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Journal articles on the topic 'Stratigraphy – Namibia'

Author: Grafiati

Published: 4 June 2021

Last updated: 12 February 2022

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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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2

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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4

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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6

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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7

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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8

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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9

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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10

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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11

Cook, Robert B. "Connoisseur's Choice: Prehnite Brandberg, Namibia." Rocks & Minerals 74, no. 3 (1999): 178–80. http://dx.doi.org/10.1080/00357529909602536.

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12

Southwood, Malcolm. "Connoisseur's Choice: Alamosite, Tsumeb, Namibia." Rocks & Minerals 96, no. 2 (2021): 158–63. http://dx.doi.org/10.1080/00357529.2021.1848218.

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13

Eckardt, F. D., and B. Spiro. "The origin of sulphur in gypsum and dissolved sulphate in the Central Namib Desert, Namibia." Sedimentary Geology 123, no. 3-4 (1999): 255–73. http://dx.doi.org/10.1016/s0037-0738(98)00137-7.

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14

Cook, Robert B. "Connoisseur's Choice: Spessartine Marienfluss, Northern Namibia." Rocks & Minerals 85, no. 1 (2009): 50–59. http://dx.doi.org/10.1080/00357520903458194.

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15

Bowell, Rob, and Robert B. Cook. "Connoisseur's Choice: Shattuckite Kunene District Kaokoveld, Namibia." Rocks & Minerals 84, no. 6 (2009): 544–50. http://dx.doi.org/10.1080/00357520903272231.

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16

Southwood, Malcolm, and James Robison. "Dolomite “Casts” and Epimorphs From Tsumeb, Namibia." Rocks & Minerals 91, no. 4 (2016): 334–45. http://dx.doi.org/10.1080/00357529.2016.1172174.

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17

Cairncross, Bruce. "Connoisseur's Choice: Leiteite, Tsumeb Mine, Tsumeb, Namibia." Rocks & Minerals 92, no. 3 (2017): 264–69. http://dx.doi.org/10.1080/00357529.2017.1283661.

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18

Cairncross, Bruce. "Minerals of Berg Aukas, Otavi Mountainland, Namibia." Rocks & Minerals 96, no. 2 (2021): 110–47. http://dx.doi.org/10.1080/00357529.2021.1848216.

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19

Ward, J. D. "Eolian, fluvial and pan (playa) facies of the Tertiary Tsondab Sandstone Formation in the central Namib Desert, Namibia." Sedimentary Geology 55, no. 1-2 (1988): 143–62. http://dx.doi.org/10.1016/0037-0738(88)90094-2.

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20

Kirkpatrick, Lynette H., Andrew N. Green, and John Pether. "The seismic stratigraphy of the inner shelf of southern Namibia: The development of an unusual nearshore shelf stratigraphy." Marine Geology 408 (February 2019): 18–35. http://dx.doi.org/10.1016/j.margeo.2018.11.016.

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21

Cairncross, Bruce, and Uli Bahmann. "Minerals from the Goboboseb Mountains: Brandberg Region, Namibia." Rocks & Minerals 81, no. 6 (2006): 442–57. http://dx.doi.org/10.3200/rmin.81.6.442-457.

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22

Cairncross, Bruce. "Connoisseur's Choice: Tarbuttite, Skorpion Mine, Lüderitz District, Namibia." Rocks & Minerals 94, no. 2 (2019): 150–57. http://dx.doi.org/10.1080/00357529.2019.1530039.

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23

Cook, Robert B. "Connoisseur's Choice: Azurite: Tsumeb, Namibia, and Touissit, Oujda, Morocco." Rocks & Minerals 77, no. 1 (2002): 40–43. http://dx.doi.org/10.1080/00357529.2002.9926655.

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24

Cairncross, Bruce. "The Where of Mineral Names: Karibibite, Karibib District, Namibia." Rocks & Minerals 95, no. 2 (2020): 174–79. http://dx.doi.org/10.1080/00357529.2019.1641030.

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25

Cairncross, Bruce. "Connoisseur's Choice: Nambulite, Kombat Mine, Grootfontein, Otjozondjupa Region, Namibia." Rocks & Minerals 95, no. 6 (2020): 530–34. http://dx.doi.org/10.1080/00357529.2020.1791625.

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26

Cairncross, Bruce. "Connoisseur's Choice: Boltwoodite, Goanikontes Claim, Arandis, Erongo Region, Namibia." Rocks & Minerals 96, no. 3 (2021): 238–47. http://dx.doi.org/10.1080/00357529.2021.1875746.

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27

GEYER, G. "The Fish River Subgroup in Namibia: stratigraphy, depositional environments and the Proterozoic–Cambrian boundary problem revisited." Geological Magazine 142, no. 5 (2005): 465–98. http://dx.doi.org/10.1017/s0016756805000956.

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The Fish River Subgroup of the Nama Group, southern Namibia, is restudied in terms of lithostratigraphy and depositional environment. The study is based on partly fine-scaled sections, particularly of the Nababis and Gross Aub Formation. The results are generally in accordance with earlier studies. However, braided river deposits appear to be less widely distributed in the studied area, and a considerable part of the formations of the middle and upper subgroup apparently were deposited under shallowest marine conditions including upper shore-face. Evidence comes partly from sedimentary feature

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28

COMPTON, JOHN S. "Holocene evolution of the Anichab Pan on the south-west coast of Namibia." Sedimentology 54, no. 1 (2007): 55–70. http://dx.doi.org/10.1111/j.1365-3091.2006.00826.x.

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29

Cairncross, Bruce. "Connoisseur's Choice: Mimetite after Cerussite (Part 2), Tsumeb Mine, Namibia." Rocks & Minerals 96, no. 4 (2021): 352–57. http://dx.doi.org/10.1080/00357529.2021.1901209.

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30

Mountney and Howell. "Aeolian architecture, bedform climbing and preservation space in the Cretaceous Etjo Formation, NW Namibia." Sedimentology 47, no. 4 (2000): 825–49. http://dx.doi.org/10.1046/j.1365-3091.2000.00318.x.

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31

Smith, R. M. H., T. R. Mason, and J. D. Ward. "Flash-flood sediments and ichnofacies of the Late Pleistocene Homeb Silts, Kuiseb River, Namibia." Sedimentary Geology 85, no. 1-4 (1993): 579–99. http://dx.doi.org/10.1016/0037-0738(93)90103-c.

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32

Bagguley, Joanne, and Sarah Prosser. "The interpretation of passive margin depositional processes using seismic stratigraphy: examples from offshore Namibia." Geological Society, London, Special Publications 153, no. 1 (1999): 321–44. http://dx.doi.org/10.1144/gsl.sp.1999.153.01.20.

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33

Le Ber, Erwan, Daniel P. Le Heron, Gerd Winterleitner, Dan W. J. Bosence, Bernie A. Vining, and Fred Kamona. "Microbialite recovery in the aftermath of the Sturtian glaciation: Insights from the Rasthof Formation, Namibia." Sedimentary Geology 294 (August 2013): 1–12. http://dx.doi.org/10.1016/j.sedgeo.2013.05.003.

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34

HOFFMAN, PAUL F. "Strange bedfellows: glacial diamictite and cap carbonate from the Marinoan (635 Ma) glaciation in Namibia." Sedimentology 58, no. 1 (2011): 57–119. http://dx.doi.org/10.1111/j.1365-3091.2010.01206.x.

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35

Swart, Roger. "The late Proterozoic Amis River Formation of Namibia—a turbidite system developed by vertical accretion." Sedimentary Geology 67, no. 1-2 (1990): 101–13. http://dx.doi.org/10.1016/0037-0738(90)90029-s.

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36

Pickford, Martin, Brigitte Senut, and Yannicke Dauphin. "Biostratigraphyof the Tsondab sandstone (Namibia) based on gigantic avian eggshells." Geobios 28, no. 1 (1995): 85–98. http://dx.doi.org/10.1016/s0016-6995(95)80205-3.

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37

Viles, Heather A., Mark P. Taylor, Kathleen Nicoll, and Stuart Neumann. "Facies evidence of hydroclimatic regime shifts in tufa depositional sequences from the arid Naukluft Mountains, Namibia." Sedimentary Geology 195, no. 1-2 (2007): 39–53. http://dx.doi.org/10.1016/j.sedgeo.2006.07.007.

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38

Hoffman, Paul F., Eric J. Bellefroid, Benjamin W. Johnson, Malcolm S. W. Hodgskiss, Daniel P. Schrag, and Galen P. Halverson. "Early extensional detachments in a contractional orogen: coherent, map-scale, submarine slides (mass transport complexes) on the outer slope of an Ediacaran collisional foredeep, eastern Kaoko belt, Namibia." Canadian Journal of Earth Sciences 53, no. 11 (2016): 1177–89. http://dx.doi.org/10.1139/cjes-2015-0164.

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The existence of coherent, large-scale, submarine landslides on modern continental margins implies that their apparent rarity in ancient orogenic belts is due to non-recognition. Two map-scale, coherent, pre-orogenic, normal-sense detachment structures of Ediacaran age are present in the Kaoko belt, a well-exposed arc–continent collision zone in northwestern Namibia. The structures occur within the Otavi Group, a Neoproterozoic carbonate shelf succession. They are brittle structures, evident only through stratigraphic omissions of 400 m or more, that ramp down to the west with overall ramp ang

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39

Cornell, D. H., M. Harris, B. S. Mapani, et al. "Dating of Guperas Formation rhyolites changes the stratigraphy of the Mesoproterozoic Sinclair Supergroup of Namibia." South African Journal of Geology 123, no. 4 (2020): 633–48. http://dx.doi.org/10.25131/sajg.123.0040.

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Abstract The volcanosedimentary Guperas Formation contains the youngest volcanic rocks of the Sinclair Supergroup in the Konkiep Terrane of southern Namibia. Precise U-Pb zircon microbeam dating shows that the Guperas Formation as mapped includes felsic volcanic rocks which belong to both the first (1.37 to 1.33 Ga) and the third (1.11 to 1.07 Ga) magmatic cycle of the Sinclair Supergroup. Volcanic rocks of the ‘true’ Guperas Formation are dated by three samples, with a combined age of 1108 ± 10 Ma. The sedimentary rocks mapped as Guperas Formation are also distinguished by two different detri

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40

Lamothe, Kelsey G., Paul F. Hoffman, J. Wilder Greenman, and Galen P. Halverson. "Stratigraphy and isotope geochemistry of the pre-Sturtian Ugab Subgroup, Otavi/Swakop Group, northwestern Namibia." Precambrian Research 332 (September 2019): 105387. http://dx.doi.org/10.1016/j.precamres.2019.105387.

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41

Porada, Hubertus. "Stratigraphy and facies in the upper proterozoic damara orogen, Namibia, based on a geodynamic model." Precambrian Research 29, no. 1-3 (1985): 235–64. http://dx.doi.org/10.1016/0301-9268(85)90070-1.

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42

SAYLOR, B., J. GROTZINGER, and G. GERMS. "Sequence stratigraphy and sedimentology of the Neoproterozoic Kuibis and Schwarzrand Subgroups (Nama Group), southwestern Namibia." Precambrian Research 73, no. 1-4 (1995): 153–71. http://dx.doi.org/10.1016/0301-9268(94)00076-4.

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43

Cairncross, Bruce. "The Where of Mineral Names: Skorpionite, Skorpion Mine, Lüderitz District, Karas Region, Namibia." Rocks & Minerals 93, no. 6 (2018): 562–67. http://dx.doi.org/10.1080/00357529.2018.1502593.

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44

Svendsen, Johan, Harald Stollhofen, Carmen B. E. Krapf, and Ian G. Stanistreet. "Mass and hyperconcentrated flow deposits record dune damming and catastrophic breakthrough of ephemeral rivers, Skeleton Coast Erg, Namibia." Sedimentary Geology 160, no. 1-3 (2003): 7–31. http://dx.doi.org/10.1016/s0037-0738(02)00334-2.

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45

Grab, Stefan, and Tizian Zumthurm. "“Everything is scorched by the burning sun”: missionary perspectives and experiences of 19th- and early 20th-century droughts in semi-arid central Namibia." Climate of the Past 16, no. 2 (2020): 679–97. http://dx.doi.org/10.5194/cp-16-679-2020.

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Abstract. Limited research has focussed on historical droughts during the pre-instrumental weather-recording period in semi-arid to arid human-inhabited environments. Here we describe the unique nature of droughts over semi-arid central Namibia (southern Africa) between 1850 and 1920. More particularly, our intention is to establish temporal shifts in influence and impact that historical droughts had on society and the environment during this period. This is achieved through scrutinizing documentary records sourced from a variety of archives and libraries. The primary source of information com

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46

JENSEN, S., and G. E. BUDD. "Introduction to thematic set of papers on the Ediacaran–Cambrian palaeoecology, sedimentology and stratigraphy of Namibia." Geological Magazine 142, no. 5 (2005): 463–64. http://dx.doi.org/10.1017/s0016756805001238.

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The Neoproterozoic was a time of profound biological and geological change. After a long time of verymodest changes in the flora and fauna, the Ediacaran period finally brought forward the first diverse microflora, the first diverse macrophytes, as well as the first diverse macroscopic organisms, some of which likely are animals. There were significant palaeogeographic changes, at least two, or probably three, pronounced levels of widely recorded glaciations, and extensive fluctuations in δ13 C. Much thought has recently been directed at understanding if, and how, several, or most, of these ev

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47

Riccomini, Claudio, Afonso C. R. Nogueira, and Alcides N. Sial. "Carbon and oxygen isotope geochemistry of Ediacaran outer platform carbonates, Paraguay Belt, central Brazil." Anais da Academia Brasileira de Ciências 79, no. 3 (2007): 519–27. http://dx.doi.org/10.1590/s0001-37652007000300012.

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After the late Cryogenian glaciation the central region of Brazil was the site of extensive deposition of platformal carbonates of the Araras Group. This group includes a basal cap carbonate sequence succeeded by transgressive, deep platform deposits of bituminous lime mudstone and shale. Facies and stratigraphic data combined with carbon and oxygen isotopic analyses of the most complete section of the transgressive deposits, exposed in the Guia syncline, were used to evaluate the depositional paleoenvironment and to test the correlation of these deposits along the belt and with other units wo

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48

Saylor, B. Z. "Sequence Stratigraphy and Carbonate-Siliciclastic Mixing in a Terminal Proterozoic Foreland Basin, Urusis Formation, Nama Group, Namibia." Journal of Sedimentary Research 73, no. 2 (2003): 264–79. http://dx.doi.org/10.1306/082602730264.

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49

Kamona, A. F., and A. Günzel. "Stratigraphy and base metal mineralization in the Otavi Mountain Land, Northern Namibia—a review and regional interpretation." Gondwana Research 11, no. 3 (2007): 396–413. http://dx.doi.org/10.1016/j.gr.2006.04.014.

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50

Maslanyj, M. P., M. P. R. Light, R. J. Greenwood, and N. L. Banks. "Extension tectonics offshore Namibia and evidence for passive rifting in the South Atlantic." Marine and Petroleum Geology 9, no. 6 (1992): 590–601. http://dx.doi.org/10.1016/0264-8172(92)90032-a.

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