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Relevant bibliographies by topics / Stratigraphy – Namibia

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Dissertations / Theses
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Academic literature on the topic 'Stratigraphy – Namibia'

Author: Grafiati

Published: 4 June 2021

Last updated: 12 February 2022

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Journal articles on the topic "Stratigraphy – Namibia"

1

Light, M. P. R., M. P. Maslanyj, R. J. Greenwood, and N. L. Banks. "Seismic sequence stratigraphy and tectonics offshore Namibia." Geological Society, London, Special Publications 71, no. 1 (1993): 163–91. http://dx.doi.org/10.1144/gsl.sp.1993.071.01.08.

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FRYBERGER, STEVEN G., PATRICK HESP, and KATHLEEN HASTINGS. "Aeolian granule ripple deposits, Namibia." Sedimentology 39, no. 2 (1992): 319–31. http://dx.doi.org/10.1111/j.1365-3091.1992.tb01041.x.

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3

Cook, Robert B. "Connoisseur'sChoice: Cerussite, Tsumeb, Namibia." Rocks & Minerals 72, no. 3 (1997): 176–80. http://dx.doi.org/10.1080/00357529709605035.

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Cook, Robert B. "Connoisseur's Choice: Mimetite, Tsumeb, Namibia." Rocks & Minerals 76, no. 2 (2001): 114–17. http://dx.doi.org/10.1080/00357520109603204.

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5

Cook, Robert B. "Connoisseur's Choice: Smithsonite, Tsumeb, Namibia." Rocks & Minerals 75, no. 3 (2000): 176–79. http://dx.doi.org/10.1080/00357520009605637.

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Cook, Robert B. "Connoisseur's Choice: Dioptase, Tsumeb, Namibia." Rocks & Minerals 77, no. 3 (2002): 176–80. http://dx.doi.org/10.1080/00357529.2002.9926680.

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Pohwat, Paul W. "Connoisseur's Choice: Tennantite, Tsumeb, Namibia." Rocks & Minerals 86, no. 4 (2011): 330–37. http://dx.doi.org/10.1080/00357529.2011.583601.

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Bowell, Robert J., and Janet H. Clifford. "Connoisseur's Choice: Leadhillite, Tsumeb, Namibia." Rocks & Minerals 89, no. 4 (2014): 354–63. http://dx.doi.org/10.1080/00357529.2014.904665.

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Southwood, Malcolm. "Connoisseur's Choice: Ekatite, Tsumeb, Namibia." Rocks & Minerals 93, no. 6 (2018): 524–27. http://dx.doi.org/10.1080/00357529.2018.1502581.

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Southwood, Malcolm. "Connoisseur's Choice: Minrecordite, Tsumeb, Namibia." Rocks & Minerals 95, no. 1 (2019): 42–47. http://dx.doi.org/10.1080/00357529.2020.1670563.

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Dissertations / Theses on the topic "Stratigraphy – Namibia"

1

Bagguley, Joanne Gail. "The application of seismic and sequence stratigraphy to the post-rift megasequence offshore Namibia." Thesis, Online version, 1996. http://ethos.bl.uk/OrderDetails.do?did=1&uin=uk.bl.ethos.388958.

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Smith, Odin Alonso 1973. "Terminal proterozoic carbonate platform development : stratigraphy and sedimentology of the Kuibis Subgroup (ca. 550-548 Ma), Northern Nama Basin, Namibia." Thesis, Massachusetts Institute of Technology, 1999. http://hdl.handle.net/1721.1/36672.

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Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 1999.<br>Includes bibliographical references (leaves 61-79).<br>A stratigraphic and sedimentologic investigation of the Kuibis Subgroup, northern Nama Basin, was undertaken. An U-Pb zircon age determination on an intercalated volcanic ash directly constrains the age of the subgroup to be on the order of 550-548 Ma. The study involved logging eight sections which were measured and described in detail, spanning the region extending from Driedoornvlagte, located east of the Naukluft mountain

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3

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.

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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

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4

Hartmann, Kerstin. "Jungquartäre Reliefentwicklung, Substratgenese, Klimageschichte und aktuelle Morphodynamik am Ostrand der Namib in der Region Hartmannstal-Marienflusstal (NW-Namibia) /." Köln : Geograph. Inst. der Univ. zu Köln, 2007. http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&doc_number=016293693&line_number=0002&func_code=DB_RECORDS&service_type=MEDIA.

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5

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.

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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

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Saylor, Beverly Z. (Beverly Zella). "Sequence stratigraphic and chemostratigraphic constraints on the evolution of the terminal Proterozoic to Cambrian Nama Basin, Namibia." Thesis, Massachusetts Institute of Technology, 1996. http://hdl.handle.net/1721.1/10668.

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Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 1996.<br>Includes bibliographical references (p. 117-124).<br>by Beverly Z. Saylor.<br>Ph.D.

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7

Runds, Megan Jean. "Sedimentology and depositional environment of a marine target, Southern Namibia: 3D stratigraphic architecture and diamond mineralisation potential." Master's thesis, University of Cape Town, 2018. http://hdl.handle.net/11427/28120.

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The world's largest diamond placer lies on the southwestern coast of Namibia, within the restricted area known as the Sperrgebiet, and comprises, amongst others, a series of Plio-Pleistocene to Holocene littoral deposits preserved onshore for >120 km northwards from the Orange River mouth. Through comprehensive seismic and sedimentological analysis, this study provides the first attempt at linking the well-documented onshore diamondiferous deposits of the Sperrgebiet with the submerged landscape of a diamondiferous marine target, called the Purple Target Area (PTA), situated beneath up to 70 m

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DiBenedetto, Steven P. (Steven Paul) 1976. "High resolution sedimentologic and stratigraphic investigation of a storm-dominated carbonate ramp, Hoogland Platform (ca. 549 Ma), Nama Group, Namibia." Thesis, Massachusetts Institute of Technology, 2002. http://hdl.handle.net/1721.1/57764.

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Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 2002.<br>Includes bibliographical references.<br>A high resolution stratigraphic study of the Terminal Proterozoic (ca 549 Ma) Hoogland Member of the Kuibis Subgroup, Nama Group, Namibia, revealed the controls on overall carbonate ramp platform morphology in a storm-dominated foreland basin setting. It was found that a generalized suite or class of physical processes that act to restore the seafloor to a relatively flat state by sweeping sediment from the highs and deposit in the lows doe

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Nxumalo, Valerie. "Stratigraphy and basin modelling of the Gemsbok Sub-Basin (Karoo Supergroup) of Botswana and Namibia." Thesis, 2011. http://hdl.handle.net/10539/10167.

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The Gemsbok Sub-basin is situated in the south-western corner of the Kalahari Karoo Basin and extends south from the Kgalagadi District of Botswana into the Northern Cape (South Africa); and west into the Aranos Basin (southeast Namibia). The Sub-basin preserves a heterogeneous succession of Upper Palaeozoic to Lower Mesozoic sedimentary and volcanic rocks of the Karoo Supergroup. Because the succession is largely covered by the Cenozoic Kalahari Group, the stratigraphy of the succession is not as well understood as the Main Karoo Basin in South Africa. Most research in the Gemsbok Sub-

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10

Werner, Mario. "The stratigraphy, sedimentology, and age of the Late Palaeozoic Mesosaurus Inland Sea, SW-Gondwana : new implications from studies on sediments and altered pyroclastic layers of the Dwyka and Ecca Group (lower Karoo Supergroup) in southern Namibia." Doctoral thesis, 2006. https://nbn-resolving.org/urn:nbn:de:bvb:20-opus-21757.

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The Mesosaurus Inland Sea covered, in the Late Paleozoic, vast areas (~5 Mio km2) of the SW-Gondwanan continental interior. Major depocentres are represented by the Karoo basins of SW-Africa and the Paraná Basin in South America. These areas were interconnected prior to the break-up of Gondwana and the subsequent opening of the South Atlantic Ocean. In Namibia and South Africa deposits of the Mesosaurus Inland Sea are preserved in the successions of the glacial Dwyka Group and the postglacial Ecca Group (Karoo Supergroup). These deposits comprise the major part of a 60-70 Ma depositional cycle

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Books on the topic "Stratigraphy – Namibia"

1

T, Becker, and Geological Survey (Namibia), eds. The geology of Namibia. Ministry of Mines and Energy, Geological Survey, 2008.

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2

Jungquartäre Reliefentwicklung, Substratgenese, Klimageschichte und aktuelle Morphodynamik am Ostrand der Namib in der Region Hartmannstal-Marienflusstal (NW-Namibia). Geographisches Institut der Universität zu Köln, 2007.

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3

Ziegler, U. R. F. Age determinations in the Rehoboth Basement Inlier, Namibia. Geological Survey of Namibia, Ministry of Mines and Energy, 1993.

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4

Kukla, Peter A. Tectonics and sedimentation of a Late Proterozoic Damaran convergent continental margin, Khomas Hochland, Central Namibia. Edited by Galloway Clare Kennedy. Ministry of Mines and Energy, Geological Survey of Namibia, 1992.

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5

Horsthemke, Ewald. Fazies der Karoosedimente in der Huab-Region, Damaraland, NW-Namibia. Im Selbstverlag der Geologischen Institute der Georg-August-Universität Göttingen, 1992.

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6

Hoal, B. G. The geology and geochemistry of the Proterozoic Awasib Mountain terrain, southern Namibia. Ministry of Mines and Energy, Geological Survey of Namibia, 1990.

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7

Swart, Roger. The sedimentology of the Zerrissene turbidite system, Damara Orogen, Namibia. Ministry of Mines and Energy, Geological Survey of Namibia, 1992.

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8

Ward, J. D., Ph. D. The Cenozoic succession in the Kuiseb Valley, central Namib Desert. Geological Survey of South West Africa/Namibia, 1987.

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9

Carvalho, Heitor de. The Precambrian of SW Angola and NW Namibia: General remarks, correlation analysis, economic geology. Edição Financiada Pelo, Instituto Para a Cooperação Económica, 1993.

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10

Richter, Jürgen. Studien zur Urgeschichte Namibias: Holozäne Stratigraphien im Umkreis des Brandberges. Heinrich-Barth-Institut, 1991.

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Conference papers on the topic "Stratigraphy – Namibia"

1

Quinn, Daven P., and J. P. Grotzinger. "STRATIGRAPHY AND SEDIMENTOLOGY OF THE ZEBRA NAPPE, NAUKLUFT NAPPE COMPLEX, NAMIBIA." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-287992.

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2

Turk, Katherine A., and Simon A. F. Darroch. "INTEGRATED ICHNOLOGY AND STRATIGRAPHY OF THE LATE EDIACARAN NASEP-HUNS TRANSITION (NAMA GROUP, SOUTHERN NAMIBIA)." In Joint 69th Annual Southeastern / 55th Annual Northeastern GSA Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020se-345160.

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Quinn, Daven P., John P. Grotzinger, and Theodore M. Present. "A SEQUENCE-STRATIGRAPHIC FRAMEWORK FOR THE ZEBRA NAPPE, SOUTHERN NAUKLUFT MOUNTAINS, NAMIBIA." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-323354.

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4

McBride, John H., Jani Radebaugh, Clayton K. Chandler, and R. William Keach, II. "High-resolution imaging of internal stratigraphy of linear dunes of the Namib Sand Sea." In SEG Technical Program Expanded Abstracts 2020. Society of Exploration Geophysicists, 2020. http://dx.doi.org/10.1190/segam2020-3426004.1.

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