(Q69672274)

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A reconnaissance teleseismic study of the upper mantle and transition zone beneath the Archean Slave craton in NW Canada

scientific article published in April 2000

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A reconnaissance teleseismic study of the upper mantle and transition zone beneath the Archean Slave craton in NW Canada (English)

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1 reference

C.-G Bank

1

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M.G Bostock

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2

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R.M Ellis

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3

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J.F Cassidy

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4

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publication date

April 2000

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published in

Tectonophysics

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volume

319

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issue

3

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page(s)

151-166

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cites work

Implications of new chronostratigraphy for tectonic evolution of Wopmay Orogen, Northwest Canadian Shield

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Evidence from magnetic fabric for the flow pattern of magma in the Mackenzie giant radiating dyke swarm

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Imaging the lithospheric mantle in northwestern Canada with seismic wide-angle reflections

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Shear wave splitting, continental keels, and patterns of mantle flow

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Origin of kimberlite pipes by diapiric upwelling in the upper mantle

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Refractory trace elements in diamond inclusions: Further clues to the origins of the ancient cratons

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Evolution of the Slave craton

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Composition and development of the continental tectosphere

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Structure and Formation of the Continental Tectosphere

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Traveltimes for global earthquake location and phase identification

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Accretion of the Archean Slave province

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Collapse of Archean orogens and the generation of late- to postkinematic granitoids

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Present-day plate motions

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The Slave Province: a distinct Archean craton

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The Interpretation of Shear-Wave Splitting Parameters In the Presence of Two Anisotropic Layers

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The deep structure of the Australian continent from surface wave tomography

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Seismic evidence for a fossil mantle plume beneath South America and implications for plate driving forces

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Global patterns of azimuthal anisotropy and deformations in the continental mantle

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Formation of an Archaean continent

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Superkimberlites: A geodynamic diamond window to the Earth's core

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Identifiers

DOI

10.1016/S0040-1951(00)00034-2

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ADS bibcode

2000Tectp.319..151B

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(Q69672274)

A reconnaissance teleseismic study of the upper mantle and transition zone beneath the Archean Slave craton in NW Canada

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