| 甘肃省肃北县鸡叫沟金矿床地球化学特征及成因探讨 |
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| 引用本文： | 范俊杰, 张学军, 常春郊, 张惠玉, 丛润祥, 任胜. 甘肃省肃北县鸡叫沟金矿床地球化学特征及成因探讨[J]. 地质与资源, 2006, 15(4): 272-276,294. doi: 10.13686/j.cnki.dzyzy.2006.04.006 |
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| 作者姓名： | 范俊杰 张学军 常春郊 张惠玉 丛润祥 任胜 |
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| 作者单位： | 武警黄金地质研宄所, 河北 廊坊 065000 |
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| 基金项目： | 国土资源部国土资源大调查项目 |
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| 摘 要： | 鸡叫沟金矿床矿石及含矿岩系的稳定同位素、流体包裹体及稀土元素等地球化学研究表明，金矿床形成于碰撞造山运动后期的裂谷环境，成矿物质主要来自中基性、超基性火山岩，为低温、低盐、浅成的金矿床.硫来自岩浆硫.矿物质水主要来自大气降水，后期又萃取了岩浆水.矿床类型为与岩浆作用有关的浅成低温热液型.
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| 关 键 词： | 矿床地球化学 矿床成因 金矿床 肃北县 |
| 文章编号： | 1671-1947（2006）04-0272-06 |
| 收稿时间： | 2006-04-07 |
| 修稿时间： | 2006-09-28 |
GEOCHEMISTRY AND GENESIS OF THE JIJIAOGOU GOLD DEPOSIT IN SUBEI, GANSU PROVINCE, CHINA |
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| FAN Jun-jie, ZHANG Xue-jun, CHANG Chun-jiao, ZHANG Hui-yu, CONG Run-xi ang, REN Sheng. GEOCHEMISTRY AND GENESIS OF THE JIJIAOGOU GOLD DEPOSIT IN SUBEI, GANSU PROVINCE, CHINA[J]. Geology and Resources, 2006, 15(4): 272-276,294. doi: 10.13686/j.cnki.dzyzy.2006.04.006 |
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| Authors: | FAN Jun-jie ZHANG Xue-jun CHANG Chun-jiao ZHANG Hui-yu CONG Run-xiang REN Sheng |
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| Affiliation: | Institute of Gold Geology, CAPE, Langfang 065000, Hebei Province, China |
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| Abstract: | Study on the stable isotope, fluid inclusions and REEs for the ore s and ore-bearing rock series in the Jijiaogou gold deposit in Subei County, Gans u Province indicates that the deposit was formed in rift environment during post collision orogeny. The ore-forming matters were derived from mainly intermedia te-basic to ultrabasic volcanic rocks. It is an epithermal deposit with low-te mperature and low-salinity. The sulfur is magma-derived. The mineral fluid is dominantly from atmospheric water and later extraction of magmatic water. The de posit genetically belongs to epithermal type related to magmatism. |
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| Keywords: | geochemistry of deposit genesis gold deposit Subei County |
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