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Record #202593:

Palaeomagnetic constraints on the Proterozoic tectonic evolution of Australia / Michael T.D. Wingate, David D. Evans.

Title: Palaeomagnetic constraints on the Proterozoic tectonic evolution of Australia / Michael T.D. Wingate, David D. Evans.
Author(s): Wingate, Michael T. D.
Evans, David D.
Date: 2003.
Publisher: London: Geological Society of London
In: Proterozoic East Gondwana : supercontinent assembly and break-up. (2003.),
Abstract: Assembles reliable palaeomagnetic data that overlap palaeopoles from 1.7 to 1.8 Ga and 1.5 to 1.6 Ga, concluding that North and West Australia cratons have occupied their present relative positions since at least c. 1.7 Ga, and have been joined to South Australia craton since c. 1.5 Ga.
Notes:

In: Proterozoic East Gondwana : supercontinent assembly and break-up / M. Yoshida, B.F. Windley, S. Dasgupta, eds.

Keywords: 551.1/.4 -- Geology.
551.24 -- Geotectonics.
551.241 -- Plate tectonics.
551.251 -- Metamorphism.
551.461.8 -- Palaeo-oceanography.
551.7 -- Stratigraphy.
551.72 -- Proterozoic.
551.732 -- Cambrian.
551.8 -- Palaeogeography.
550.3 -- Geophysics.
550.4 -- Geochemistry.
550.93 -- Geochronology.
550.384 -- Palaeomagnetism.
B -- Geology and soil sciences.
(217.5) -- Gondwana.
(*7) -- Antarctic regions.
(*82) -- South Atlantic Ocean.
(94) -- Australia.
(6) -- Africa.
(5) -- Asia.
SPRI record no.: 202593

MARCXML

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001 SPRI-202593
005 20240329000752.0
007 ta
008 240329s2003####enka###|#####|0||#0#eng#d
035 ## ‡aSPRI-202593
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aWingate, Michael T. D.
245 10 ‡aPalaeomagnetic constraints on the Proterozoic tectonic evolution of Australia /‡cMichael T.D. Wingate, David D. Evans.
260 ## ‡aLondon :‡bGeological Society of London,‡c2003.
300 ## ‡ap. 77-91 :‡bill., diags.
500 ## ‡aIn: Proterozoic East Gondwana : supercontinent assembly and break-up / M. Yoshida, B.F. Windley, S. Dasgupta, eds.
520 3# ‡aAssembles reliable palaeomagnetic data that overlap palaeopoles from 1.7 to 1.8 Ga and 1.5 to 1.6 Ga, concluding that North and West Australia cratons have occupied their present relative positions since at least c. 1.7 Ga, and have been joined to South Australia craton since c. 1.5 Ga.
650 07 ‡a551.1/.4 -- Geology.‡2udc
650 07 ‡a551.24 -- Geotectonics.‡2udc
650 07 ‡a551.241 -- Plate tectonics.‡2udc
650 07 ‡a551.251 -- Metamorphism.‡2udc
650 07 ‡a551.461.8 -- Palaeo-oceanography.‡2udc
650 07 ‡a551.7 -- Stratigraphy.‡2udc
650 07 ‡a551.72 -- Proterozoic.‡2udc
650 07 ‡a551.732 -- Cambrian.‡2udc
650 07 ‡a551.8 -- Palaeogeography.‡2udc
650 07 ‡a550.3 -- Geophysics.‡2udc
650 07 ‡a550.4 -- Geochemistry.‡2udc
650 07 ‡a550.93 -- Geochronology.‡2udc
650 07 ‡a550.384 -- Palaeomagnetism.‡2udc
650 07 ‡aB -- Geology and soil sciences.‡2local
651 #7 ‡a(217.5) -- Gondwana.‡2udc
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*82) -- South Atlantic Ocean.‡2udc
651 #7 ‡a(94) -- Australia.‡2udc
651 #7 ‡a(6) -- Africa.‡2udc
651 #7 ‡a(5) -- Asia.‡2udc
700 1# ‡aEvans, David D.
773 0# ‡7nnam ‡aM. Yoshida, B.F. Windley, S. Dasgupta, eds. ‡tProterozoic East Gondwana : supercontinent assembly and break-up. ‡dLondon : Geological Society of London, 2003. ‡wSPRI-202327
916 ## ‡aJR
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240329 ‡bJR