Zobrazeno 1 - 10
of 14
pro vyhledávání: '"H. C. Henderson"'
Autor:
Trond Slagstad, Evgeniy V. Kulakov, Mark W. Anderson, Kerstin Saalmann, Christopher L. Kirkland, Iain H. C. Henderson, Morgan Ganerød
Publikováno v:
Terra Nova. 35:167-173
Late Ediacaran opening of the Iapetus Ocean is typically considered to reflect separation of Baltica and Laurentia during final breakup of the Rodinia supercontinent, with subsequent closure during the Caledonian Orogeny. However, evidence of the pre
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fdd70d40679938a580e8bebb00ac1442
https://doi.org/10.1111/ter.12640
https://doi.org/10.1111/ter.12640
Autor:
A. Jarna, B. O. Grøtan, I. H. C. Henderson, S. Iversen, E. Khloussy, B. Nordahl, B. I. Rindstad
Publikováno v:
The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XLII-2/W2, Pp 115-121 (2016)
Geology and all geological structures are three-dimensional in space. GIS and databases are common tools used by geologists to interpret and communicate geological data. The NGU (Geological Survey of Norway) is the national institution for the study
Externí odkaz:
https://doaj.org/article/e9e50529ad8948b5a389020ab99b9d01
Publikováno v:
The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XL-2-W4, Pp 11-16 (2015)
Geology and all geological structures are three-dimensional in space. Geology can be easily shown as four-dimensional when time is considered. Therefore GIS, databases, and 3D visualization software are common tools used by geoscientists to view, ana
Externí odkaz:
https://doaj.org/article/5b85a36edf8c4d439cae422edf79bbb1
Publikováno v:
The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XL-2-W4, Pp 11-16 (2015)
Geology and all geological structures are three-dimensional in space. Geology can be easily shown as four-dimensional when time is considered. Therefore GIS, databases, and 3D visualization software are common tools used by geoscientists to view, ana
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b6d6d6edf7adc6ae7a0ebfe2e9e7b9cf
https://doi.org/10.5194/isprsarchives-xl-2-w4-11-2015
https://doi.org/10.5194/isprsarchives-xl-2-w4-11-2015
Autor:
B. O. Grøtan, B. Nordahl, S. Iversen, B. I. Rindstad, E. Khloussy, A. Jarna, I. H. C. Henderson
Publikováno v:
The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XLII-2/W2, Pp 115-121 (2016)
Geology and all geological structures are three-dimensional in space. GIS and databases are common tools used by geologists to interpret and communicate geological data. The NGU (Geological Survey of Norway) is the national institution for the study
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ceb751c341368d63761e03d16a7fd985
https://www.int-arch-photogramm-remote-sens-spatial-inf-sci.net/XLII-2-W2/115/2016/
https://www.int-arch-photogramm-remote-sens-spatial-inf-sci.net/XLII-2-W2/115/2016/
Publikováno v:
Journal of African Earth Sciences. 53:45-58
The Niassa Gold Belt, in northernmost Mozambique, is hosted in the Txitonga Group, a Neoproterozoic rift sequence overlying Paleoproterozoic crust of the Congo–Tanzania Craton and deformed during the Pan-African Orogeny. The Txitonga Group is made
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ae1766e428b49aa213bf9901317fd7f4
https://doi.org/10.1016/j.jafrearsci.2008.09.003
https://doi.org/10.1016/j.jafrearsci.2008.09.003
Autor:
Victor A. Melezhik, Bernard Bingen, D. Jamal, T. Bjerkgård, Arne Solli, Anthony E. Fallick, A. Moniz, A. B. Kuznetsov, I. H. C. Henderson, R. Boyd, J.S. Sandstad, Igor M. Gorokhov
Publikováno v:
Precambrian Research. 162:540-558
Marbles are minor but characteristic components of metasedimentary units within nappes in the Pan-African Mozambique Belt in NE Mozambique. Metasedimentary units remain largely undated, and carbon and strontium isotope stratigraphy of marbles has bee
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f09ea0a47f55f94597113baf551707dd
https://doi.org/10.1016/j.precamres.2007.11.002
https://doi.org/10.1016/j.precamres.2007.11.002
Autor:
A. C. Barnicoat, D. Strydom, Rob J. Knipe, N. P. C. Fox, S. R. Freeman, I. H. C. Henderson, A. Pather, M.T.G. Birch, S. J. Jolley, G.M. Phillips, T.W. Rowland
Publikováno v:
Journal of Structural Geology. 26:1067-1086
Structural controls on the distribution of gold in the Witwatersrand Basin can be seen at scales ranging from that of thin sections up to regional seismic data sets. At the thin section scale, gold occurs largely in fractures with hydrocarbons. These
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2e3fc08ab907772fcba82750d36617d2
https://doi.org/10.1016/j.jsg.2003.11.011
https://doi.org/10.1016/j.jsg.2003.11.011
Publikováno v:
Geological Society, London, Special Publications. 155:153-165
This paper examines the geometry and genesis of a mineralized thrust-related fracture system, developed at a major rheological interface between Witwatersrand sediments and Ventersdorp volcanics in the Witwatersrand Basin of South Africa. At the Elan
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d5d2c1e0bd4e131e595e1d0388f29109
https://doi.org/10.1144/gsl.sp.1999.155.01.12
https://doi.org/10.1144/gsl.sp.1999.155.01.12
Autor:
N. P. C. Fox, C. Cornford, R. W. Napier, S. R. Lawrence, K. S. Winkler, D. J. Muntingh, A. K. Kenyon, Bruce W. D. Yardley, Rob J. Knipe, A. C. Barnicoat, D. Strydom, I. H. C. Henderson
Publikováno v:
Nature. 386:820-824
The origin of the gold mineralization in the Witwaterstrand basin of South Africa—the largest known gold province—has been controversial for decades, with arguments favouring detrital1,2 (placer), modified placer3,4 and hydrothermal5,6 origins. H
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5fad0d05399224b23228ee0e91dc74e0
https://doi.org/10.1038/386820a0
https://doi.org/10.1038/386820a0