摘要
古油藏、沥青及沥青包裹体和某些金属矿床都是自然界成矿作用的产物，它们在时空关系上极为密切，成因上有内在联系，可作为研究Hg、Sb、As、An、U、Cu、Pb、Zn等改造矿床的物质来源、迁移形成、成矿物理化学条件、划分改造阶段及找矿标志等，并对探讨有机与金属成矿理论具有重要意义。
Ancient oil resevoirs, bitumens and bitumen inclusions as well as some metallic ore deposits are all products of metallogenesis in nature. They have colse spatial-temporal and genetic connec-tions. They can be used to study the material sources of reworked deposits of chemically mobile el-ements such as Hg, Sb, As, Au, U,Cu, Pb, Zn, etc., the way of their migration, the physicochemical conditions of ore deposition, how to divide the reworking stages, and how to serve as indicators for ore prospecting. They are also of great theoretical significance in discussing the relationship be-tween organic matter and metallogenesis.
出处
《矿物学报》
CAS
CSCD
北大核心
1995年第2期117-122,共6页
Acta Mineralogica Sinica
关键词
古油藏
沥青
矿物包体
金属矿床
成矿
ancient oil reservoir
bitumen
inclusion
ore deposit
organometallogencesis
