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Maboko, M.A.H (2000) Nd and Sr isotopic investigation of the Archean–Proterozoic boundary in north eastern Tanzania: constraints on the nature of Neoproterozoic tectonism in the Mozambique Belt. Precambrian Research, 102 (1) 87-98 doi:10.1016/s0301-9268(00)00060-7

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Reference TypeJournal (article/letter/editorial)
TitleNd and Sr isotopic investigation of the Archean–Proterozoic boundary in north eastern Tanzania: constraints on the nature of Neoproterozoic tectonism in the Mozambique Belt
JournalPrecambrian Research
AuthorsMaboko, M.A.HAuthor
Year2000 (July)Volume102
Issue1
PublisherElsevier BV
URL
DOIdoi:10.1016/s0301-9268(00)00060-7Search in ResearchGate
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Mindat Ref. ID704102Long-form Identifiermindat:1:5:704102:4
GUID0
Full ReferenceMaboko, M.A.H (2000) Nd and Sr isotopic investigation of the Archean–Proterozoic boundary in north eastern Tanzania: constraints on the nature of Neoproterozoic tectonism in the Mozambique Belt. Precambrian Research, 102 (1) 87-98 doi:10.1016/s0301-9268(00)00060-7
Plain TextMaboko, M.A.H (2000) Nd and Sr isotopic investigation of the Archean–Proterozoic boundary in north eastern Tanzania: constraints on the nature of Neoproterozoic tectonism in the Mozambique Belt. Precambrian Research, 102 (1) 87-98 doi:10.1016/s0301-9268(00)00060-7
In(2000, July) Precambrian Research Vol. 102 (1) Elsevier BV

See Also

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Maboko, M.A.H., Nakamura, E. (1996) Nd and Sr isotopic mapping of the Archaean-Proterozoic boundary in southeastern Tanzania using granites as probes for crustal growth. Precambrian Research, 77 (1) 105-115 doi:10.1016/0301-9268(95)00048-8
Maboko, M.A.H., Nakamura, E. (2002) Isotopic dating of Neoproterozoic crustal growth in the Usambara Mountains of Northeastern Tanzania: evidence for coeval crust formation in the Mozambique Belt and the Arabian–Nubian Shield. Precambrian Research, 113 (3) 227-242 doi:10.1016/s0301-9268(01)00213-3
Manya, S., Maboko, M.A.H. (2003) Dating basaltic volcanism in the Neoarchaean Sukumaland Greenstone Belt of the Tanzania Craton using the Sm–Nd method: implications for the geological evolution of the Tanzania Craton. Precambrian Research, 121 (1) 35-45 doi:10.1016/s0301-9268(02)00195-x
Maboko, M.A.H. (2001) Isotopic and geochemical constraints on Neoproterozoic crust formation in the Wami River area, eastern Tanzania. Journal of African Earth Sciences, 33 (1) 91-101 doi:10.1016/s0899-5362(01)90092-2
Maboko, M.A.H. (2001) Dating Post-Metamorphic Cooling of the Eastern Granulites in the Mozambique Belt of Northern Tanzania Using the Garnet Sm-Nd Method. Gondwana Research, 4 (3) 329-336 doi:10.1016/s1342-937x(05)70333-6
Riller, U (1999) Transpressive tectonism in the eastern Penokean orogen, Canada Consequences for Proterozoic crustal kinematics and continental fragmentation. Precambrian Research, 93 (1) 51-70 doi:10.1016/s0301-9268(98)00097-7
Dickin, A.P., Guo, A. (2001) The location of the Allochthon Boundary Thrust and the Archean–Proterozoic suture in the Mattawa area of the Grenville Province: Nd isotope evidence. Precambrian Research, 107 (1) 31-43 doi:10.1016/s0301-9268(00)00153-4
Maboko, M. A. H. (1995) Neodymium isotopic constraints on the protolith ages of rocks involved in Pan-African tectonism in the Mozambique Belt of Tanzania. Journal of the Geological Society, 152 (6) 911-916 doi:10.1144/gsl.jgs.1995.152.01.05
Maboko, M (1995) Sm_Nd garnet ages from the Uluguru granulite complex of Eastern Tanzania: further evidence for post-metamorphic slow cooling in the Mozambique belt. Precambrian Research, 74 (4) 195-202 doi:10.1016/0301-9268(95)00008-s
Lan, C (2003) Geochemical and Sr–Nd isotopic constraints from the Kontum massif, central Vietnam on the crustal evolution of the Indochina block. Precambrian Research, 122 (1) 7-27 doi:10.1016/s0301-9268(02)00205-x
Rickers, Karen, Mezger, Klaus, Raith, Michael M (2001) Evolution of the Continental Crust in the Proterozoic Eastern Ghats Belt, India and new constraints for Rodinia reconstruction: implications from Sm–Nd, Rb–Sr and Pb–Pb isotopes. Precambrian Research, 112 (3) 183-210 doi:10.1016/s0301-9268(01)00146-2
 
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