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If we have highly sheared and hydrothermally altered metasediments, what are the criteria using which we can differentiate between detrital, metamorphic and hydrothermally formed allanite grains?
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Is it possible to differentiate xenotime from bastnaesite using optical properties?
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is there any method to know the age of an ultramafic body which is now thoroughly altered to serpentinite?
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the ability of hydrotherms produced during thermal metamorphism to mobilize elements largely depends on its oxygen fugacity. Can anyone guide me what exactly are the factors controlling oxygen...
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