Structural analysis of the Hasan-Robat marbles as traces of folded basement in the Sanandaj–Sirjan Zone, Iran
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Lots of granitoids occur in north Kunlun faults zone of western Qaidam Basin. Comprehensive petrology,laser ablation ICPMS zircon U-Pb geochronology( LA-ICPMS U-Pb) and geochemistry of drilling basement granites were carried out from north Kunlun faults zone,western Qaidam Basin. Zircon U-Pb isotopic ages of 467 ~ 450Ma,i. e. Middle-Late Ordovician,show the crystallization age of the basement granites which belong to the Caledonian magmatic cycles. Detailed geochemical analyses show that the basement granites are per-aluminous and high-K calc-alkaline series,characterized by obvious LREE enrichment with medium to strong negative Eu anomalies. These geochemical features indicate that the basement granites probably resulted from crustal remelting of syn-collision setting. There exist Middle Ordovician-Early Silurian Caledonian tectonic-magmatic events,which provide important information for the researches on magmatic and tectonic evolution in north Kunlun faults zone and its west.
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