陈小华.江苏主要含矿花岗岩体的地球化学特征及找矿方向[J].地质与勘探,2004,(5):61-66 |
江苏主要含矿花岗岩体的地球化学特征及找矿方向 |
GEOCHEMICAL FEATURES AND PROSPECTING FOR MAIN ORE-BEARING GRANITOIDS IN JIANGSU PROVINCE |
修订日期:2003-08-21 |
DOI: |
中文关键词: 含矿花岗岩体 地球化学 包裹体 江苏省 |
英文关键词: ore-bearing granite masses, geochemistry, inclusions, Jiangsu Province, |
基金项目: |
陈小华 |
南京森林公安高等专科学校,南京210046 |
摘要点击次数: 1955 |
全文下载次数: 1393 |
中文摘要: |
分析了江苏省主要含矿花岗岩体的主元素、微量元素含量,所含黑云母的成分以及包裹体的类型等地球化学特征.结果表明它们大多属于岩浆花岗岩,且以I型花岗岩为主.成矿元素Cu、Pb、Zn在I型含矿花岗岩中普遍有一定程度的富集,其中以Cu的富集程度最好;Cr、Co、Ni在此类岩体中含量亦较高.广泛发育多种包裹体,尤其是发育含子矿物多相包裹体是含矿花岗岩体的重要特征.指出应加强在宁镇中段某些I型花岗岩体中寻找Cu多金属矿的工作. |
英文摘要: |
Major and trace elements, biotite composition, and inclusion types of main ore-bearing granitoids in Jiangsu province has been investigated. The results show that the most granitoids are belong to magmatic granites, and dominated by I type granite. Ore-forming elements such as Cu, Pb, and Zn are generally enriched to a certain extent in I type granites, in which Cu is the most. Content of Cr, Co and Ni is comparatively higher in I type granites. Well-developed inclusions, especially the multi-phase inclusions with daughter minerals, are a key feature for ore-bearing granitoids. It is pointed out that Cu polymetallic prospecting should be strengthened in some I type granitoids in the middle parts of Nanjing-Zhengjiang area. |
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