张玉成.柳西地区金矿成矿规律及找矿方向[J].地质找矿论丛,2002,(3):175-179
柳西地区金矿成矿规律及找矿方向
METALLOGENIC REGULARITIES AND PROSPECTING OF GOLD DEPOSITS IN THE LIUXI AREA
投稿时间:2001-11-27  修订日期:2002-04-30
DOI:10.6053/j.issn.1001-1412.2002.3. 006
中文关键词:  金矿类型  成矿规律  构造环境  找矿方向  柳西地区  甘肃省
英文关键词:Gold deposit types  Metallogenic regularities  Tectonic settings  Prospecting orientation  Liuxi area  Gansu province
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作者单位
张玉成 甘肃有色地质勘查局四队, 甘肃张掖, 734012 
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中文摘要:
      柳西地区自古生代以来形成的柳园—俞井子裂谷带等构造奠定了金矿床产出的地质背景,金矿成矿作用受一定的地层、构造、岩浆岩控制,不同级别和规模的构造分别控制着金矿成矿带、矿床(体)的产出,同时控制着金矿的矿床类型及成矿元素组合。找矿方向为柳园—俞井子裂谷带南北缘深大断裂带及其内部次级大断裂两侧
英文摘要:
      Gold deposits in Liuxi area were formed under the background of Liuyan-Yujingzi rift zone which took shape since Paleozoic Era. Ore formation is controled by certain stratigraphic units, tectonics and magmatism. Tectonics or stractures in varied scales control ore belt, ore deposits(bodies) and ore deposit type and ore element assemblages respectively. The further exploration should be oriented to deep and large fractural zones in the south and north margins of the rift and the subscale fractures in itself.
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