| 会泽黄草岭磷矿地质特征及成矿浅析 |
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| 引用本文： | 丁小平,牛泽林,杨义明.会泽黄草岭磷矿地质特征及成矿浅析[J].云南地质,2014(2):201-206. |
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| 作者姓名： | 丁小平 牛泽林 杨义明 |
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| 作者单位： | 云南伟力达地球物理勘测有限公司,云南昆明650217 |
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| 摘 要： | 会泽县黄草岭磷矿含矿层位为下寒武统渔户村组中谊村段（∈1yz）,胶磷矿由砂屑、砾屑、鲕粒组成,孔隙一基底胶结,多伴铁泥质胶结,颗粒形态次圆、不规则状,细、粗颗粒含量不均;沉积环境处于古陆边缘浅海地域,矿物质来源主要取决于古陆风化淋滤作用.
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| 关 键 词： | 浅海沉积磷矿 风化淋滤 水动力震筛 同层同期 云南会泽黄草岭 |
THE GEOLOGICAL FEATURE AND PRELIMINARY ANALYSIS OF METALLOGENESIS OF HUANGCAOLING P DEPOSIT IN HUIZE |
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| DING Xiao-ping,NIU Ze-lin,YANG Yi-ming.THE GEOLOGICAL FEATURE AND PRELIMINARY ANALYSIS OF METALLOGENESIS OF HUANGCAOLING P DEPOSIT IN HUIZE[J].Yunnan Geology,2014(2):201-206. |
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| Authors: | DING Xiao-ping NIU Ze-lin YANG Yi-ming |
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| Institution: | ( Yunnan Weilida Geophysical Exploration Company (Ltd) , Kunming 650217) |
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| Abstract: | The ore-beating bed of Huangcaoling Zhongyicun Member （ ∈1yz）. The colophane is sandy The sedimentary environment is an epicontinental sea from the weathering-leaching of old land. P deposit in Huize is Lower Cambrian Yuhucun Formation clast, gravel clast, ooidal, fine and coarse grain unequal. beside the old land margin. The mineral originates mainly |
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| Keywords: | Sedimentary P Deposit of Epicontinental Sea Weathering-Leaching Water Dynamic Vibration Sieve Equivalent Beds Synehrony Huangeaoling Huize Yunnan |
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