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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

MARCXML

LDR 01872naa#a2200000#a#4500
001 SPRI-202578
005 20240329123525.0
007 ta
008 240329s2003####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# ‡a20240329 ‡bJR