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    Volume 37 Issue 1
    Jan.  2012
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    Article Contents
    JIN Ye, FANG Nian-qiao, YANG Shu-ying, 2012. In Situ Gabbro Geochemical Characteristics and Implications from the Southwest Indian Ocean Ridge. Earth Science, 37(1): 57-68. doi: 10.3799/dqkx.2012.006
    Citation: JIN Ye, FANG Nian-qiao, YANG Shu-ying, 2012. In Situ Gabbro Geochemical Characteristics and Implications from the Southwest Indian Ocean Ridge. Earth Science, 37(1): 57-68. doi: 10.3799/dqkx.2012.006

    In Situ Gabbro Geochemical Characteristics and Implications from the Southwest Indian Ocean Ridge

    doi: 10.3799/dqkx.2012.006
    • Received Date: 2010-11-03
    • Publish Date: 2012-01-15
    • In this paper, geochemical data of the major and trace elements are analyzed for the samples with different depths and lithology of the upper part of ocean drilling program (ODP) ODP 735B hole, Southwest Indian Ocean ridge. Based on these data, together with some other achievements, geochemical comparisions between and within these two cycles are discussed, and their petrogenesis are constrained. The major element characteristics indicate that their variation was well dominated by the mineral assemblage modal which are controlled by fractional crystallization of the rocks. The correlation of the bulk composition of major elements can, to some extent, indicate the formation of minerals and evolution of geochemical characteristics during the crystallization of basaltic melts. Besides the positive Eu anomaly, LREEs are clearly fractionated, while no fractionation of HREEs occurs. The spidergram shows depletion in Nb and Ta, and enrichment in Sr and K; however, this feature cannot be considered as the basis to decide the geochemical characteristics of the source so as to look into the geological significance.

       

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