THE ISOTOPIC GEOCHEMISTRY OF ORE DEPOSITS AND COGNATE ROCKS IN ANJIAYINGZI GOLD FIELD
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Graphical Abstract
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Abstract
Study on the S,Pb,C,O,H and Sr isotopes shows that:(1)the ore-forming substances of Anjiayingzi gold field were mianly derived from deep magmatic source;(2)the ore-forming fluid was re-equilibrated magmatic water;and(3)Anjiayingzi adamellite mass related to gold deposits was derived from remelting lower crust rocks,it should belong to Au-Cu series granitoid.The minerogenetic ages of gold deposits are 120~130Ma.
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