Relevant bibliographies by topics / Structural geology – Namibia – Damara belt / Journal articles
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Journal articles on the topic 'Structural geology – Namibia – Damara belt'

Author: Grafiati
Published: 4 June 2021
Last updated: 8 February 2022

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1

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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2

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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3

Hawkesworth, C. J., M. A. Menzies, and P. van Calsteren. "Geochemical and tectonic evolution of the Damara Belt, Namibia." Geological Society, London, Special Publications 19, no. 1 (1986): 305–19. http://dx.doi.org/10.1144/gsl.sp.1986.019.01.17.

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4

Meneghini, Francesca, Alex Kisters, Ian Buick, and Åke Fagereng. "Fingerprints of late Neoproterozoic ridge subduction in the Pan-African Damara belt, Namibia." Geology 42, no. 10 (2014): 903–6. http://dx.doi.org/10.1130/g35932.1.

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5

Toé, W., O. Vanderhaeghe, A. S. André-Mayer, J. L. Feybesse, and J. P. Milési. "From migmatites to granites in the Pan-African Damara orogenic belt, Namibia." Journal of African Earth Sciences 85 (September 2013): 62–74. http://dx.doi.org/10.1016/j.jafrearsci.2013.04.009.

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6

Goscombe, Ben, David A. Foster, David Gray, and Ben Wade. "Metamorphic response and crustal architecture in a classic collisional orogen: The Damara Belt, Namibia." Gondwana Research 52 (December 2017): 80–124. http://dx.doi.org/10.1016/j.gr.2017.07.006.

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7

Cross, C. B., J. F. A. Diener, and Å. Fagereng. "Metamorphic imprint of accretion and ridge subduction in the Pan-African Damara Belt, Namibia." Journal of Metamorphic Geology 33, no. 6 (2015): 633–48. http://dx.doi.org/10.1111/jmg.12139.

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8

Bačík, Peter, Jana Fridrichová, Pavel Uher, et al. "Beryl crystal chemistry and trace elements: Indicators of pegmatite development and fractionation (Damara Belt, Namibia)." Lithos 404-405 (December 2021): 106441. http://dx.doi.org/10.1016/j.lithos.2021.106441.

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9

Lehmann, Jérémie, Kerstin Saalmann, Kalin V. Naydenov, et al. "Structural and geochronological constraints on the Pan-African tectonic evolution of the northern Damara Belt, Namibia." Tectonics 35, no. 1 (2016): 103–35. http://dx.doi.org/10.1002/2015tc003899.

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10

de Kock, Gerrit S. "Forearc basin evolution in the Pan-African Damara Belt, central Namibia: the Hureb formation of the Khomas zone." Precambrian Research 57, no. 3-4 (1992): 169–94. http://dx.doi.org/10.1016/0301-9268(92)90001-5.

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11

Clemens, J. D., and A. F. M. Kisters. "Magmatic indicators of subduction initiation: The bimodal Goas intrusive Suite in the Pan-African Damara Belt of Namibia." Precambrian Research 362 (August 2021): 106309. http://dx.doi.org/10.1016/j.precamres.2021.106309.

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12

Whitehead, Kerryn, Anton Le Roex, Cornelia Class, and David Bell. "Composition and Cretaceous thermal structure of the upper mantle beneath the Damara Mobile Belt: evidence from nephelinite-hosted peridotite xenoliths, Swakopmund, Namibia." Journal of the Geological Society 159, no. 3 (2002): 307–21. http://dx.doi.org/10.1144/0016-764901-113.

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13

Johnson, S. D., M. Poujol, and A. F. M. Kisters. "Constraining the timing and migration of collisional tectonics in the Damara Belt, Namibia: U-Pb zircon ages for the syntectonic Salem-type Stinkbank granite." South African Journal of Geology 109, no. 4 (2006): 611–24. http://dx.doi.org/10.2113/gssajg.109.4.611.

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14

Longridge, L., J. Kinnaird, R. Gibson, C. Hawkesworth, and R. Armstrong. "Crustal recycling in the Damara Belt, Namibia, and interaction of the Congo and Kalahari Cratons – evidence from zircon U-Pb, Hf and O isotopes." South African Journal of Geology 121, no. 3 (2018): 237–52. http://dx.doi.org/10.25131/sajg.121.0018.

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15

Jung, S., A. Kröner, F. Hauff, and P. Masberg. "Petrogenesis of synorogenic diorite–granodiorite–granite complexes in the Damara Belt, Namibia: Constraints from U–Pb zircon ages and Sr–Nd–Pb isotopes." Journal of African Earth Sciences 101 (January 2015): 253–65. http://dx.doi.org/10.1016/j.jafrearsci.2014.09.015.

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16

Kisters, A. F. M. "Controls of gold-quartz vein formation during regional folding in amphibolite-facies, marble-dominated metasediments of the Navachab Gold Mine in the Pan-African Damara Belt, Namibia." South African Journal of Geology 108, no. 3 (2005): 365–80. http://dx.doi.org/10.2113/108.3.365.

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17

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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18

Jung, Stefan, Soenke Brandt, Rebecca Bast, Erik E. Scherer, and Jasper Berndt. "Metamorphic petrology of a high-T /low-P granulite terrane (Damara belt, Namibia) - Constraints from pseudosection modelling and high-precision Lu-Hf garnet-whole rock dating." Journal of Metamorphic Geology 37, no. 1 (2018): 41–69. http://dx.doi.org/10.1111/jmg.12448.

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19

Kisters, Alexander F. M., L. Smith Jordaan, and Kathrin Neumaier. "Thrust-related dome structures in the Karibib district and the origin of orthogonal fabric domains in the south Central Zone of the Pan-African Damara belt, Namibia." Precambrian Research 133, no. 3-4 (2004): 283–303. http://dx.doi.org/10.1016/j.precamres.2004.05.001.

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20

Fuchsloch, Warrick C., Paul A. M. Nex, and Judith A. Kinnaird. "The geochemical evolution of Nb–Ta–Sn oxides from pegmatites of the Cape Cross–Uis pegmatite belt, Namibia." Mineralogical Magazine 83, no. 02 (2018): 161–79. http://dx.doi.org/10.1180/mgm.2018.151.

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AbstractThe Cape Cross–Uis pegmatite belt, Damara Orogen, north-central Namibia hosts multiple Ta–Nb- and Sn-oxide-bearing pegmatites. Columbite-group minerals, tapiolite, cassiterite and minor ixiolite and wodginite occur in abundance within pegmatites and display various compositional and internal structural mineralogical variations. Ta–Nb oxides display various zonation patterns indicative of multiple crystallisation phases, whereas cassiterite is dominantly homogeneous with minor euhedral columbite-group mineral inclusions. Ta–Nb oxides are mostly rich in Fe, with fractionation patterns in
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21

Jung, S., and K. Mezger. "Geochronology in migmatites - a Sm-Nd, U-Pb and Rb-Sr study from the Proterozoic Damara belt (Namibia): implications for polyphase development of migmatites in high-grade terranes." Journal of Metamorphic Geology 19, no. 1 (2001): 77–97. http://dx.doi.org/10.1046/j.0263-4929.2000.00297.x.

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22

Kitt, Shawn, Alexander Kisters, Nick Steven, Ken Maiden, and Karl Hartmann. "Shear-zone hosted copper mineralisation of the Omitiomire deposit — Structural controls of fluid flow and mineralisation during subduction accretion in the Pan-African Damara Belt of Namibia." Ore Geology Reviews 75 (June 2016): 1–15. http://dx.doi.org/10.1016/j.oregeorev.2015.10.035.

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23

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 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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