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Are all mantle plumes equal in Nickel and PGE potential?

Kuo-Lung WangSuzanne Y. O’ReillyJon HronskyWilliam L. Griffin

GEMOC ARC National Key Centre,Department of Earth and Planetary Sciences,Macquarie University,NSW 2109,AustraliaGEMOC ARC National Key Centre,Department of Earth and Planetary Sciences,Macquarie University,NSW 2109,Australia BHP Billiton,Level 34 Central Park,152-158 St Georges Tce,Perth,WA 6000,AustraliaGEMOC ARC National Key Centre,Department of Earth and Planetary Sciences,Macquarie University,NSW 2109,Australia CSIRO Exploration and Mining,North Ryde,NSW 2113,Australia

摘要:<正>Continental flood basalts (CFBs), derived from mantle plumes (rising from the convecting mantle and possibly as deep as the core-mantle boundary), are one of the major hosts for world-class Ni-Cu-PGE ore deposits. Each plume may have a complex history and heterogeneous composition. Therefore, some plumes may be predisposed to be favourable for large-scale Ni-PGE mineralisation.
会议名称:

International Conference on Continental Volcanism

会议时间:

2006-05

会议地点:

中国广东广州

  • 专辑:

    基础科学; 工程科技Ⅰ辑

  • 专题:

    地质学; 矿业工程

  • 分类号:

    P618.71;P618.4

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