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《Earth Science-Journal of China University of Geosciences》 1993-01
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GEOCHEMISTRY OF BASIC VOLCANIC ROCKS IN NORTHERN QINLING AND THEIR UPPER MANTLE MAGMATIC SOURCES

Ouyang Jianping Zhang Benren Han Yinwen Zheng Haifei Xie Qianli (China University of Geosciences, Wuhan 430074)  
The Proterozoic and Early Palaeozoic were two main periods of volcanic-magmatism in Northern Qinling. It would be possible for the basic volcanic rocks to provide the important information from upper mantle magmatic sources. The Proterozoic basic volcanic rocks had relative low SiO2, A12O3 and high TiO2 , and showed a normal and stable mag-matism in terms of the various relation of TiO2-P2O5, MgO/FeO*-Y and MgO/FeO*-REE. The distribution model of compatible elements applied to the upper mantle partial melt in North China appears to be consistent with the composition of the basalt in the Proterozoic. The Early Palaeozoic basic volcanic rocks had, in addition to high A12O3 and low TiO2, marked nonhomogeneity in their chemical composition, it seems that polygene and mixed magma would cause complicated change of composition relation in magmatic evolution as only single-source. Compatible element distribution model of polygene magma, derived separately from the upper mantle of North China and Northern Qinling, is identical with composition character of the Early Paleozoic. The basic volcanic magmaism in Northern Qinling is related to tectonic development from the Proterozoic to the Early Palaeozoic in the area. It reflects, to a great extent, reformation of the upper mantle and the litho-sphere in Northern Qinling during the two periods. Sr isotope composition also provides the further evidence for the above statement.
【Fund】: 地矿部“七五”秦巴重大项目二级课题“秦巴区域地球化学”;; 国家自然科学基金488150项资助
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