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Journal articles on the topic 'Geology, Structural – Namibia – Kaoko Belt'

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1

Goscombe, Ben, David Gray, Richard Armstrong, David A. Foster, and James Vogl. "Event geochronology of the Pan-African Kaoko Belt, Namibia." Precambrian Research 140, no. 3-4 (2005): 103.e1–103.e41. http://dx.doi.org/10.1016/j.precamres.2005.07.003.

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2

Luft, João Luiz, Farid Chemale, and Maria de Fátima Bitencourt. "Significance of Paleoproterozoic to Neoproterozoic Ages in the Kaoko Belt, NW Namibia." Gondwana Research 4, no. 4 (2001): 693. http://dx.doi.org/10.1016/s1342-937x(05)70489-5.

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3

Goscombe, Ben, Martin Hand, and David Gray. "Structure of the Kaoko Belt, Namibia: progressive evolution of a classic transpressional orogen." Journal of Structural Geology 25, no. 7 (2003): 1049–81. http://dx.doi.org/10.1016/s0191-8141(02)00150-5.

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4

Seth, B. "Isotope constraints on the origin of Pan-African granitoid rocks in the Kaoko belt, NW Namibia." South African Journal of Geology 105, no. 2 (2002): 179–92. http://dx.doi.org/10.2113/105.2.179.

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5

Konopásek, Jiří, Stephan Kröner, Shawn L. Kitt, Cees W. Passchier, and Alfred Kröner. "Oblique collision and evolution of large-scale transcurrent shear zones in the Kaoko belt, NW Namibia." Precambrian Research 136, no. 2 (2005): 139–57. http://dx.doi.org/10.1016/j.precamres.2004.10.005.

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6

Seth, B., A. Kröner, K. Mezger, A. A. Nemchin, R. T. Pidgeon, and M. Okrusch. "Archaean to Neoproterozoic magmatic events in the Kaoko belt of NW Namibia and their geodynamic significance." Precambrian Research 92, no. 4 (1998): 341–63. http://dx.doi.org/10.1016/s0301-9268(98)00086-2.

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7

Stanistreet, I. G. "Damaran basement-cored fold nappes incorporating pre-collisional basins, Kaoko Belt, Namibia, and controls on Mesozoic supercontinental break-up." South African Journal of Geology 104, no. 1 (2001): 1–12. http://dx.doi.org/10.2113/104.1.1.

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8

Janoušek, V., J. Konopásek, S. Ulrich, V. Erban, L. Tajčmanová, and P. Jeřábek. "Geochemical character and petrogenesis of Pan-African Amspoort suite of the Boundary Igneous Complex in the Kaoko Belt (NW Namibia)." Gondwana Research 18, no. 4 (2010): 688–707. http://dx.doi.org/10.1016/j.gr.2010.02.014.

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9

Konopásek, Jiří, Jan Košler, Jiří Sláma, and Vojtěch Janoušek. "Timing and sources of pre-collisional Neoproterozoic sedimentation along the SW margin of the Congo Craton (Kaoko Belt, NW Namibia)." Gondwana Research 26, no. 1 (2014): 386–401. http://dx.doi.org/10.1016/j.gr.2013.06.021.

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10

Will, T. M. "Barrovian and Buchan type metamorphism in the Pan-African Kaoko belt, Namibia: implications for its geotectonic position within the framework of Western Gondwana." South African Journal of Geology 107, no. 3 (2004): 431–54. http://dx.doi.org/10.2113/107.3.431.

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11

Basson, I. J., M. J. McCall, J. Andrew, and E. Daweti. "Structural controls on mineralisation at the Namib Lead and Zinc Mine, Damara Belt, Namibia." Ore Geology Reviews 95 (April 2018): 931–44. http://dx.doi.org/10.1016/j.oregeorev.2018.03.028.

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12

Kroner, S. "U-Pb and Pb-Pb zircon ages for metamorphic rocks in the Kaoko Belt of Northwestern Namibia: A Palaeo- to Mesoproterozoic basement reworked during the Pan-African orogeny." South African Journal of Geology 107, no. 3 (2004): 455–76. http://dx.doi.org/10.2113/107.3.455.

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13

Brayshaw, M. M., and M. K. Watkeys. "Structural evolution and architecture of the outer margin of the Gariep Belt at Rosh Pinah, southern Namibia." South African Journal of Geology 121, no. 2 (2018): 171–90. http://dx.doi.org/10.25131/sajg.121.0011.

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14

Jung, S., S. Brandt, O. Nebel, E. Hellebrand, B. Seth, and C. Jung. "The P–T–t paths of high-grade gneisses, Kaoko Belt, Namibia: Constraints from mineral data, U–Pb allanite and monazite and Sm–Nd/Lu–Hf garnet ages and garnet ion probe data." Gondwana Research 25, no. 2 (2014): 775–96. http://dx.doi.org/10.1016/j.gr.2013.05.017.

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15

Kitt, Shawn, Alexander Kisters, Ian Buick, and Jan Kramers. "Structural, geochronological and P-T constraints on subduction-accretion processes in a Pan-African accretionary wedge – The Deep Level Southern Zone of the Damara Belt in Namibia." Precambrian Research 310 (June 2018): 39–62. http://dx.doi.org/10.1016/j.precamres.2018.02.012.

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16

Hoffman, P. F. "On the kinematics and timing of Rodinia breakup: a possible rift–transform junction of Cryogenian age at the southwest cape of Congo Craton (northwest Namibia)." South African Journal of Geology, May 31, 2021. http://dx.doi.org/10.25131/sajg.124.0038.

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Abstract:
Abstract After tilt correction for Ediacaran thick-skinned folding, a pair of Cryogenian half grabens at the autochthonous southwest cape of Congo Craton (CC) in northwest Namibia restore to different orientations. Toekoms sub-basin trended east-northeast, parallel to Northern Zone (NZ) of Damara belt, and was bounded by a normal-sense growth fault (2 290 m throw) dipping 57° toward CC. Soutput sub-basin trended northwest, oblique to NZ and to north-northwest-trending Kaoko Belt. It was bounded by a growth fault (750 m down-dip throw) dipping steeply (~75°) toward CC. Soutput growth fault coul
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