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dc.contributor.author De Waele, B.
dc.contributor.author Kampunzu, A.B.
dc.contributor.author Mapani, B.S.E.
dc.contributor.author Tembo, F.
dc.date.accessioned 2009-10-28T06:46:08Z
dc.date.available 2009-10-28T06:46:08Z
dc.date.issued 2006
dc.identifier.citation De Waele, B. et al (2006) The Mesoproterozoic Irumide belt of Zambia, Journal of African Earth Sciences, Vol. 46, pp. 36–70 en_US
dc.identifier.issn 1464-343X
dc.identifier.uri http://hdl.handle.net/10311/398
dc.description.abstract The Mesoproterozoic Irumide belt is a northeast-trending structural province stretching from central Zambia to the Zambia–Tanzania border and northern Malawi. Mesoproterozoic and Neoproterozoic transcurrent shear zones within reactivated parts of the Palaeoproterozoic Ubendian belt define its northeastern limit. The northwestern margin is defined by the largely undeformed basement lithologies of the Bangweulu block. An intensely folded and sheared zone at the southeastern margin of the Mporokoso Group sedimentary depocentre on the Bangweulu block, interpreted to have developed above a thrust at the basement-cover interface, indicates that far-field effects of the Irumide Orogen also affected the southeastern part of the Bangweulu block sedimentary cover. To the west and southwest, Irumide and basement lithologies were reworked by the Damara–Lufilian–Zambezi Orogen within the Neoproterozoic Zambezi and Lufilian belts. The Choma–Kalomo block, previously regarded as the southwesterly continuation of the Irumide belt, is a distinct Mesoproterozoic province, while a succession of structurally juxtaposed tectonic terranes in eastern Zambia record a deformation event related to the Irumide Orogen. The lithological units identified in the Irumide belt include: (1) limited Neoarchaean rocks emplaced between 2.73 and 2.61 Ga and representing the oldest rocks in the Bangweulu block; (2) ca. 2.05–1.85 Ga volcano-plutonic complexes and gneisses representing the most important components in the Bangweulu block; (3) an extensive quartzite–metapelite succession with minor carbonate forming the Muva Supergroup, and deposited at ca. 1.85 Ga; (4) granitoids emplaced between 1.65 and 1.55 Ga; (5) a minor suite of anorogenic plutons (nepheline syenite and biotite granite) restricted to the far northeastern Irumide belt and emplaced between 1.36 and 1.33 Ga; (6) voluminous syn- to post-kinematic Irumide granitoids emplaced between 1.05 and 0.95 Ga. Crustal shortening and thickening in the Irumide belt are shown by northwestward-directed thrusts and related folds and metamorphic parageneses recording a clockwise medium-pressure/medium-temperature P–T–t path. Metamorphic grades range from greenschist facies in the foreland to the northwest to upper amphibolite facies in the southeast, with local granulites. Peak metamorphism is diachronous across the belt and bracketed between 1.05 in the southeast and 1.02 Ga in the northwest. en_US
dc.language.iso en en_US
dc.publisher Elsevier www.elsevier.com/locate/jafrearsci en_US
dc.subject Irumide belt en_US
dc.subject Palaeoproterozoic Muva Supergroup en_US
dc.subject Mesoproterozoic granitoids en_US
dc.subject Bangweulu block en_US
dc.title The Mesoproterozoic Irumide belt of Zambia en_US
dc.type Published Article en_US


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