南美洲中安第斯地區(qū)構(gòu)造——巖漿事件與成礦
發(fā)布時(shí)間:2018-06-27 13:23
本文選題:構(gòu)造—巖漿事件 + 成礦作用; 參考:《地質(zhì)論評(píng)》2017年S1期
【摘要】:正中安第斯地區(qū)是Cu、Fe、Au、多金屬礦床的重要產(chǎn)地,位于環(huán)太平洋成礦域東南部,在全球構(gòu)造—巖漿作用與成礦關(guān)系研究中具有重要地位(Sillitoe et al.,2005)。該區(qū)自前寒武紀(jì)至新生代均有構(gòu)造—巖漿活動(dòng),尤以中—新生代最為強(qiáng)烈。前人對(duì)該區(qū)不同地段和時(shí)代的構(gòu)造-巖漿演化及其與大規(guī)模成礦作用的關(guān)系進(jìn)行了研究(如Sillitoe,2003;Sillitoe et al.,2005),目前尚未見(jiàn)到整體的歸
[Abstract]:The central Andes region is an important producer of the Cu-Fe au, polymetallic deposit, located in the southeast of the Pacific Rim metallogenic domain. It plays an important role in the study of the relationship between global tectonic-magmatism and mineralization (Sillitoe et al.2005). From Precambrian to Cenozoic, there are tectonic-magmatic activities in this area, especially in Mesozoic and Cenozoic. Previous studies on tectonic-magmatic evolution in different sections and ages of the area and its relationship with large-scale mineralization (e.g. Sillitoeo ei 2003 Sillitoe et al.2005) have not yet seen a holistic return.
【作者單位】: 中國(guó)地質(zhì)調(diào)查局發(fā)展研究中心;中國(guó)地質(zhì)大學(xué)地質(zhì)過(guò)程與礦產(chǎn)資源國(guó)家重點(diǎn)實(shí)驗(yàn)室;
【基金】:中國(guó)地質(zhì)調(diào)查局項(xiàng)目“海上絲綢之路重點(diǎn)地區(qū)有色金屬資源潛力評(píng)價(jià)”(編號(hào):DD20160118)資助的成果
【分類(lèi)號(hào)】:P618.2
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本文編號(hào):2074054
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