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Record #202578:
Supercontinents, superplumes and continental growth: the Neoproterozoic record / Kent C. Condie.
Title: | Supercontinents, superplumes and continental growth: the Neoproterozoic record / Kent C. Condie. |
Author(s): | Condie, Kent C. |
Date: | 2003. |
Publisher: | London: Geological Society of London |
In: | Proterozoic East Gondwana : supercontinent assembly and break-up. (2003.), |
Abstract: | Describes aggregation and break up of Neoproterozoic supercontinent Rodinia, and formation of new supercontinent Pannotia-Gondwana. Hypothesises that low rates of continental growth in Neoproterozoic are due to absence of superplume events associated with formation of Rodinia or Gondwana. |
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. 551.8 -- Palaeogeography. 550.3 -- Geophysics. 550.4 -- Geochemistry. 550.93 -- Geochronology. 550.384 -- Palaeomagnetism. 54.027 -- Isotope analysis. B -- Geology and soil sciences. (217.5) -- Gondwana. (*7) -- Antarctic regions. (*82) -- South Atlantic Ocean. (94) -- Australia. (6) -- Africa. (5) -- Asia. |
SPRI record no.: | 202578 |
LDR 01872naa#a2200000#a#4500 001 SPRI-202578 005 20231204194035.0 007 ta 008 231204s2003####enkab##|#####|0||#0#eng#d 035 ## ‡aSPRI-202578 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aCondie, Kent C. 245 10 ‡aSupercontinents, superplumes and continental growth :‡bthe Neoproterozoic record /‡cKent C. Condie. 260 ## ‡aLondon :‡bGeological Society of London,‡c2003. 300 ## ‡ap. 1-21 :‡bill., diags., tables, map. 500 ## ‡aIn: Proterozoic East Gondwana : supercontinent assembly and break-up / M. Yoshida, B.F. Windley, S. Dasgupta, eds. 520 3# ‡aDescribes aggregation and break up of Neoproterozoic supercontinent Rodinia, and formation of new supercontinent Pannotia-Gondwana. Hypothesises that low rates of continental growth in Neoproterozoic are due to absence of superplume events associated with formation of Rodinia or Gondwana. 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 ‡a551.8 -- 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 ‡a54.027 -- Isotope analysis.‡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 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# ‡a20231204 ‡bJR