【摘 要】
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Helium isotopic composition of inclusion fluid in pyrites from Machangqing copper deposit, China, has been measured. The measurements, with 3He/ 4He
【出 处】
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Chinese Science Bulletin
论文部分内容阅读
Helium isotopic composition of inclusion fluid in pyrites from Machangqing copper deposit, China, has been measured. The measurements, with 3He/ 4He ratios ranging from 0 46-2 08 Ra, indicate that the helium in ore_forming fluid is a mixture of crust and mantle, and are consistent with the fact that the parental magma responsible for the formation of ore_forming fluid of the deposit is of crust_mantle provenance.
Helium isotopic composition of inclusion fluid in pyrites from Machangqing copper deposit, China, has been measured. The measurements, with 3He / 4He ratios ranging from 0 46-2 08 Ra, indicate that the helium in ore_forming fluid is a mixture of crust and mantle , and are consistent with the fact that the parental magma responsible for the formation of ore_forming fluid of the deposit is of crust_mantle provenance.
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