Citation: | Hassan Abdelslam Mustafa, Fanxi Liao, Nengsong Chen, Zhendong You, Meshaal Abdelgadir Salih, Lu Wang, Lu Zhang. Early Paleoproterozoic Post-Collisional Basaltic Magmatism in Quanji Massif: Implications for Precambrian Plate Tectonic Regime in NW China. Journal of Earth Science, 2022, 33(3): 706-718. doi: 10.1007/s12583-020-1062-y |
Basaltic magmas can provide important information about mantle source nature, tectonic settings and tectonic evolution for a given terrain. This paper reports geology, petrography and geochemistry of whole-rock major and trace elements and Nd-Sr isotopes for a suite of garnet amphibolites from southeastern Wulan (Ulan), Quanji Massif, northwestern China. The garnet amphibolites were likely generated from basaltic lavas, associated with both paragneisses and orthogneisses of the lower Delingha Group. The basaltic protolith of these amphibolites can be broadly constrained to be formed at ~2.33 Ga in an extensional setting post-collision. The geochemistry of amphibolites shows subalkaline and highly evolved characteristics. They display high-Fe low-Ti characteristics, with TFeO of 13.1 wt.%–17.9 wt.% and TiO2 of 1.42 wt.%–3.09 wt.% (in most samples TiO2 ≤2.5 wt.%). The chondrite-normalized REE patterns show enrichment of LREE and LILE and the primitive-mantle-normalized incompatible element patterns display negative P, Ti, Nb-Ta and Zr-Hf anomalies. The (87Sr/86Sr)
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