| 甘肃省稀有金属矿产特征与成矿规律初探 |
| Received:March 31, 2014 Revised:July 03, 2014 点此下载全文 |
| 引用本文：ZHOU HuiWu,LI TongGuo,ZHANG YouKui,YU JunPeng,ZHU WenGe,LIU YangXiong,ZHANG HongBin.2015.A preliminary study of characteristics and metallogenic regularity of rare metal mineral resources in Gansu Province[J].Mineral Deposits,34(5):1030~1045 |
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| Author Name | Affiliation | | ZHOU HuiWu | Geological Survey of Gansu Province, Lanzhou 730000, Gansu, China | | LI TongGuo | Geological Survey of Gansu Province, Lanzhou 730000, Gansu, China | | ZHANG YouKui | Geological Survey of Gansu Province, Lanzhou 730000, Gansu, China | | YU JunPeng | Geological Survey of Gansu Province, Lanzhou 730000, Gansu, China | | ZHU WenGe | Geological Survey of Gansu Province, Lanzhou 730000, Gansu, China | | LIU YangXiong | Geological Survey of Gansu Province, Lanzhou 730000, Gansu, China | | ZHANG HongBin | Geological Survey of Gansu Province, Lanzhou 730000, Gansu, China |
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| 基金项目:本文由中国地质调查局项目“甘肃省稀有金属远景调查(编号:1212011220821)”和甘肃省地质勘查基金项目“甘肃省瓜州县国宝山铷等稀有金属矿普查”、“甘肃省阿克塞县余石山铌钽多金属矿普查”、“甘肃省天水市麦积区六丈山铷等稀有金属矿普查”、“甘肃省玉门市刘家河铷等稀有金属矿普查"和"甘肃省肃北县白头山铷矿普查”联合资助 |
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| 中文摘要:通过20世纪六七十年代和2010年至今2个主要勘查阶段的工作,甘肃省境内共发现了51处稀有金属矿床和矿(化)点,主要成矿类型为碱性花岗岩型和花岗伟晶岩型,其次有变粒岩型、云英岩型和变中酸性火山岩型等。这些矿床和矿(化)点主要分布在北山地区,其次为龙首山、阿尔金山和西秦岭地区,大部分产出于古老地块边缘的火山、岩浆及构造活动带。矿体的产出受岩浆岩侵入体或断裂构造控制,新太古界—古元古界变质地层是主要的赋矿围岩地层,矿体主要产出于华力西中-晚期侵入的花岗岩和伟晶岩中,成矿时代主要为石炭纪—二叠纪,其次为志留纪、三叠纪、奥陶纪、第四纪、侏罗纪。 |
| 中文关键词:地质学 稀有金属 矿产特征 成矿规律 初探 甘肃省 |
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| A preliminary study of characteristics and metallogenic regularity of rare metal mineral resources in Gansu Province |
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| Abstract:During 1960's～1970's and from 2010 up till now, the two main exploration phases of the geological work, geologists discovered 51 rare metal deposits or ore (mineralization) spots in Gansu Province. The main metallogenic types include alkaline granite type and granite pegmatite type, followed by granulite type, greisen type, metamorphic intermediate-acid volcanic rock type, etc. They are mainly distributed in Beishan area, followed by Longshoushan, Aerjinshan and west Qingling areas. Most deposits occur at the edge of the volcanic, magmatic and tectonic belts. The orebodies are controlled by fracture structure and magmatic rock intrusion, with late Archean-Paleoproterozoic metamorphic rock being the main ore rock formation. Orebodies mainly occur in middle and late Variscan intrusive granite and pegmatite, and the ore-forming epochs are mainly Carboniferous and Permian, followed by Silurian, Triassic, Ordovician, Quaternary and Jurassic. |
| keywords:geology rare metal mineral characteristics metallogenic regularity preliminary study Gansu Province |
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