西秦岭造山带蛇塘—博阳地区酸性火山岩地球化学特征及构造意义

A. Ma, Hao Guan, Lifei Zou, Lanlan Sun
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摘要

射塘—博阳地区酸性火山岩位于西秦岭造山带,由流纹岩和花岗斑岩组成。它们的化学成分相似,富含硅、碱、铝和少量的镁、钙和钛。HFSE (Zr、Hf)和LILE (Rb、Th、U)含量较高,Ba、Sr、Ti、P含量明显减少,Eu呈明显负异常(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。地球化学资料结合区域研究表明,这些火山岩形成于大陆伸展环境,西秦岭造山带2111ma时期处于碰撞后伸展构造环境。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geochemical Characteristics and Tectonic Significance of the Acidic Volcanic Rocks from the Shetang-Boyang Area, Western Qinling Orogenic Belt, China
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 A 1 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.
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