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ORIGIN OF ORE-FORMING FLUIDS OF THE BANGPU PORPHYRY MO(CU) DEPOSIT, TIBET: EVIDENCE FROM HELIUM AND ARGON ISOTOPE IN PYRITES
LUO MAOCHENG; TANG JUXING; MAO JINGWEN; WANG LIQIANG; CHEN WEI; LENG QIUFENG
2013
会议日期2013年6月17日
会议地点成都
关键词HELIUMANDARGONISOTOPE PYRITE ORE-FORMINGFLUID BANGPUMO(CU)DEPOSIT TIBET
会议录THE FIRST JOINT SCIENTIFIC MEETING OF GEOLOGICAL SOCIETY OF CHINA AND GEOLOGICAL SOCIETY OF AMERICA(ROOF OF THE WORLD)(第一届中国地质学会与美国地质学会联合学术会议——世界屋脊讨论会)论文集
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内容类型会议论文
URI标识http://www.corc.org.cn/handle/1471x/4664470
专题成都理工大学
作者单位1.[1]SCHOOL OF EARTH SCIENCES AND RESOURCES, CHINA UNIVERSITY OF GEOSCIENCES, BEIJING 100083, CHINA
2.[2]MLR KEY LABORATORY OF METALLOGENY AND MINERAL ASSESSMENT, INSTITUTE OF MINERAL RESOURCES, CHINESE ACADEMY OF GEOLOGICAL SCIENCES, BEIJING 100037, CHINA
3.[3]COLLEGE OF EARTH SCIENCES, CHENGDU UNIVERSITY OF TECHNOLOGY, CHENGDU, SICHUAN, 610059, CHINA
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LUO MAOCHENG,TANG JUXING,MAO JINGWEN,et al. ORIGIN OF ORE-FORMING FLUIDS OF THE BANGPU PORPHYRY MO(CU) DEPOSIT, TIBET: EVIDENCE FROM HELIUM AND ARGON ISOTOPE IN PYRITES[C]. 见:. 成都. 2013年6月17日.
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