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How Garnet Is Washing In Mongolia

Garnet amphibolite in the Baoyintu Group, Inner Mongolia, is mainly composed of garnet, hornblende, plagioclase, quartz and minor rutile/ilmenite. Garnet occurs as porphyroblasts surrounded by plagioclase, forming typical “white-eye socket” texture. Garnet shows grossular content of 0.26–0.28 and pyrope of 0.11–0.13, without significant

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