Relevant bibliographies by topics / Structural geology – Namibia – Damara belt

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books

Academic literature on the topic 'Structural geology – Namibia – Damara belt'

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

Create a spot-on reference in APA, MLA, Chicago, Harvard, and other styles

Select a source type:

Consult the lists of relevant articles, books, theses, conference reports, and other scholarly sources on the topic 'Structural geology – Namibia – Damara belt.'

Next to every source in the list of references, there is an 'Add to bibliography' button. Press on it, and we will generate automatically the bibliographic reference to the chosen work in the citation style you need: APA, MLA, Harvard, Chicago, Vancouver, etc.

You can also download the full text of the academic publication as pdf and read online its abstract whenever available in the metadata.

Journal articles on the topic "Structural geology – Namibia – Damara belt"

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.

Full text
APA, Harvard, Vancouver, ISO, and other styles
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.

Full text
APA, Harvard, Vancouver, ISO, and other styles
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.

Full text
APA, Harvard, Vancouver, ISO, and other styles
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.

Full text
APA, Harvard, Vancouver, ISO, and other styles
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.

Full text
APA, Harvard, Vancouver, ISO, and other styles
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.

Full text
APA, Harvard, Vancouver, ISO, and other styles
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.

Full text
APA, Harvard, Vancouver, ISO, and other styles
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.

Full text
APA, Harvard, Vancouver, ISO, and other styles
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.

Full text
APA, Harvard, Vancouver, ISO, and other styles
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.

Full text
APA, Harvard, Vancouver, ISO, and other styles
More sources

Dissertations / Theses on the topic "Structural geology – Namibia – Damara belt"

1

Johnson, Shannon D. "Structural geology of the Usakos Dome in the Damara Belt, Namibia." Thesis, Stellenbosch : Stellenbosch University, 2005. http://hdl.handle.net/10019.1/50457.

Full text
Abstract:
Thesis (MSc)--Stellenbosch University, 2005.<br>ENGLISH ABSTRACT: The northeast-trending south Central Zone (sCZ) of the Pan-African Damara belt in central Namibia is structurally characterized by kilometer-scale, northeast-trending dome structures developed in Neoproterozoic rocks of the Damara Sequence. A number of different structural models have been proposed for the formation of these domes in the literature. This study describes the structural geology of the Usakos dome. The study discusses the structural evolution of the dome within the regional framework of the cSZ that represen
APA, Harvard, Vancouver, ISO, and other styles
2

Petzel, V. "Vein and replacement type Sn and Sn-W mineralization in the Southern Kaoko Zone, Damara Province, South West Africa/Namibia." Thesis, Rhodes University, 1986. http://hdl.handle.net/10962/d1007633.

Full text
Abstract:
The ENE trending Brandberg West - Goantagab Sn-W belt is located in the Southern Kaoko Zone of the northern coastal branch of the Damara Orogen. The lithologies in this area are turbiditic and consist of three schist units separated by two marble horizons, all of which are correlated with the Swakop Group. The formations are intensely folded by at least three episodes of which the first two are coaxial and resulted in prominent, approximately N-S trending, structures. Sn and Sn-W mineralization predominantly occurs as vein and replacement type mineralization. Vein type mineralization occurs as
APA, Harvard, Vancouver, ISO, and other styles
3

Owen, Geoffrey J. "Geology of the Kranzberg syncline and emplacement controls of the Usakos pegmatite field, Damara belt, Namibia." Thesis, Stellenbosch : University of Stellenbosch, 2011. http://hdl.handle.net/10019.1/6743.

Full text
Abstract:
Thesis (MSc (Earth Sciences))--University of Stellenbosch, 2011.<br>ENGLISH ABSTRACT: The Central Zone (CZ) of the Damara belt in central Namibia is underlain by voluminous Pan-African granites and is host to numerous pegmatite occurrences, some of which have economic importance and have been mined extensively. This study discusses the occurrence, geometry, relative timing and emplacement mechanisms for the Usakos pegmatite field, located between the towns of Karibib and Usakos and within the core of the regional-scale Kranzberg syncline. Lithological mapping of the Kuiseb Formation in t
APA, Harvard, Vancouver, ISO, and other styles
4

Creus, Pieter Koenraad. "Geology and structural controls of lode-gold mineralisation around the Navachab Gold Mine in the Pan-African Damara Belt of Namibia." Thesis, Stellenbosch : Stellenbosch University, 2011. http://hdl.handle.net/10019.1/17845.

Full text
Abstract:
Thesis (MSc)--Stellenbosch University, 2011.<br>ENGLISH ABSTRACT: Numerous quartz-vein hosted gold prospects in the Karibib district in central Namibia testify to the presence of a large hydrothermal system during Pan-African times in rocks of the Damara Belt and centred around the Navachab Gold Mine. This study presents the results of the regional and detailed mapping of the Navachab synform, a NE-SW trending, regional-scale structure hosting a number of these gold prospects, locally referred to as the “zoo prospects”, in the direct vicinity of the main Navachab Gold Mine. The zoo prospects
APA, Harvard, Vancouver, ISO, and other styles
5

Anthonissen, Christoffel Jasper. "The mid-crustal architecture of a continental arc - a transect through the South Central Zone of the Pan-African Damara Belt, Namibia." Thesis, Stellenbosch : University of Stellenbosch, 2010. http://hdl.handle.net/10019.1/4172.

Full text
Abstract:
Thesis (MSc (Earth Sciences))--University of Stellenbosch, 2010.<br>ENGLISH ABSTRACT: The NE-trending South Central Zone of the Pan-African (ca. 550-500) Damara orogen in central Namibia exposes deeply eroded mid-crustal rocks, thought to represent the magmatic arc of the Damara orogen. Above average exposure of outcrop left unmodified by subsequent post-orogenic processes made it possible to study the internal architecture of a ca. 50km traverse, stretching from the continental suture-zone (between the Congo craton in the NW and the underplating Kalahari craton in the SE) at the Okahandj
APA, Harvard, Vancouver, ISO, and other styles
6

Guj, P., and P. Guj. "The Damara mobile belt in the south-Western Kaokoveld." Doctoral thesis, University of Cape Town, 2016. http://hdl.handle.net/11427/23739.

Full text
Abstract:
After the establishment of the N-S Andib-Ganamub trough, the ubiquitous Lower Nosib subarkose was succeeded in the west by the Upper Nosib greywacke which indicates that orthogeosynclinal subsidence was already active in pre-Damara times. A pulse of NNE folding (F₁N) concluded this sedinentary cycle and was accompanied by amphibolite-grade metamorphism (M₁), occasional migmatisation (A₁), and later feldspar blastesis. This episode was most intense in the west, so that the overlying Damara rocks paraconformable in the east, are unconformable there. Martin's (1965) separation of the succeeding D
APA, Harvard, Vancouver, ISO, and other styles
7

Hartnady, Michael Ian Hay. "The structural evolution of an ancient accretionary prism in the Damara Belt, Namibia." Master's thesis, University of Cape Town, 2015. http://hdl.handle.net/11427/15756.

Full text
Abstract:
The Southern Marginal Zone (SMZ) of the Damara Belt, exposed in the Gaub Canyon in central Namibia, consists of fourteen lithotectonic units of high strain amphiholite facies rock with pelagic, hemi-pelagic and clastic sedimentary protoliths. These rocks are intercalated With lenses of metabasite. Regional high-pressure - low-temperature metamorphic conditions (~1O kbar and ~600°C) dominate the Southern and Southern Marginal Zones of the Damara Belt, leading to the interpretation that these tectonostratigraphic terranes formed in an accretionary prism along an ancient subduction margin. The st
APA, Harvard, Vancouver, ISO, and other styles
8

Kitt, Shawn. "Structural controls of auriferous quartz veins in the Karibib Area, southern central zone of the Pan-African Damara Belt, Namibia." Thesis, Stellenbosch : Stellenbosch University, 2008. http://hdl.handle.net/10019.1/2547.

Full text
Abstract:
Thesis (MSc (Earth Sciences))--Stellenbosch University, 2008.<br>Detailed geological mapping and a structural analysis of auriferous quartz veins were undertaken in the Karibib region of the Pan-African Damara belt in central Namibia. The study focuses on the formation and controls of quartz-vein sets and associated lodegold mineralization in heterogeneous, siliciclastic- and marble- dominated amphibolitefacies host rocks around the Navachab gold mine and adjacent areas. Two main arrays of shallowly-dipping quartz veins can be distinguished that form a conjugate set. Steep, bedding-paral
APA, Harvard, Vancouver, ISO, and other styles
9

Vietze, Martin Ernst. "Geology and emplacement controls of the Stinkbank granite in the south Central Zone of the Pan-African Damara Belt, Namibia." Thesis, Stellenbosch : University of Stellenbosch, 2010. http://hdl.handle.net/10019.1/4271.

Full text
Abstract:
Thesis (MSc (Earth Sciences))--University of Stellenbosch, 2010.<br>ENGLISH SUMMARY: Regional mapping of the Stinkbank granite in the south Central Zone of the Damara Belt, focused on an area of ca. 150 km2 in the SW parts of the granite along well exposed sections of the Khan River to the SW of the town of Usakos. The granite forms part of the regionally widespread granite suite of Salem-type granites that intruded at ca. 550-540 Ma into amphibolite-facies rocks of the Damara Supergroup. The Stinkbank granite is intrusive into the regional-scale, NE-trending D2 Kransberg syncline, cored by sc
APA, Harvard, Vancouver, ISO, and other styles
10

Longridge, Luke. "Tectonothermal evolution of the Southwestern central zone, Damara Belt, Namibia." Thesis, 2013. http://hdl.handle.net/10539/12341.

Full text
Abstract:
This is an integrated study of the stratigraphy, deformation, magmatism, and metamorphism in the vicinity of the Ida and Palmenhorst Domes, an area in the southwestern Central Zone of the Damara Orogen, Namibia. The principal aim is to understand the timing of tectonic events through high-precision U-Pb dating of structurally constrained intrusions and anatectic rocks, and link these tectonic events across the Damara Orogen and Pan-African Orogeny. A secondary aim is to compare the Central Zone and Damara Orogen to other collisional orogens. The stratigraphy of the study area is similar to th
APA, Harvard, Vancouver, ISO, and other styles

Books on the topic "Structural geology – Namibia – Damara belt"

1

Martin, H., and F. W. Eder. Intracontinental Fold Belts: Case Studies in the Variscan Belt of Europe and the Damara Belt in Namibia. Springer, 2012.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
You might also be interested in the extended bibliographies on the topic 'Structural geology – Namibia – Damara belt' for particular source types:
Journal articles
We offer discounts on all premium plans for authors whose works are included in thematic literature selections. Contact us to get a unique promo code!

To the bibliography