钨锑金型金矿床构造成矿浅析 |
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引用本文: | 彭渤,邓志强.钨锑金型金矿床构造成矿浅析[J].大地构造与成矿学,1995,19(2):161-170. |
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作者姓名: | 彭渤 邓志强 |
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摘 要: | 综合研究表明,W-Sb-Au型金矿床的赋矿层位形成于地壳强烈活动期(地槽期、地洼期)。富含钙泥质,凝灰质的砂板岩系是该类金矿床的有利控矿围岩。层间断层在其成矿过程中有特别重要的作用,断层作用过程中发生的构造地球化学反应导致金的聚集成矿,伴随地壳演化而发生的构造成矿演化促使金等矿化元素富集成矿。
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关 键 词: | 断层构造,构造成矿,W-Sb-Au型金矿床 |
PRELIMINARY ANALYSIS ON TECTONIC METALLOGENESIS OF W-SB-Au TYPE GOLD DEPOSITS |
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Abstract: | The synthetic study shows that the host-rock layers of the W-Sb-Au type gold deposits were formed during the strongly active stages of the crust evolution; the stages of geosyncline and geodepression. The sa dy-slate rock series containing many calcareous-petitic and tuffaceous substances is the best favorable ore-controlling rocks for the W-Sb-Au type gold tectonogeochemical reactions caused by faulting led gold accumulate and form gold deposits.The tectono-metallogenic evolution followed with the crust evolution made the ore-forming elements, such as gold,enriched to form the gold deposits. |
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Keywords: | fault tectonometallogenesis W-Sb-Au type gold deposits |
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