| 杨晓坤,姜华,王光旺,张裴培,张庆松.西藏冈底斯带东段岗讲铜钼矿床含矿斑岩地球化学特征[J].地质找矿论丛,2013,28(2):197-202 |
| 西藏冈底斯带东段岗讲铜钼矿床含矿斑岩地球化学特征 |
| Geochemical characteristics of the host porphyry of Gangjiang Cu-Mo deposit in east Gangdese belt of Tibet |
| 投稿时间：2012-05-08 修订日期：2013-09-05 |
| DOI：10.6053/j.issn.1001-1412.2013.02.005 |
| 中文关键词: 冈底斯 斑岩 铜钼矿床 地球化学 西藏 |
| 英文关键词:Gangdese porphyry Cu-Mo deposit geochemistry Tibet |
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| 摘要点击次数: 2058 |
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| 中文摘要: |
| 西藏冈底斯带东段的岗讲铜钼矿床产于复式岩体中,岩体主要由二长斑岩、英安斑岩和流纹斑岩类岩石组成,其岩性属于钙碱性系列岩石。岩石地球化学特征表明该复式岩体可能形成于碰撞后抬升期,矿化与低温低压的岩浆结晶分异环境有关。 |
| 英文摘要: |
| Gangjiang Cu-Mo deposit occurs in a complex rock body consisting mainly of monzonitic porphyry, dacitic porphyry and rhyolitic porphyry. The porphyries belong to the calc-alkaline rock series. Their geochemical characteristics indicate that the complex rock body may be formed in the post-collision uplift period and the mineralization is related to crystal differentiation under low-temperature low-pressure condition of magma. |
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