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Lefort, J.P., Aïfa, T. (2001) Paleomagnetic and Geochronological Evidence for a Large Rotation of the West African Craton Between 1.9 and 1.4 Ga: A Kinematic Model for the Fragmentation of Columbia and the Accretion of Rodinia. Gondwana Research, 4 (4) 678-679 doi:10.1016/s1342-937x(05)70474-3

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Reference TypeJournal (article/letter/editorial)
TitlePaleomagnetic and Geochronological Evidence for a Large Rotation of the West African Craton Between 1.9 and 1.4 Ga: A Kinematic Model for the Fragmentation of Columbia and the Accretion of Rodinia
JournalGondwana Research
AuthorsLefort, J.P.Author
Aïfa, T.Author
Year2001 (October)Volume4
Issue4
PublisherElsevier BV
URL
DOIdoi:10.1016/s1342-937x(05)70474-3Search in ResearchGate
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Mindat Ref. ID710508Long-form Identifiermindat:1:5:710508:5
GUID0
Full ReferenceLefort, J.P., Aïfa, T. (2001) Paleomagnetic and Geochronological Evidence for a Large Rotation of the West African Craton Between 1.9 and 1.4 Ga: A Kinematic Model for the Fragmentation of Columbia and the Accretion of Rodinia. Gondwana Research, 4 (4) 678-679 doi:10.1016/s1342-937x(05)70474-3
Plain TextLefort, J.P., Aïfa, T. (2001) Paleomagnetic and Geochronological Evidence for a Large Rotation of the West African Craton Between 1.9 and 1.4 Ga: A Kinematic Model for the Fragmentation of Columbia and the Accretion of Rodinia. Gondwana Research, 4 (4) 678-679 doi:10.1016/s1342-937x(05)70474-3
In(2001, October) Gondwana Research Vol. 4 (4) Elsevier BV

See Also

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Aïfa, T., Lefort, J.P., Drareni, A. (2001) New Paleopoles at 1.4 – 1.9 Ga from Dyke Swarms of the West African Craton: Paleomagnetic Contribution to the Accretionary Phase of Rodinia. Gondwana Research, 4 (4) 559-560 doi:10.1016/s1342-937x(05)70362-2
Meert, Joseph G. (2001) Growing Gondwana and Rethinking Rodinia: A Paleomagnetic Perspective. Gondwana Research, 4 (3) 279-288 doi:10.1016/s1342-937x(05)70329-4
Grantham, G.H. (2001) Cryptic Pan-African Transpression Along the Eastern Margin of the Kalahari Craton and Beyond — A Possible Suture Between East and West Gondwana. Gondwana Research, 4 (4) 623-624 doi:10.1016/s1342-937x(05)70427-5
KRONER, A (2001) The East African Orogen: New Zircon and Nd Ages and Implications for Rodinia and Gondwana Supercontinent Formation and Dispersal. Gondwana Research, 4 (2) 179-181 doi:10.1016/s1342-937x(05)70685-7
Glebovitsky, Viktor A. (2001) Precambrian Collision Orogen Formation and Supercontinents: Tectonic, Petrologic and Isotope Geochronological Evidence. Gondwana Research, 4 (4) 621 doi:10.1016/s1342-937x(05)70424-x
Meert, Joseph G. (2002) Paleomagnetic Evidence for a Paleo-Mesoproterozoic Supercontinent Columbia. Gondwana Research, 5 (1) 207-215 doi:10.1016/s1342-937x(05)70904-7
Pisarevsky, S.A., Natapov, L.M. (2001) Siberia and Rodinia. Gondwana Research, 4 (4) 734-735 doi:10.1016/s1342-937x(05)70526-8
Condie, Kent C. (2001) Global Change Related to Rodinia and Gondwana. Gondwana Research, 4 (4) 598-599 doi:10.1016/s1342-937x(05)70401-9
Shanker, Ravi, Singh, Gopal, Kumar, Gopendra, Maithy, P.K. (2001) Assembly and Break-up of Rodinia and Gondwana — Evidence from India. Gondwana Research, 4 (4) 783-784 doi:10.1016/s1342-937x(05)70565-7
Kampunzu, A.B., Tembo, F., Huntsman-Mapila, P. (1999) Break-up of Rodinia in Central and Southwestern Africa and Implication for the Evolution of West Gondwana: Evidence from Geochemistry of Igneous Mafic Units Within the Pan-African Belt. Gondwana Research, 2 (4) 572-573 doi:10.1016/s1342-937x(05)70201-x
CONDIE, K (2001) Rodinia and Continental Growth. Gondwana Research, 4 (2) 154-155 doi:10.1016/s1342-937x(05)70673-0
 
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