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Geology, Geochemistry and Geochronology of Neoprotero-zoic Volcanics from Huaiyil Mountains of Southeastern Chi-na: Implication for Its Tectonic Setting and Origin

机译:从东南部淮北山脉围堰的地质,地球化学与地理学和地理学论,东南部山脉:构造与原产地的影响

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On the basis of lithologic association, metamorphism and deformation, the Proterozoic rocks in Huaiyil Mountains can be divided into three successions: Mesoproterozoic Shuangqiaoshan Group, early Neopro-terozoic rocks and later Neoproterozoic Sinian System. The early Neoproterozoic rocks in this range are composed mainly of slates, sandstones, rhyolites, rhyolitic dacites, basalts and basaltic andesites. The Neoproterozoic volcanics have given the Itb-Sr and Sm-Nd isochron ages between 900Ma and 800Ma, which is further confirmed by single zirconU-Pb ages of 8O0-83OMa. Meanwhile, 1638Ma, 2096Ma, 2339Ma and 2378Ma of detrital zircon ages have, been obtained trom rhyolites, which show some, age information of felsic protoliths in the deep crust. The Neoproterozoic volcanics in Huaiyu Mountains show bimodal feature in which the basalts and balastic andesitea exhibit relatively evolved nature in composition and show an enrich-ment of incompatible elements including Ti, Nb and Ta, high SREE contents and highly fractionated REE patterns, inferring continental rift setting. The basalts and basaltic andesites have the relatively low sn
机译:在岩性协会的基础上,翻筋斗和变形,淮北山区的正古代岩石可以分为三次演替:中索佐科双桥山,早期新罗古代岩石及后续新典型山东山东山东省。该范围内的早期内耳古代岩石主要由板岩,砂岩,流螺栓,血管霉菌,玄武岩和玄武岩和玄武岩组成。 NeoproteroZoicoOce Volcanics已经给出了900mA和800mA之间的ITB-SR和SM-ND等象碑,其由80-83岁的单ZIRCONU-PB常年进一步证实。同时,已经获得了1638mA,2096mA,2339mA和2378mA的替代锆石,已经获得了Trom rhyolites,其展示了深海地壳中的肠果促味的某些年龄信息。淮宇山脉的新核古代火山岩展示了双峰特征,其中玄武岩和巴利斯·安塞特省在组成中表现出相对进化的性质,并显示了不相容的元素,包括Ti,Nb和Ta,高Sree含量和高度分馏的REE模式,推断大陆裂缝环境。玄武岩和玄武岩和玄武岩具有相对低的Sn

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