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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2005-05
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Sm and Nd isotopic geochemistry of Paleo-Mesoproterozoic meta-basic volcanics from Middle Hainan,China

XU De-ming,XIE Cai-fu,FU Tai-an,ZHANG Ye-ming,LI Zhi-hongYichang Institute of Geology and Mineral Resources,Yichang 443003,China  
The protolith of the plagioamphibolites in Middle Hainan is the metamorphosed Paleo-Mesoproterozoic basic volcanics.It belongs to a suit of high-K calc-alkaline basalts with high Al and low Ti contents.The volcanic rocks have characteristics of typical island-arc basalts.Large-ion elements(LILE) are evidently enriched and high field strength elements(HFSE) relatively depleted the volcanic rocks.The geochemical features of trace elements and Sm/Nd isotopes also indicate that magama source is departed from the composition of primary mantle and not evidently contaminated by mature crust materials.It is the result of patial melting of two-coponent mixture made of the mantle wedge(the MORB type depleted mantle) located over subducted zone and the fluid released from the subducted oceanic crust.During Paleo-Mesoproterozoic Age,the Hainan block might have suffered geodynamic shifting from "extending" to "squeezing",leading to form oceanic-ridge type and oceanic-arc transitional tholeiites in the western Hainan at earlier extending stage and high-K calc-alkaline basalts in the middle Hainan at later strong subduction stage,while the South China unified block was subducting.
【Fund】: 中国地质调查局国土资源大调查项目(20013900018)
【CateGory Index】: P588.14;
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