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Showing 1 to 1 of 1 for “"alteration geochemistry"”.
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Deciphering the signature of fluid/rock reactions in the lower oceanic crust: The Oman ophiolite analogue
… record of fluid circulation reveals that alteration occurred mostly under greenschist facies conditions and continued down to prehnite-pumpellyite facies. However, the textural characteristics of amphibole-rich fault zones imply an earlier, high temperature stage of deformation. The …