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Geochemical Characteristics and Tectonic Significance of the Acidic Volcanic Rocks from the Shetang-Boyang Area, Western Qinling Orogenic Belt, China

机译:西秦岭造山带蛇塘-博阳地区酸性火山岩的地球化学特征及其构造意义

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Acidic volcanic rocks of Shetang-Boyang area are located in the western Qinling orogenic belt, consist of rhyolite and granite porphyry. They are comparable in the chemical composition, enriched in Si, alkali, Al and a little bit of Mg, Ca and Ti. The contents of HFSE (Zr, Hf) and LILE (Rb, Th, U) are high, however, the content of Ba, Sr, Ti, P have obviously depleted and there are obvious negative Eu anomalies (Eu/Eu*=0.06-0.13). These geochemical characteristics are revealed that these volcanic rocks have an A1 type affinity. Geochemical data combined with regional studies, show that these volcanic rocks were formed in a continental extension setting and the western Qinling orogenic belt in 211Ma has been in the tectonic setting of post-collisional extension.
机译:蛇塘-博阳地区的酸性火山岩位于秦岭西部造山带,由流纹岩和花岗岩斑岩组成。它们的化学组成相当,富含硅,碱,铝以及少量的镁,钙和钛。 HFSE(Zr,Hf)和LILE(Rb,Th,U)的含量较高,但是Ba,Sr,Ti,P的含量明显耗尽,并且存在明显的负Eu异常(Eu / Eu * = 0.06)。 -0.13)。这些地球化学特征表明,这些火山岩具有A1型亲和力。地球化学数据与区域研究相结合,表明这些火山岩形成于大陆伸展带,而211Ma秦岭西部造山带一直处于碰撞后伸展的构造环境。

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