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-List Of Titles -Lithospheric domains and controls on kimberlite emplacement, Slave Province, Canada : evidence from elastic thickness and upper mantle composition

Please use this identifier to cite or link to this item: http://hdl.handle.net/1959.14/31575

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Title
Lithospheric domains and controls on kimberlite emplacement, Slave Province, Canada : evidence from elastic thickness and upper mantle composition
Related
Geochemistry, geophysics, geosystems (G³), Vol. 6, Issue 10, p.1-16
DOI
10.1029/2005GC000978
Publisher
American Geophysical Union
Date
2005
Author/Creator
Poudjom Djomani, Yvette H
Author/Creator
Griffin, William L
Author/Creator
O'Reilly, Suzanne Y
Author/Creator
Doyle, Buddy J
Description
We have mapped the deep structure of the Slave craton by combining analysis the effective elastic thickness (Te) with data on mantle samples from numerous kimberlites. Three-dimensional mapping of the subcontinental lithospheric mantle (SCLM), using mantle-derived xenoliths and xenocrysts in kimberlites, has shown that much of the craton is underlain by a strongly layered SCLM; a highly depleted upper layer (low in basaltic components Ca, Al, Fe) is separated from a relatively fertile lower layer by a sharp boundary. This boundary lies at 140–150 km depth in the Lac de Gras area and shallows to ≤100 km in the northern and southern parts of the Craton. Weak lithosphere (Te < 25 km) on the northern edge of the craton may reflect the intrusion of the Mackenzie Plume (circa 1270 Ma). The strongest lithosphere (Te > 56 km), in the younger eastern part of the craton, is separated from the older western part by a zone of steep Te gradient parallel to the major locus of kimberlite intrusion, which may map the deep extension of the boundary between the two domains. Another strong Te gradient across the Kilohigok Basin accompanies a marked compositional change in the upper layer of the lithospheric mantle; the Basin probably marks a major translithospheric fault. Correlations between Te and mantle composition suggest that Te is strongly influenced by the rheology of the upper mantle.
Description
16 page(s)
Subject Keyword
Slave craton mantle
Subject Keyword
elastic thickness
Subject Keyword
deep lithosphere structure
Subject Keyword
Canada kimberlite emplacement
Subject Keyword
lithospheric mantle composition
Resource Type
journal article
Organisation
Macquarie University. National Key Centre for Geochemical Evolution and Metallogeny of Continents (GEMOC)

Identifier
http://hdl.handle.net/1959.14/31575
Identifier
ISSN:1525-2027
Identifier
mq-rm-2005002243
Language
eng
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Subject
"Geochemistry, geophysics, geosystems (G³)"
 
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