664 cites W2171086159 @default.
- W3208454664 cites W2214450867 @default.
- W3208454664 cites W2247098479 @default.
- W3208454664 cites W2331273514 @default.
- W3208454664 cites W2394135397 @default.
- W3208454664 cites W2530479946 @default.
- W3208454664 cites W2545937306 @default.
- W3208454664 cites W2552762488 @default.
- W3208454664 cites W2554936634 @default.
- W3208454664 cites W2555164195 @default.
- W3208454664 cites W2605428171 @default.
- W3208454664 cites W2607736094 @default.
- W3208454664 cites W2609574058 @default.
- W3208454664 cites W2617199804 @default.
- W3208454664 cites W2619868733 @default.
- W3208454664 cites W2629885935 @default.
- W3208454664 cites W2756282726 @default.
- W3208454664 cites W2767324758 @default.
- W3208454664 cites W2791283863 @default.
- W3208454664 cites W2794194473 @default.
- W3208454664 cites W2890033278 @default.
- W3208454664 cites W2895673797 @default.
- W3208454664 cites W2899737432 @default.
- W3208454664 cites W2916755135 @default.
- W3208454664 cites W2931011700 @default.
- W3208454664 cites W2962848136 @default.
- W3208454664 cites W2970268617 @default.
- W3208454664 cites W2979989490 @default.
- W3208454664 cites W3017418187 @default.