The pre-basaltic sediments and the Lower Basalts at Kangerdlugssuaq, East Greenland: their stratigraphy, lithology, palaeomagnetism and petrology
This paper presents a new 1:40 000 topographic and geological map of the area around Miki Fjord and l. C. Jacobsen Fjord, East Greenland. The post-Precambrian sedimentary succession, the Kangerdlugssuaq Group, begins with the Ryberg Formation (Campanian to Danian (?)) and continues into the Vandfald...
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The Commission for Scientific Research in Greenland /Danish Polar Center
1981
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ftkbcopenhojs:oai:ojs.tidsskrift.dk:article/141017 2024-01-28T10:05:27+01:00 The pre-basaltic sediments and the Lower Basalts at Kangerdlugssuaq, East Greenland: their stratigraphy, lithology, palaeomagnetism and petrology Nielsen, Troels F. D. Soper, N. J. Brooks, C. Kent Faller, Angela M. Higgins, Alan C. Matthews, David W. 1981-07-15 application/pdf https://tidsskrift.dk/meddrgroenland_geosci/article/view/141017 eng eng The Commission for Scientific Research in Greenland /Danish Polar Center https://tidsskrift.dk/meddrgroenland_geosci/article/view/141017/184920 https://tidsskrift.dk/meddrgroenland_geosci/article/view/141017 Meddelelser om Grønland. Geoscience; Vol. 6 (1981): Meddelelser om Grønland. Geoscience; 25 pp. Meddelelser om Grønland. Geoscience; Årg. 6 (1981); 25 pp. 1600-4590 0106-1046 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 1981 ftkbcopenhojs 2024-01-03T23:58:29Z This paper presents a new 1:40 000 topographic and geological map of the area around Miki Fjord and l. C. Jacobsen Fjord, East Greenland. The post-Precambrian sedimentary succession, the Kangerdlugssuaq Group, begins with the Ryberg Formation (Campanian to Danian (?)) and continues into the Vandfaldsdalen Formation of Late Paleocene age. These sediments were laid down in a basin which subsequently became filled and covered by basaltic rocks of the Blosseville Group, including lavas, hyaloclastites, tuffs and breccias. Considerable facies variations are apparent in both the sediments and volcanics indicating that the basin deepened in an easterly direction. Palaeomagnetic measurements confirm previous results for the Blosseville Group on the Lower Basalts but do not yet entirely eliminate the possibility that some of the succession has normal polarity. Petrographically the volcanics include picrites (oceanites and ankaramites), olivine tholeiites, tholeiites and tholeiitic andesites. They have almost all suffered alteration up to greenschist facies and some show evidence of sedimentary contamination. They are all of tholeiitic affinity and are Fe and Ti enriched when compared to normal ocean ridge basalts. They are however much more variable in composition than the overlying Plateau Basalts and have not been produced in such large volumes. It is suggested that a primary picritic magma gave rise to the oceanites and ankaramites by olivine and clinopyroxene fractionation and accumulation. The olivine tholeiites, which appear to be separated from the picrites by a compositional gap, may be derived from a different parental magma. Petrological parallels are drawn with other provinces. This paper presents a new 1:40 000 topographic and geological map of the area around Miki Fjord and l. C. Jacobsen Fjord, East Greenland. The post-Precambrian sedimentary succession, the Kangerdlugssuaq Group, begins with the Ryberg Formation (Campanian to Danian (?)) and continues into the Vandfaldsdalen Formation of Late Paleocene ... Article in Journal/Newspaper East Greenland Greenland Tidsskrift.dk (The Royal Library, Denmark) Greenland Miki Fjord ENVELOPE(-31.499,-31.499,68.149,68.149) Vandfaldsdalen ENVELOPE(-31.550,-31.550,68.183,68.183) |
institution |
Open Polar |
collection |
Tidsskrift.dk (The Royal Library, Denmark) |
op_collection_id |
ftkbcopenhojs |
language |
English |
description |
This paper presents a new 1:40 000 topographic and geological map of the area around Miki Fjord and l. C. Jacobsen Fjord, East Greenland. The post-Precambrian sedimentary succession, the Kangerdlugssuaq Group, begins with the Ryberg Formation (Campanian to Danian (?)) and continues into the Vandfaldsdalen Formation of Late Paleocene age. These sediments were laid down in a basin which subsequently became filled and covered by basaltic rocks of the Blosseville Group, including lavas, hyaloclastites, tuffs and breccias. Considerable facies variations are apparent in both the sediments and volcanics indicating that the basin deepened in an easterly direction. Palaeomagnetic measurements confirm previous results for the Blosseville Group on the Lower Basalts but do not yet entirely eliminate the possibility that some of the succession has normal polarity. Petrographically the volcanics include picrites (oceanites and ankaramites), olivine tholeiites, tholeiites and tholeiitic andesites. They have almost all suffered alteration up to greenschist facies and some show evidence of sedimentary contamination. They are all of tholeiitic affinity and are Fe and Ti enriched when compared to normal ocean ridge basalts. They are however much more variable in composition than the overlying Plateau Basalts and have not been produced in such large volumes. It is suggested that a primary picritic magma gave rise to the oceanites and ankaramites by olivine and clinopyroxene fractionation and accumulation. The olivine tholeiites, which appear to be separated from the picrites by a compositional gap, may be derived from a different parental magma. Petrological parallels are drawn with other provinces. This paper presents a new 1:40 000 topographic and geological map of the area around Miki Fjord and l. C. Jacobsen Fjord, East Greenland. The post-Precambrian sedimentary succession, the Kangerdlugssuaq Group, begins with the Ryberg Formation (Campanian to Danian (?)) and continues into the Vandfaldsdalen Formation of Late Paleocene ... |
format |
Article in Journal/Newspaper |
author |
Nielsen, Troels F. D. Soper, N. J. Brooks, C. Kent Faller, Angela M. Higgins, Alan C. Matthews, David W. |
spellingShingle |
Nielsen, Troels F. D. Soper, N. J. Brooks, C. Kent Faller, Angela M. Higgins, Alan C. Matthews, David W. The pre-basaltic sediments and the Lower Basalts at Kangerdlugssuaq, East Greenland: their stratigraphy, lithology, palaeomagnetism and petrology |
author_facet |
Nielsen, Troels F. D. Soper, N. J. Brooks, C. Kent Faller, Angela M. Higgins, Alan C. Matthews, David W. |
author_sort |
Nielsen, Troels F. D. |
title |
The pre-basaltic sediments and the Lower Basalts at Kangerdlugssuaq, East Greenland: their stratigraphy, lithology, palaeomagnetism and petrology |
title_short |
The pre-basaltic sediments and the Lower Basalts at Kangerdlugssuaq, East Greenland: their stratigraphy, lithology, palaeomagnetism and petrology |
title_full |
The pre-basaltic sediments and the Lower Basalts at Kangerdlugssuaq, East Greenland: their stratigraphy, lithology, palaeomagnetism and petrology |
title_fullStr |
The pre-basaltic sediments and the Lower Basalts at Kangerdlugssuaq, East Greenland: their stratigraphy, lithology, palaeomagnetism and petrology |
title_full_unstemmed |
The pre-basaltic sediments and the Lower Basalts at Kangerdlugssuaq, East Greenland: their stratigraphy, lithology, palaeomagnetism and petrology |
title_sort |
pre-basaltic sediments and the lower basalts at kangerdlugssuaq, east greenland: their stratigraphy, lithology, palaeomagnetism and petrology |
publisher |
The Commission for Scientific Research in Greenland /Danish Polar Center |
publishDate |
1981 |
url |
https://tidsskrift.dk/meddrgroenland_geosci/article/view/141017 |
long_lat |
ENVELOPE(-31.499,-31.499,68.149,68.149) ENVELOPE(-31.550,-31.550,68.183,68.183) |
geographic |
Greenland Miki Fjord Vandfaldsdalen |
geographic_facet |
Greenland Miki Fjord Vandfaldsdalen |
genre |
East Greenland Greenland |
genre_facet |
East Greenland Greenland |
op_source |
Meddelelser om Grønland. Geoscience; Vol. 6 (1981): Meddelelser om Grønland. Geoscience; 25 pp. Meddelelser om Grønland. Geoscience; Årg. 6 (1981); 25 pp. 1600-4590 0106-1046 |
op_relation |
https://tidsskrift.dk/meddrgroenland_geosci/article/view/141017/184920 https://tidsskrift.dk/meddrgroenland_geosci/article/view/141017 |
_version_ |
1789331751496056832 |