Diagenetic Features at White Pine (Michigan), Redstone (N. W. Territories, Canada) and Kamoto (Zaire). Sequence of Mineralization in Sediment-Hosted Copper Deposits (Part 1)-Reference-Cited by-同舟云学术

Diagenetic Features at White Pine (Michigan), Redstone (N. W. Territories, Canada) and Kamoto (Zaire). Sequence of Mineralization in Sediment-Hosted Copper Deposits (Part 1)

Published:1986 Issue: Volume: Page:390-397
ISSN:0723-8835
Container-title:Special Publication No. 4 of the Society for Geology Applied to Mineral Deposits
language:
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Author:

Brown A. C.,Chartrand F. M.

Publisher

Springer Berlin Heidelberg

Link

http://link.springer.com/content/pdf/10.1007/978-3-642-70902-9_28

Reference20 articles.

1. Bartholomé P (1962) Les minerais cupro-cobaltifères de Kamoto (Katanga Ouest). I Pétrographie. Stud Univ Louvanium, Fac Sci Kinshasa 14, p 40

2. Bartholomé P, Evrard P, Katekesha F, Lopez-Ruiz JM, Ngongo M (1972) Diagenetic ore-forming processes at Kamoto, Katanga, Republic of the Congo. In: Amstutz GC, Bernard AJ (eds) Ores in sediments. Springer, Berlin Heidelberg New York, pp 21–41

3. Brown AC (1978) Stratiform copper deposits — evidence for their post-sedimentary origin. Miner Sci Eng 10: 145–163

4. Brown AC (1980a) The diagenetic origin of stratiform copper deposits. In: Ridge JD (ed) Proc 5th Q IAGOD Symp, pp 81–89

5. Brown AC (1980b) Stratiform copper deposits and pene-exhalative environments. Geol Soc Am, Abstracts with Programs 13: 418

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