| 内蒙古东乌旗哈巴特盖银多金属矿土壤地球化学异常特征 |
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| 引用本文： | 夏广清.内蒙古东乌旗哈巴特盖银多金属矿土壤地球化学异常特征[J].地质找矿论丛,2006,21(Z1):144-148. |
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| 作者姓名： | 夏广清 |
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| 作者单位： | 中国冶金地质勘查工程总局,第一地质勘查院,河北,三河,065201 |
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| 摘 要： | 哈巴特盖测区1/5万土壤地球化学测量发现了4个异常区,多元素组合异常多分布在黑云母二长花岗岩的内、外接触带上,土壤地球化学异常特征显示本区成矿是多期次的,多元素组合异常在露头矿和盲矿上方均有出现,且异常连续、浓集中心明显,异常的强度和规模大,呈带状、宽带状或面状产出.
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| 关 键 词： | 哈巴特盖银多金属矿 土壤地球化学异常特征 组合异常 异常强度 浓集中心 内蒙古 |
| 文章编号： | 1001-1412(2006)S0-0144-05 |
| 修稿时间： | 2006年7月5日 |
SOIL GEOCHEMICAL ANOMALY CHARACTERISTICS OF HABATEGAI SILVER POLYMETALLIC ORE DEPOSIT,EAST UJIMQIN COUNTY, INNER MONGOLIA |
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| XIA Guang-qing.SOIL GEOCHEMICAL ANOMALY CHARACTERISTICS OF HABATEGAI SILVER POLYMETALLIC ORE DEPOSIT,EAST UJIMQIN COUNTY, INNER MONGOLIA[J].Contributions to Geology and Mineral Resources Research,2006,21(Z1):144-148. |
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| Authors: | XIA Guang-qing |
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| Abstract: | Four anomaly areas are delineated by soil geochemical survey at 1:50,000 scale in Habategai area.Composite poly-element anomalies are distributed along inner-contact zone and outer-contact zone of biotite-monzonitic granite.Judged from the characteristics of soil geochemical anomaly the ore forming processes is characteristic of poly-epochs and poly-stages.Poly-element composite anomalies are found(above) surface ores and blind ores.Anomalies are big and continuous in belt,zone or area with clear concentration centers. |
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| Keywords: | Habategai soil geochemical anomaly characteristics composite anomaly anomaly intensity concentration center east Ujimqin Inner Mongolia |
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