Geology and diamond distribution of the 140/141 kimberlite, Fort à la Corne, central Saskatchewan, Canada-Reference-Cited by-同舟云学术

Geology and diamond distribution of the 140/141 kimberlite, Fort à la Corne, central Saskatchewan, Canada

Published:2004-09 Issue:1-4 Volume:76 Page:99-114
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Berryman Adrian K.,Scott Smith Barbara H.,Jellicoe Brent C.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference19 articles.

1. Kisseynew metasedimentary gneiss belt, Trans-Hudson Orogen (Canada): back-arc origin and collisional inversion;Ansdell;Geology,1995

2. The Case for a Flin-Flon-Glennie Protocontinent;Ashton,1997

3. Characterisation, origin and paleaproterozoic history of the Saskatchewan Craton and possible implications for Trans-Hudson Orogen;Chiarenzelli,1996

4. Red Deer Hill: a drumlinized, glaciotectonic feature near Prince Albert, Saskatchewan, Canada;Christiansen;Canadian Journal of Earth Sciences,1993

5. Clement, C.R., 1982. A comparative geological study of some major kimberlite pipes in the northern Cape and Orange Free State. Unpublished PhD thesis, University of Cape Town, South Africa, 431 pp.

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