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有机质的热液成熟作用在云南金顶铅锌矿床形成过程中的意义
引用本文:胡明安.有机质的热液成熟作用在云南金顶铅锌矿床形成过程中的意义[J].地球科学,1989,14(5):503-512.
作者姓名:胡明安
作者单位:China University of Geosciences,Wuhan 430074
摘    要:

关 键 词:有机地球化学  含矿热液  铅锌矿床

HYDROTHERMAL MATURATION OF INDIGENOUS ORGANIC MATTERS AND THEIR SIGNIFICANCE IN THE METALLOGE-NIC PROCESSES OF THE JINDING LEAD-ZINC DEPOSIT,YUNNAN PROVINCE
Hu Ming''''an.HYDROTHERMAL MATURATION OF INDIGENOUS ORGANIC MATTERS AND THEIR SIGNIFICANCE IN THE METALLOGE-NIC PROCESSES OF THE JINDING LEAD-ZINC DEPOSIT,YUNNAN PROVINCE[J].Earth Science-Journal of China University of Geosciences,1989,14(5):503-512.
Authors:Hu Ming'an
Abstract:There are a lot of organic matters in the Jinding lead-zinc deposit. The organic matters can be distingushed as three types by their occurrence, a) the indigenous type, b) the type of hydrothermal metamorphism.c) the type of migration. The studies of organic geochemistry demonstrate that the indigenous organic matters in the host rock are in immature stage or low-grade mature stage. The thermal degradation of the indigenous organic matters resulted from ore-bearing hydrother-matism, then the anomaly of hydrothermal maturation is formed. As a result of the reaction of the ore-bearing hydrothermal fluid a lot of hydrogen sulfides are produced by partial organic matters.This process generates precipitation and enrichment of the metallic sulfides. Studies on the distributive form of thermal mature anomaly of the organic matters are a great help to research and exploration of the Jinding-type lead-zinc deposit.
Keywords:organic geochemistry  ore-bearing hydrothermal solution  thermal mature anomaly  lead-zinc mineralization  Yunnan Jinding
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