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Record #202593:
- #202593
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MARC recordPalaeomagnetic 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 |
LDR 01901naa#a2200000#a#4500 001 SPRI-202593 005 20230331004020.0 007 ta 008 230331s2003####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# ‡a20230331 ‡bJR