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The mafic high-pressure rocks of the Tianshan (NW China) display an interconnected network of eclogite-facies veins derived by prograde blueschist dehydration. They provide insight into fluid–rock interaction and element load during long-distance fluid flow occurring due to the major fluid release of subducting oceanic crust. This case study focuses on an eclogite-facies transport vein, its blueschist...
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