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• W2055721201 endingPage "56" @default.
• W2055721201 startingPage "33" @default.
• W2055721201 abstract "The Quanji Massif, located in the northeastern margin of the Tibet Plateau, is interpreted as a fragment of the Tarim Craton. The massif exposes a suite of metamorphosed mafic dykes. LA-ICP-MS U–Pb dating constrains the timing of intrusion of these dykes at ca. 1834 ± 23 Ma. The dykes display minor variations in major elements, with SiO2 = 46.8–53.4 wt%, MgO = 5.19–8.10 wt%, FeOt = 8.83–15.6 wt%, TiO2 = 0.58–1.78 wt% and Mg# = 46.3–69.7. Their immobile trace element compositions show a sub-alkali basalt affinity. The positive correlation of TiO2 with FeOt/MgO in these rocks shows an arc tholeiite evolutionary trend. The enrichment of LILE and LREE and depletion in HFSE suggest that the precursor magma was generated in a back-arc environment. Furthermore, these rocks possess (Nb/La)N of 0.31–0.52 and (Th/La)N of 0.61–1.39, whole rock (87Sr/86Sr)i values of 0.707598–0.724141, ɛNd(t) of −2.9 to +0.3 and (206Pb/204Pb)t of 16.8148–24.1513, (207Pb/204Pb)t of 15.3422–16.3630 and (208Pb/204Pb)t of 36.8415–39.7926. The magmatic zircons yielded ɛHf(t) of −3.4 to +6.1 and depleted mantle model ages (TDM) of 2.01–2.37 Ga. The geochemical and isotopic characteristics of these rocks suggest that their precursor magma was derived from a subduction-related fluid-metasomatized subcontinental lithospheric mantle mixed with a depleted mantle component. We suggest that a prolonged subduction-accretion-collision process along the southeastern margin of the Tarim Craton prevailed at ∼2.1–1.80 Ga, with local consumption of the Southeast Tarim Archipelagic Ocean during the collision of the Southeast Tarim Block with the Quanji Massif (microcontinent) at around 2.1–1.9 Ga. The final closure of the whole Southeast Tarim Archipelagic Ocean occurred at ∼1.85–1.82 Ga and collision between the Southeast margin of the Tarim Craton and other unknown continental blocks at 1.82–1.80 Ga, broadly coeval with the amalgamation of the Western and Eastern Blocks of the North China Craton and their assembly in the Columbia supercontinent." @default.
• W2055721201 created "2016-06-24" @default.
• W2055721201 creator A5000573728 @default.
• W2055721201 creator A5021826323 @default.
• W2055721201 creator A5022310530 @default.
• W2055721201 creator A5041402889 @default.
• W2055721201 creator A5046468748 @default.
• W2055721201 creator A5068285146 @default.
• W2055721201 creator A5074051679 @default.
• W2055721201 date "2014-08-01" @default.
• W2055721201 modified "2023-10-15" @default.
• W2055721201 title "Geochronology and geochemistry of meta-mafic dykes in the Quanji Massif, NW China: Paleoproterozoic evolution of the Tarim Craton and implications for the assembly of the Columbia supercontinent" @default.
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