%0 Journal Article %T LA-ICPMS zircon U-Pb ages and geochemistry of Neoproterozoic low-grade metavolcanic rocks in Wuyuan-Dexing area of northeastern Jianxi Province
赣东北婺源-德兴地区新元古代浅变质火山岩的地球化学和锆石U-Pb年龄 %A LIU ShuWen %A YANG PengTao %A WANG ZongQi %A LUO Ping %A WANG YongQing %A LUO GuoHui %A WANG Wei %A GUO BoRan %A
刘树文 %A 杨朋涛 %A 王宗起 %A 罗平 %A 王永庆 %A 罗国辉 %A 王伟 %A 郭博然 %J 岩石学报 %D 2013 %I %X Low-grade metamorphosed volcanic rocks consist mainly of metamorphic basalt, dacite and rhyolite in the Wuyuan to Dexing region of the northeastern Jiangxi Province. Whole-rock geochemical analyses reveal that the metabasalt has chemical features of the tholeiite, and the basaltic magma originated from low-degreed partial melting of a spinel lhezolite in disturbed deleted mantle. However, the dacitic magma was derived from a partial melting of a meta-greywacke, and the rhyolite was produced by the fractionation of the dacitic magma. LA-ICP-MS zircon U-Pb isotope dating indicates low-grade meta-dacite from the Wuyuan area was formed at 861±8Ma, and meta-rhyolite and tuffaceous slate from the Dexing area at 860±3Ma and 860±6Ma, respectively, which indicate that these metamorphic volcanic rocks erupted at Neoproterozoic Tonian era. Meanwhile, these samples also preserved some signatures of Neoarchean (2.8~2.5Ga), Middle-Late Paleoproterozoic (2.0~1.7Ga) and Mesoproterozoic (~1.0 Ga) inherited and/or captured zircon ages. Integrated the whole-rock geochemistry, petrogenesis and zircon ages, we suggest that these metamorphic volcanic rocks formed under an Early Neoproterozoic tectonic background of back-arc basin in Andes-type actively continental margin. %K Low-grade metamorphosed volcanic rocks %K Whole-rock petrochemistry %K LA-ICP-MS zircon U-Pb isotope ages %K Petrogenesis %K Tectonic background %K Northeast Jiangxi Province
浅变质火山 %K 岩石地球化学 %K LA-ICP-MS锆石U-Pb年龄 %K 岩石成因 %K 构造背景 %K 赣东北地区 %U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=2013B5467E3054B1614CEC199353FCED&aid=423E4EA2B40352F0C976ABD8630F997C&yid=FF7AA908D58E97FA&vid=771469D9D58C34FF&iid=0B39A22176CE99FB&sid=93ADA2AA3F969E58&eid=2EAE52BA5B1222A9&journal_id=1000-0569&journal_name=岩石学报&referenced_num=0&reference_num=47