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• W2086586604 endingPage "230" @default.
• W2086586604 startingPage "209" @default.
• W2086586604 abstract "The Heishan mafic–ultramafic intrusion was emplaced into Neoproterozoic metamorphic strata in the eastern Beishan Fold Belt at the southern margin of the Central Asian Orogenic Belt. The dominant rocks of the intrusion are harzburgite and lherzolite. Olivine gabbro-norite and gabbro dyke occur only along the southern margins of the intrusion. The rocks of the Heishan intrusion are characterized by enrichments of large ion lithophile elements, strong negative Nb (Ta) anomalies and positive K and Pb anomalies. These features are perfectly consistent with those of the Devonian volcanics in the Beishan Fold Belt and indicate subduction-related magmatism. The Heishan intrusive rocks have restricted εNd(t) (+ 0.34 to + 3.95) and a large range of (87Sr/86Sr)t ratios (0.7041 to 0.7087). Their high (207Pb/204Pb)t (15.55–15.64) and (208Pb/204Pb)t (37.71–38.29) values are comparable with those of the volcanics along the Pacific margins of the Americas. Zircon ID-TIMS U–Pb age data (356.4 ± 0.6 Ma and 366.6 ± 0.6 Ma) and SHRIMP U–Pb age data (358 ± 5 Ma and 357 ± 4 Ma) indicate that the intrusion was emplaced in the Late Devonian. Our calculations indicate that the parental magma of the Heishan intrusion had a high-Mg basaltic composition with ~ 11.3 wt.% MgO and ~ 10.0 wt.% FeOT. It is proposed that the high-Mg basaltic magma was generated from partial melting of the asthenosphere and mantle wedge triggered by upwelling of asthenosphere due to slab break-off in an active continental margin." @default.
• W2086586604 created "2016-06-24" @default.
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• W2086586604 date "2012-07-01" @default.
• W2086586604 modified "2023-10-06" @default.
• W2086586604 title "Geochemistry and petrogenetic implications of a Late Devonian mafic–ultramafic intrusion at the southern margin of the Central Asian Orogenic Belt" @default.
• W2086586604 cites W1493314112 @default.
• W2086586604 cites W1566514932 @default.
• W2086586604 cites W1577430152 @default.
• W2086586604 cites W1650609279 @default.
• W2086586604 cites W183765136 @default.
• W2086586604 cites W1963994224 @default.
• W2086586604 cites W1964909252 @default.
• W2086586604 cites W1964977415 @default.
• W2086586604 cites W1970551344 @default.
• W2086586604 cites W1975821545 @default.
• W2086586604 cites W1977875524 @default.
• W2086586604 cites W1978493830 @default.
• W2086586604 cites W1981465880 @default.
• W2086586604 cites W1984911596 @default.
• W2086586604 cites W1987275845 @default.
• W2086586604 cites W1987329135 @default.
• W2086586604 cites W1987997607 @default.
• W2086586604 cites W1991250009 @default.
• W2086586604 cites W1992333048 @default.
• W2086586604 cites W1993916748 @default.
• W2086586604 cites W1996340995 @default.
• W2086586604 cites W1997142214 @default.
• W2086586604 cites W1999326497 @default.
• W2086586604 cites W2000148870 @default.
• W2086586604 cites W2001285983 @default.
• W2086586604 cites W2002256044 @default.
• W2086586604 cites W2003323528 @default.
• W2086586604 cites W2009360266 @default.
• W2086586604 cites W2012351910 @default.
• W2086586604 cites W2013388505 @default.
• W2086586604 cites W2014165584 @default.
• W2086586604 cites W2020384898 @default.
• W2086586604 cites W2029506771 @default.
• W2086586604 cites W2032430672 @default.
• W2086586604 cites W2033084766 @default.
• W2086586604 cites W2036143042 @default.
• W2086586604 cites W2036333570 @default.
• W2086586604 cites W2038323134 @default.
• W2086586604 cites W2040372579 @default.
• W2086586604 cites W2044401903 @default.
• W2086586604 cites W2053339612 @default.
• W2086586604 cites W2055902050 @default.
• W2086586604 cites W2059015933 @default.
• W2086586604 cites W2060655431 @default.
• W2086586604 cites W2065065857 @default.
• W2086586604 cites W2065636104 @default.
• W2086586604 cites W2066028168 @default.
• W2086586604 cites W2068403951 @default.
• W2086586604 cites W2069220978 @default.
• W2086586604 cites W2071093973 @default.
• W2086586604 cites W2076011702 @default.
• W2086586604 cites W2076755830 @default.
• W2086586604 cites W2077577717 @default.
• W2086586604 cites W2080522683 @default.
• W2086586604 cites W2083465209 @default.
• W2086586604 cites W2083774164 @default.
• W2086586604 cites W2089096123 @default.
• W2086586604 cites W2091324857 @default.
• W2086586604 cites W2091757178 @default.
• W2086586604 cites W2099444631 @default.
• W2086586604 cites W2100957263 @default.
• W2086586604 cites W2103463307 @default.
• W2086586604 cites W2112109341 @default.
• W2086586604 cites W2119695127 @default.
• W2086586604 cites W2120941750 @default.
• W2086586604 cites W2123387016 @default.
• W2086586604 cites W2124044757 @default.
• W2086586604 cites W2128624170 @default.
• W2086586604 cites W2129835846 @default.
• W2086586604 cites W2137561172 @default.
• W2086586604 cites W2138150662 @default.
• W2086586604 cites W2138438324 @default.
• W2086586604 cites W2139788788 @default.
• W2086586604 cites W2162335679 @default.
• W2086586604 cites W2162457106 @default.
• W2086586604 cites W2165094726 @default.
• W2086586604 cites W2171801505 @default.
• W2086586604 cites W2332760329 @default.
• W2086586604 cites W4214495636 @default.
• W2086586604 doi "https://doi.org/10.1016/j.lithos.2012.03.010" @default.
• W2086586604 hasPublicationYear "2012" @default.
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