The internal structure and geochemistry of many Phanerozoic ophiolites show a complex pattern of igneous accretion that involved multiple stages and sources of melt evolution and life cycles in suprasubduction zone (SSZ) environments ([Shervais, 2001][1]; [Dilek and Flower, 2003][2]). Some of the
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Dilek et al. (2008) studied this question.
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