Udokan-Chiney ore-magmatic system, Russia

摘要：

1 IntroductionIn the South framework of the Siberian platform there is an extra large metallogenic province. Many giant deposits of different genetic types are concentrated here: Udokan (Cu), Chiney (Ti-Fe-V, Pd-Cu), Katugin (Ta, Nb), Sulumat (Fe) etc. (Fig. 1). Copper deposits are in the centre of our interest for the reason that 40 Mt of Cu were found in Kodaro-Udokan region. They are concentrated in different rocks. All deposits are subdivided into three genetic types which were formed since Proterozoic epoch till Late Mesozoic. The most part of them belongs to copper sandstone formation (Udokan deposit and its satellites - Krasnoye, Burpala, Sakinskoe, PR1), and residual part is concentrated in gabbro in Cu-Ni sulphide ores (Chiney massif and in some related intrusions, PR1).

作者: B.I.Gongalskiy N.A.Krivolutskaya

作者单位: Institute of the Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry RAS, Moscow Vernadsky Institute of Geochemistry RAS, Moscow

会议类型: 国际会议

会议名称: Xian International Ni-Cu(Pt) Deposit Symposium 2009(2009 西安·Ni-Cu(Pt)岩浆矿床国际学术研讨会)

会议地点: 西安

会议语种:英文

页码: 180-184

在线出版日期: 2009-09-01（万方平台首次上网日期，不代表论文的发表时间）