| 薛燕萍,袁小平.承德大庙铁矿深部找矿探析[J].矿产勘查,2012,3(4):476-482 |
| 承德大庙铁矿深部找矿探析 |
| Analysis on the deep prospecting in Damiao magnetite mining area |
| 投稿时间：2012-03-16 |
| DOI： |
| 中文关键词: 承德 大庙式钒钛磁铁矿 地质特征 深部找矿 |
| 英文关键词: Chengde Damiao vanadium-titanium magnetite geological characteristics deep prospecting |
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| 摘要点击次数: 1984 |
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| 中文摘要: |
| 文章阐述了承德大庙钒钛磁铁矿成矿地质特征,并通过对成矿地质条件分析,认为成矿是岩浆及构造活动综合作用的结果,深部岩浆(晚期)分凝、贯入是成矿的内在因素,推测大庙铁矿有巨大延深,深部可能存在隐伏铁矿体。 |
| 英文摘要: |
| It is described the metallogenic geological characteristics of Damiao vanadium-titanium magnetite in this paper. By analyzing the metallogenic geological condition of the deposit, it is considered that the mineralization results from the comprehensive effects of magmatic and tectonic activities, and the deep-seated magmatic segregation and injection are the internal factors of mineralization. Therefore, the author speculated that Damiao magnetite mining area has great extension and hidden iron ore bodies may exist in its deep regions. |
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