MOLYBDENITE Re-Os ISOTOPIC DATING OF SANGBUJIALA COPPER DEPOSIT IN THE SOUTH MARGIN OF THE EASTERN GANGDESE SECTION, TIBET, AND ITS GEOLOGICAL IMPLICATIONS

ZHAO Zhen; HU Dao-gong; WU Zhen-han; LU Lu

Volume 18 Issue 2

Jun. 2012

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Article Navigation > Journal of Geomechanics > 2012 > 18(2): 178-186

LIU Du Juan, GUO Tao, LU Gu-xian, 2001. THE METALLOGENETIC STRESS FIELD AND RECONSTRUCTION OF DYNAMIC MECHANISM IN FUSHAN GOLD FIELD, SHANDONG. Journal of Geomechanics, 7 (3): 245-253.

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ZHAO Zhen, HU Dao-gong, WU Zhen-han, et al., 2012. MOLYBDENITE Re-Os ISOTOPIC DATING OF SANGBUJIALA COPPER DEPOSIT IN THE SOUTH MARGIN OF THE EASTERN GANGDESE SECTION, TIBET, AND ITS GEOLOGICAL IMPLICATIONS. Journal of Geomechanics, 18 (2): 178-186.

LIU Du Juan, GUO Tao, LU Gu-xian, 2001. THE METALLOGENETIC STRESS FIELD AND RECONSTRUCTION OF DYNAMIC MECHANISM IN FUSHAN GOLD FIELD, SHANDONG. Journal of Geomechanics, 7 (3): 245-253.

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MOLYBDENITE Re-Os ISOTOPIC DATING OF SANGBUJIALA COPPER DEPOSIT IN THE SOUTH MARGIN OF THE EASTERN GANGDESE SECTION, TIBET, AND ITS GEOLOGICAL IMPLICATIONS

1.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
2.
Chinese Academy of Geological Sciences, Beijing 100037, China

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Abstract

Abstract

Located in north side of Yaluzangbujiang Suture, Sangbujiala skarn-type copper deposit is one of the typical polymetallic deposits in the south subzone of the Gangdese metallogenic belt. For the purpose of finding out the mineralization time, the authors selected eight molybdenite samples from Sangbujiala ore district to perform the Re-Os dating. The age of Re-Os isotime line from molybdenite is 93.3±4.1 Ma, with an average model age of 94.5±1.6 Ma. Therefore, the Sangbujiala ore formed during Late Cretaceous, which belongs to the Neo-Tethys subduction stage. The Sangbujiala ore and other Cenozoic deposits showed that the Gangdese metallogenic belt occurring large-scale mineralization in the subduction stage, main collision stage, late collision stage and post-collisional stage, and to form a complete series of metallogenic evolution.
- Re-Os isotope age,
- molybdenite,
- skarn-type copper deposit,
- Gangdese,
- metallogenic evolution

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MOLYBDENITE Re-Os ISOTOPIC DATING OF SANGBUJIALA COPPER DEPOSIT IN THE SOUTH MARGIN OF THE EASTERN GANGDESE SECTION, TIBET, AND ITS GEOLOGICAL IMPLICATIONS

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MOLYBDENITE Re-Os ISOTOPIC DATING OF SANGBUJIALA COPPER DEPOSIT IN THE SOUTH MARGIN OF THE EASTERN GANGDESE SECTION, TIBET, AND ITS GEOLOGICAL IMPLICATIONS

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