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THE orthorhombic anthophyllite minerals and the monoclinic cummingtonites and grunerites are members of two isomorphous amphibole series of composition (Mg,Fe2+)7Si8O22(OH)2. (All anthophyllites… (More)
THE enrichment of nickel in minerals such as olivine which appear at any early stage during fractional crystallization of magmas is well established1,2. This behaviour of nickel is contrary to all… (More)