Ketilidian mobile belt in South Greenland

Jan H. Allaart

doi:10.22008/gpub/38212

Ketilidian mobile belt in South Greenland

Jan H. Allaart

Research output: Chapter in Book/Report/Conference proceeding › Chapter in book › Research

Abstract

The Ketilidian mobile belt occupies the region between lvigtut in the west, Ikermit in the east, and Kap Farvel, the southern tip of Greenland (fig. 138). To the north an extensive area of Archaean rocks is exposed (see Bridgwater et al., this volume). The mobile belt comprises gneisses, granites and metamorphosed supracrustal rocks and is characterised by the occurrence of numerous late, intrusive granite plutons covering large areas.

Original language	English
Title of host publication	Geology of Greenland
Editors	Arthur Escher, W. Stuart Watt
Place of Publication	Copenhagen
Publisher	GGU
Pages	120-151
Number of pages	32
ISBN (Print)	87-980404-0-5
DOIs	https://doi.org/10.22008/gpub/38212
Publication status	Published - 31 Dec 1976

Keywords

Greenland

Programme Area

Programme Area 4: Mineral Resources

Access to Document

10.22008/gpub/38212Licence: Unspecified

https://data.geus.dk/pure-pdf/38212_GoG_6_Allaart_Ketilidian_mobile_belt_in_South_Greenland_ocr.pdfLicence: Unspecified

Cite this

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title = "Ketilidian mobile belt in South Greenland",

abstract = "The Ketilidian mobile belt occupies the region between lvigtut in the west, Ikermit in the east, and Kap Farvel, the southern tip of Greenland (fig. 138). To the north an extensive area of Archaean rocks is exposed (see Bridgwater et al., this volume). The mobile belt comprises gneisses, granites and metamorphosed supracrustal rocks and is characterised by the occurrence of numerous late, intrusive granite plutons covering large areas.",

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AU - Allaart, Jan H.

PY - 1976/12/31

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N2 - The Ketilidian mobile belt occupies the region between lvigtut in the west, Ikermit in the east, and Kap Farvel, the southern tip of Greenland (fig. 138). To the north an extensive area of Archaean rocks is exposed (see Bridgwater et al., this volume). The mobile belt comprises gneisses, granites and metamorphosed supracrustal rocks and is characterised by the occurrence of numerous late, intrusive granite plutons covering large areas.

AB - The Ketilidian mobile belt occupies the region between lvigtut in the west, Ikermit in the east, and Kap Farvel, the southern tip of Greenland (fig. 138). To the north an extensive area of Archaean rocks is exposed (see Bridgwater et al., this volume). The mobile belt comprises gneisses, granites and metamorphosed supracrustal rocks and is characterised by the occurrence of numerous late, intrusive granite plutons covering large areas.

KW - Greenland

U2 - 10.22008/gpub/38212

DO - 10.22008/gpub/38212

M3 - Chapter in book

SN - 87-980404-0-5

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BT - Geology of Greenland

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A2 - Watt, W. Stuart

PB - GGU

CY - Copenhagen

ER -

Ketilidian mobile belt in South Greenland

Abstract

Keywords

Programme Area

Access to Document

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Cite this