兰坪金顶铅锌矿床泥底辟流体成矿特征初探
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引用本文:唐菊兴,范小华,陈洪德,陈生华,陈文彬,王成辉,解惠.2010.A tentative discussion on mud diapiric fluid metallogenic characteristics of Jinding lead-zinc deposit in Lanping [J].Mineral Deposits,29(2):361~370
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Author NameAffiliation
张峰 成都理工大学沉积地质研究院 
唐菊兴,范小华 中国地质科学院矿产资源研究所 
陈洪德 成都理工大学沉积地质研究院 
陈生华 中国科学院地球化学研究所环境地球化学国家重点实验室 
陈文彬 中国地质大学 
王成辉 中国地质科学院矿产资源研究所 
解惠 成都理工大学沉积地质研究院 
基金项目:国家重点基础发展规划“973”项目(2002CB412607)和中国地质调查局国土 资源大调查项目(1212010530605)
中文摘要:兰坪金顶铅锌矿床的成矿过程与油气的生成有许多相似之处,泥底辟 构造在金顶铅锌矿床的成矿过程中起着极为重要的作用。首先,随着泥底辟的上侵,塑性泥 流夹带大量气体到构造圈闭中释放压力,扩大成矿空间;其次,流体的去气作用在构造圈闭 中进行一系列的强改造活动,进而促使铅锌矿体的形成。文章通过对金顶铅锌矿床形成有关 的泥底辟流体的来源、流体形成原因、流体在张性_挤压走滑盆地阶段的演化及金顶铅锌矿 床成矿的泥底辟流体特征的分析,认为兰坪金顶铅锌矿床的形成与泥底辟构造密切相关,该 矿床具泥底辟流体的成矿特征。
中文关键词:地质学  泥底辟  流体  兰坪金顶铅锌矿床
 
A tentative discussion on mud diapiric fluid metallogenic characteristics of Jinding lead-zinc deposit in Lanping
Abstract:The Jinding lead-zinc deposit in Lanping is genetically quite similar to the oil-gas reservoir,i.e., the mud diapiric structure played an important role in the metallogenic process of the Jinding lead-zinc deposit.First of all,with the upward invasion of mud diapir, a large quantity of gas in the plastic mud flow released pressure when it entered structural traps, thus expanding the space of mineralization.Second, fluids with the degassing effect caused a series of transformation events in the structural traps, thus contributing to the formation of lead-zinc ore bodies. The authors analyzed the source of the mud diapiric fluid, the formation of the fluids, and the mud diapiric fluid metallogenic characteristics of the Jinding lead-zinc deposit. On such a basis, it is believed that the Jinding lead-zinc deposit is closely related to the mud diapiric structure and that this ore deposit has mud dispiric fluid metallogenic characteristics.
keywords:geology, mud diapir, fluid, Jinding lead-zinc deposit in Lanping
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