The industrial mineralogy of magnesite and huntite from eastern Iran
Vein and hydrothermal - sedimentary types of magnesite from eastern Iran probably originated from ascending hydrothermal solutions. The host rocks are part of an ophiolite unit. The cryptocrystalline magnesites are very pure although they have a variable CaO/SiO₂ ratio. The magnesite is compact with...
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University of Hull
1990
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.262297 |