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《Geochimica》 1998-06
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GEOCHEMICAL CHARACTERISTICS AND TECTONIC IMPLICATIONS OF POST-COLLISIONAL INTERMEDIATE AND ACID VOLCANIC ROCKS FROM QINLING-DABIE OROGEN

Zhou Wenge; Zhang Benren; Yang Weiran; Zhao Zhidan;Xie Hongsen (Institute of Geochemistry, Chinese Academy Sciences, Guiyang 550002)(China University of Geosciences, Wuhan 430074)  
A geochemical study, on major, trace and earth elements, of post-collisional intermediate and acid volcanic rocks from the Qinling-Dabie orogen was carried out.SiO2 contents of these volcanic rocks range from 55% to 79%; MgO contents are less than 4%; and Na2O + K2O contents are larger than 6%. Major element oxides versus SiO2 diagram shows an overall negative covariance of Al2O3 and CaO with SiO2. The other oxides are more scattered. In the chondrite-normalized abundance diagram, the acid volcanic rocks have negative slopes with large relative depletions of Nb, P, Ti comparing with the similar compatible elements. As for the intermediate volcanic rocks,no any relative depletion of Nb was found and the relative depletions of P and Ti are smaller than those of the acid volcanic rocks. In the chondrites-normalized REE diagram, trachyandesites, andesites, dacites and trachydacites show parallel patterns and small Eu anomalies. However, rhyolites have irregular patterns and show remarkable Eu anomalies. The origin of the post-collision intermediate and acid volcanic rocks is analyzed based on its geochemical characteristics. Intermediate and acid volcanic rocks in this area were derived from the mixture of the basic magma and crustal material,which experienced multi-proccess evolution. Based on the geochemical characteristics of these volcanic rocks, the thermal chronological data and the geological evidence,the tectonic setting during the formation of these volcanic rocks is constrained. It is believed that during the volcanic eruption, the structural setting in the Qinling-Dabie orogenic belt transferred from compressive to extensive regime.
【Fund】: 国家自然科学基金!49290102;;地质矿产部重大基础项目!8502206
【CateGory Index】: P588.1
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