1 edition of Nagssugtoqidian geology found in the catalog.
|Statement||edited by J.A. Korstgård.|
|Series||Rapport / Grønlands geologiske undersøgelse,, nr. 89, Publication / Department of Geology, Aarhus University ;, no. 280, Rapport (Grønlands geologiske undersøgelse) ;, nr. 89., Publication (Aarhus universitet. Geologisk institut) ;, no. 280.|
|Contributions||Korstgård, J. A., Aarhus universitet. Geologisk institut. Agto Group.|
|LC Classifications||QE70 .D43 nr. 89|
|The Physical Object|
|Pagination||146 p. :|
|Number of Pages||146|
|LC Control Number||81177661|
The published accounts of the structural geology and tectonic evolution of the Early Proterozoic Nagssugtoqidian orogen, SW Greenland, require modification in several fundamental respects. The geometry of the orogen has been attributed to important displacements on major conjugate shear zones and thrust by: The Observers Book of British Geology - Book No 10 Describing the Principal Rocks, Minerals and Fossils by I.O. Evans and a great selection of related books, art and collectibles available now at
Open Library is an open, editable library catalog, building towards a web page for every book ever published. Economic mineral deposits by Alan Mara Bateman, , J. Cited by: Regional structural geology. The Nagssugtoqidian Orogen in South-East Greenland was formerly known as the Nagssugtoqidian, Ammassalik or Angmagssalik Mobile Belt, because the link between the Palaeoproterozoic orogens of west and east Greenland, which are separated by Inland Ice, has been a matter of discussion for decades (Wright et al., Cited by:
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The Nagssugtoqidian orogeny was a late Paleoproterozoic mountain-building event that affected Greenland during the period to Ga. The orogenic belt formed during this event marks the northern boundary of the mainly Archaean North Atlantic was first recognised by Ramberg inbased on its effect on the Kangaamiut dike subsequent.
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The Laxfordian orogeny was an orogeny mountain building event between and 1 billion years ago. It primarily affected the North Atlantic Craton, in particular a section that cleaved off during the Mesozoic as the Scottish Shield Fragment.
The event produced deformation and high-grade metamorphism, migmatite formation and the emplacement granite and pegmatite in the Loch. A regional or social variety of a language distinguished by pronunciation, grammar, or vocabulary, especially a variety of speech differing Nagssugtoqidian geology book the standard literary language or speech pattern of the culture in which it exists: Cockney is a dialect of English.
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The format of the citations is: Author. Of the geology of Greenland / A. Escher and W.S. Watt -- Archaean gneiss complex of Greenland / D. Bridgwater [and others] -- Nagussugtoqidian mobile belt in West Greenland / A. Escher, K.
Sørensen and H.P. Zeck -- Nagssugtoqidian mobile belt in East Greenland / D. Bridgwater -- Rinkian mobile belt of West Greenland / A.
Escher and T.C.R. Pulvertaft -- Ketilidian mobile. Precambrian geology of the northern Nagssugtoqidian orogen,West Greenland: mapping in the Kangaatsiaq area Article (PDF Available) January with 72 Reads How we measure 'reads'.
The mountains and fjords of Greenland preserve a record of nearly four billion years of Earth history - a story of mountain building, volcanic eruptions, primitive life and ice ages. During the vast period of time, through processes of continental drift, Greenland has journeyed from the southern hemisphere through the tropics to its present polar position.
The published accounts of the structural geology and tectonic evolution of the Early Proterozoic Nagssugtoqidian orogen, SW Greenland, require modification in several fundamental : Soumyajit Mukherjee.
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The ability of a rock to conduct electrical current or sound waves is several steps removed from traditional outcrop descriptions based on the eye and hammer. The dramatic, austere west coast of Greenland is the setting of A Wilder Time: Notes From a Geologist at the Edge of the Greenland Ice by William E.
Glassley. Fresh from a divorce, looking forward Author: Paul Weideman. Laurentian margin evolution and the Caledonian orogeny—A template for Scotland and East Greenland Author(s) Elements of the geology of the Northern and Grampian Highlands of Scotland may be compared with similar sequences in the Niggli Spids thrust the Nagssugtoqidian of Greenland, and the Lapland-Kola belt of Scandinavia.
The Nagssugtoqidian orogeny of West Greenland mainly occurred between and Ga , as a consequence of the convergence and collision of the North Atlantic Craton and a poorly defined craton to the north .The Palaeoproterozoic reworking during the orogeny extends from Kangerlussuaq to southern Disko Bugt [3,4,5].Several studies have been performed in the Cited by: 9.
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