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Magmatic Ore Deposits in Layered Intrusions?Descriptive Model for Reef-Type PGE and Contact-Type Cu-Ni-PGE Deposits - Softcover
Synopsis
Layered, ultramafic to mafic intrusions are uncommon in the geologic record, but host magmatic ore deposits containing most of the world’s economic concentrations of platinum-group elements (PGE) (figs. 1 and 2). These deposits are mined primarily for their platinum, palladium, and rhodium contents (table 1). Magmatic ore deposits are derived from accumulations of crystals of metallic oxides, or immiscible sulfide, or oxide liquids that formed during the cooling and crystallization of magma, typically with mafic to ultramafic compositions.
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- PublisherCreateSpace Independent Publishing Platform
- Publication date2014
- ISBN 10 1495906531
- ISBN 13 9781495906534
- BindingPaperback
- LanguageEnglish
- Number of pages54
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Magmatic Ore Deposits in Layered Intrusions?Descriptive Model for Reef-Type PGE and Contact-Type Cu-Ni-PGE Deposits
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Createspace Independent Publishing Platform, 2014
ISBN 10: 1495906531
ISBN 13: 9781495906534
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Paperback / softback
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Paperback / softback. Condition: New. This item is printed on demand. New copy - Usually dispatched within 5-9 working days 225. Seller Inventory # C9781495906534
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Magmatic Ore Deposits in Layered Intrusions?Descriptive Model for Reef-Type PGE and Contact-Type Cu-Ni-PGE Deposits (Paperback)
Published by
Createspace Independent Publishing Platform, 2014
ISBN 10: 1495906531
ISBN 13: 9781495906534
New
Paperback
Seller: CitiRetail, Stevenage, United Kingdom
Seller rating 5 out of 5 stars
Paperback. Condition: new. Paperback. Layered, ultramafic to mafic intrusions are uncommon in the geologic record, but host magmatic ore deposits containing most of the world's economic concentrations of platinum-group elements (PGE) (figs. 1 and 2). These deposits are mined primarily for their platinum, palladium, and rhodium contents (table 1). Magmatic ore deposits are derived from accumulations of crystals of metallic oxides, or immiscible sulfide, or oxide liquids that formed during the cooling and crystallization of magma, typically with mafic to ultramafic compositions. Shipping may be from our UK warehouse or from our Australian or US warehouses, depending on stock availability. Seller Inventory # 9781495906534
Quantity: 1 available