Chating Logo Designs, Themes, Templates And Downloadable Graphic Elements On Dribbble

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Its genesis is disputable, primarily skarn sort versus SEDEX type . In this paper, we present proof from detailed area geological investigation and computational geodynamic modeling to assist its epigenetic origin, and provide insights into its ore forming processes. The extraordinarily irregular and sharp boundary of the orebodies and the presence of marble clasts in ores recommend that the ores had been deposited from mineralizing fluids in tensile fracture zones and postdating the formation of the host rocks. The positive relation of the Cu grade and orebody thickness to the Qingshanjiao intrusion signifies the position of the magmatic intrusion in ore formation.

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The Fenghuangshan copper–gold deposit, situated within the Tongling ore cluster field along the Lower Yangtze metallogenic belt in jap China, mainly consist of skarn ores hosted in granodiorite. U–Pb courting of magmatic zircons from Fenghuangshan granodiorite yields a weighted imply 206Pb/238U age of 143.1±1.6Ma. Five molybdenite samples collected within the Fenghuangshan deposit yield a Re–Os isochron age of 141.7±0.8Ma, demonstrating that the ore formation occasion is coeval with the Fenghuangshan granodiorite intrusion. The magmatic zircon ƐHf values range from −12.zero to −28.3, corresponding two-stage Hf mannequin ages between 1.6Ga to 2.4Ga.

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