前寒武纪地质体中金矿产的形成时代 |
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引用本文: | 王伏泉. 前寒武纪地质体中金矿产的形成时代[J]. 大地构造与成矿学, 1995, 19(4): 314-321 |
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作者姓名: | 王伏泉 |
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摘 要: | 赋存在前寒武纪地质体中的金矿产,除外生者与地质体沉积期为同时代形成,但一般还有沉积期后内生成矿作用叠加、改造者以外,其他内生金矿产则可能与火山喷发-沉积或岩)或侵入成岩同期,也可能是在成岩期后的前寒武纪构造-岩浆作用下新生、改造和叠加形成,还可以在显生宇地槽阶段、地洼阶段的强烈构造-岩浆作用下新生、改造和叠加形成。本文重点讨论其形成时代的判别及在地洼阶段形成、并赋存在前寒武纪地质体中的金矿产。
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关 键 词: | 金的成矿时代 前寒武纪地质体 地洼期 多因复成金矿床 |
METALLOGENETIC EPOCH OF GOLD HOSTED IN PRECAMBRIAN GEOLOGIC BODY |
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Abstract: | The gold mineral product, with the exception of the exogenetie ore deposit, hosted in Precambrian geologic body has possible following metallogenetic epoches:① Some have been formed simultaneously with the volcanic eruption-sedimentary (diagenetic) process or the magmatic invasion (segregation); ②A number of were regenerated (remade) or diplo- ectono-magmatism after their host rock was formed; ③A number of were regenerated (remade)or diplogenerated by Phanerozoic (geosynclmal and diwa ages) tectono-magmatism. In this article are mainly inquired judgment way to the gold metallogenetic epoch and the gold mineral deposit formed in the diwa age and hosted in Precambrian geologic body. |
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Keywords: | gold metallogenetic epoeb Precambrian geologic body diwa age polygenetic corn pound gold ore deposit |
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