3 edition of Lower Proterozoic Marmorilik Formation, East of Mârmorilik, West Greenland found in the catalog.
Lower Proterozoic Marmorilik Formation, East of Mârmorilik, West Greenland
Adam A. Garde
|Other titles||Mârmorilik, West Greenland.|
|Statement||by Adam A. Garde.|
|Series||Meddelelser om Grønland ;, bd. 200, nr. 3, Meddelelser om Grønland ;, bd. 200, nr. 3.|
|LC Classifications||Q115 .D39 bd. 200, Nr. 3, QE653 .D39 bd. 200, Nr. 3|
|The Physical Object|
|Pagination||71 p., 7 leaves of plates :|
|Number of Pages||71|
|LC Control Number||81464376|
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Additional Physical Format: Online version: Garde, Adam A. Lower Proterozoic Marmorilik Formation, East of Mârmorilik, West Greenland. København: Nyt Nordisk Forlag, The Marmorilik Formation, Rinkian mobile belt, West Greenland, is a large, Lower Proterozoic carbonate-rock sequence, deformed and metamorphosed under greenschist to amphibolite facies conditions.
The pre-deformation thickness of the sequence is at least m, with about m of dolomite marble and m of calcite by: 5. The Lower Proterozoic Maarmorilik Formation east of Mârmorilik, West Greenland A.A.
& Pulvertaft, T.C.R. Age relations of the Precambrian Mârmorilik marble Formation, central West Greenland. Geological Survey of Greenland Report, Relationships between the Precambrian metasediments of the Marmorilik Formation and the Karrat Cited by: The area lies between the Proterozoic Nagssugtoqidian and Rinkian mobile belts of West Greenland, which are thus separated by an area of Archaean rocks little affected by mid-Proterozoic tectono.
Garde, A. A., Strontium geochemistry and carbon and oxygen isotopic compositions of lower Proterozoic dolomite and calcite marbles from the Marmorilik Formation, West Greenland, Precambrian Res., 8, –, [C, O; no data table]Cited by: World / Greenland / Uummannaq / Maarmorilik World / Greenland / Kitaa Marmorilik, also Maarmorilik, "the location of marble", an old mine which is suppose to be opend again in.
Garde A A () The lower-Proterozoic Marmorilik Formation east of Marmorilik, West Greenland. Meddr Grønland (3) Gill E J () Experimental deformation and annealing of sulfides and interpretation of ore textures.
Econ Geol – Mobile Belt, trending as an east-west belt ac ross North-West Greenland, is a likely proximal Palaeoproterozoic detrital source that is compatible with the NE directed palaeocurrents. The northernmost occurrence of proven Archaean rocks in East Greenland is at Danmarkshavn (6 in Fig.
1) where Steiger et al. () obtained U--Pb zircon and Rb--Sr whole-rock ages of ca. 8teiger et al. (} did not find evidence of strong Proterozoic metamorphism at. The constraints on the geological history of the Marmorilik Formation marbles are that they were deposited prior to regional metamorphism dated at 50 Ma (Kalsbeek et al., ), and that an upper limit to the depositional age is set by the unconformable relationship of the Marmorilik Formation to the Archaean gneisses and granites in the.
The flysch formation is up to 5 km thick and is the most prominent unit in an area km from north to south that is bounded by Greenland's Inland Ice to the east and Baffin Bay to the west. A similar supracrustal unit underlies extensive areas in the Foxe fold belt of north-eastern Canada.
Gold mineralisation at Eqi, north-east Disko Bugt, West Greenland, is hosted in Archaean (c. Ma old) supracrustal rocks; the latter are divided by a thrust into a lower volcanic unit and an. The Mârmorilik Formation is dominated by dolomite-rich marbles in the lower part and calcite-rich marbles in the upper part.
Locally, interbedded horizons of quartzites, tremolite-rich marbles and. Strontium geochemistry and carbon and oxygen isotopic compositions of lower proterozoic dolomite and calcite marbles from the Marmorilik Formation, West Greenland Adam A.
Garde Precambrian. Information about Port of Marmorilik (Greenland): port location, harbor characteristics, water depth, port services, restrictions etc. The Rae Craton has been inferred to have acted as a long standing upper plate onto which numerous other crustal fragments were emplaced during orogenic events throughout the Proterozoic (Hoffman, ).
One of these orogenic events spawned the Rinkian Fold Belt in West Greenland at c. Ga (Sanborn-Barrie et al., ). The Karrat Group. Discover Marmorilik, Vestgronland, Greenland with the help of your friends. Search for restaurants, hotels, museums and more. The stratabound massive Fe-Zn-Pb-sulfide orebodies of the Black Angel mine, central West Greenland, occur in evaporite-bearing marbles in the upper part of the lower Proterozoic Marmorilik Formation.
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