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• W2912803914 abstract "The Xining Basin is well known for its thick and continuous sequence of fine-grained Cenozoic sediments. In addition, it contains important Xiejia fauna which define the Xiejian Stage of the early Miocene in the standard Chinese land mammal zonation, and it also provides detailed histories of eolian dust deposition which document the aridification of Asia, monsoon evolution and the initiation of the Yellow River in relation to the uplift of the Tibetan Plateau. However, the results of magnetostratigraphic dating of the fossil-bearing sequence has yielded conflicting ages for the fauna and stratigraphy, hindering the use of the sequence for addressing major paleoenvironmental and paleoclimatic issues. Here, we review the paleontological, lithological and magnetostratigraphic record of the Xining Basin and provide a new, long and continuous high-resolution magnetostratigraphy from the basin center. The results show that the observed magnetic polarity zones from the various sections at different sites in the basin exhibit similar magnetic polarity patterns which can be readily correlated, in terms of both magnetic polarity zonation and lithofacies; in addition, they show that the sedimentary sequence of the basin was sub-continuously deposited from ~54 Ma to 4.8 Ma. The magnetostratigraphic correlations confirm previous constraint of the Xiejia fauna in the late Oligocene at ~25 Ma, challenging the current Chinese mammal land zonation for the early Miocene, and we suggest that it provides a superior record of eolian dust deposition and river incision in the late Pliocene than previous studies. There is a close match of the climatic proxy records of the Xiejia section, dated by magnetostratigraphy, with the global climatic record which corroborates the paleomagnetic correlations. The evolution of the sedimentary environment provided by the lithofacies demonstrates a complete cycle of basin formation and termination, which records the eastern Qilian Shan experienced three main phases of uplifts: slow episodic uplifts at ~54 Ma and 22.5 Ma and a late rapid episodic uplifts at 8–7 Ma and since 4.8–3.6 Ma. This tectonic uplift in the NE Tibetan Plateau was mostly nearly synchronous responses to the initial and continuing collision of India and Asia since ~50 ± 5 Ma." @default.
• W2912803914 created "2019-02-21" @default.
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• W2912803914 date "2019-03-01" @default.
• W2912803914 modified "2023-10-16" @default.
• W2912803914 title "Cenozoic magnetostratigraphy of the Xining Basin, NE Tibetan Plateau, and its constraints on paleontological, sedimentological and tectonomorphological evolution" @default.
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• W2912803914 cites W1637856870 @default.
• W2912803914 cites W1658256170 @default.
• W2912803914 cites W1826999558 @default.
• W2912803914 cites W1896719854 @default.
• W2912803914 cites W1943104934 @default.
• W2912803914 cites W1965410037 @default.
• W2912803914 cites W1965438059 @default.
• W2912803914 cites W1976467450 @default.
• W2912803914 cites W1981040033 @default.
• W2912803914 cites W1983483408 @default.
• W2912803914 cites W1983602215 @default.
• W2912803914 cites W1985195204 @default.
• W2912803914 cites W1993190436 @default.
• W2912803914 cites W1996923801 @default.
• W2912803914 cites W1997698506 @default.
• W2912803914 cites W2008622484 @default.
• W2912803914 cites W2016581298 @default.
• W2912803914 cites W2019523379 @default.
• W2912803914 cites W2019797998 @default.
• W2912803914 cites W2020551982 @default.
• W2912803914 cites W2026252331 @default.
• W2912803914 cites W2031232581 @default.
• W2912803914 cites W2035424634 @default.
• W2912803914 cites W2040770303 @default.
• W2912803914 cites W2041774199 @default.
• W2912803914 cites W2049109006 @default.
• W2912803914 cites W2050585743 @default.
• W2912803914 cites W2053984125 @default.
• W2912803914 cites W2055442076 @default.
• W2912803914 cites W2058864054 @default.
• W2912803914 cites W2069815139 @default.
• W2912803914 cites W2070253566 @default.
• W2912803914 cites W2072698856 @default.
• W2912803914 cites W2074051603 @default.
• W2912803914 cites W2081241122 @default.
• W2912803914 cites W2083494618 @default.
• W2912803914 cites W2088291813 @default.
• W2912803914 cites W2089315775 @default.
• W2912803914 cites W2090240681 @default.
• W2912803914 cites W2090802740 @default.
• W2912803914 cites W2094074034 @default.
• W2912803914 cites W2094108291 @default.
• W2912803914 cites W2097179538 @default.
• W2912803914 cites W2098727981 @default.
• W2912803914 cites W2099564710 @default.
• W2912803914 cites W2102402389 @default.
• W2912803914 cites W2107391155 @default.
• W2912803914 cites W2112066153 @default.
• W2912803914 cites W2115412787 @default.
• W2912803914 cites W2115518283 @default.
• W2912803914 cites W2120682695 @default.
• W2912803914 cites W2127459091 @default.
• W2912803914 cites W2130176715 @default.
• W2912803914 cites W2135644396 @default.
• W2912803914 cites W2136897436 @default.
• W2912803914 cites W2149277645 @default.
• W2912803914 cites W2152270195 @default.
• W2912803914 cites W2152483812 @default.
• W2912803914 cites W2169131155 @default.
• W2912803914 cites W2174542363 @default.
• W2912803914 cites W2180064451 @default.
• W2912803914 cites W2314299591 @default.
• W2912803914 cites W2324789102 @default.
• W2912803914 cites W2332439330 @default.
• W2912803914 cites W2482348110 @default.
• W2912803914 cites W2509409023 @default.
• W2912803914 cites W2531169012 @default.
• W2912803914 cites W2601795338 @default.
• W2912803914 cites W2604270543 @default.
• W2912803914 cites W2623625738 @default.
• W2912803914 cites W2760497279 @default.
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• W2912803914 doi "https://doi.org/10.1016/j.earscirev.2019.01.021" @default.
• W2912803914 hasPublicationYear "2019" @default.
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