East Greenland Caledonian fold belt

Niels Henriksen; A.K. Higgins

doi:10.22008/gpub/38214

East Greenland Caledonian fold belt

Niels Henriksen
, A.K. Higgins

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

Abstract

The East Greenland fold belt is part of a major Caledonian structure which occurs on both sides of the North Atlantic Ocean (fig. 172). It extends from latitudes 70° to 82° N in East Greenland (fig. 173), occupying most of the wide strip of land between the coast and the Inland Ice.

Original language	English
Title of host publication	Geology of Greenland
Editors	Arthur Escher, W. Stuart Watt
Place of Publication	Copenhagen
Publisher	GGU
Pages	182-246
Number of pages	65
ISBN (Print)	87-980404-0-5
DOIs	https://doi.org/10.22008/gpub/38214
Publication status	Published - 31 Dec 1976

Keywords

Greenland

Programme Area

Programme Area 4: Mineral Resources

Access to Document

10.22008/gpub/38214Licence: Unspecified

https://data.geus.dk/pure-pdf/38214_GoG_8_Henriksen_Higgins_East_Greenland_Caledonian_fold_belt_ocr.pdfLicence: Unspecified

Cite this

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title = "East Greenland Caledonian fold belt",

abstract = "The East Greenland fold belt is part of a major Caledonian structure which occurs on both sides of the North Atlantic Ocean (fig. 172). It extends from latitudes 70° to 82° N in East Greenland (fig. 173), occupying most of the wide strip of land between the coast and the Inland Ice. ",

keywords = "Greenland, Greenland",

author = "Niels Henriksen and A.K. Higgins",

year = "1976",

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TY - CHAP

T1 - East Greenland Caledonian fold belt

AU - Henriksen, Niels

AU - Higgins, A.K.

PY - 1976/12/31

Y1 - 1976/12/31

N2 - The East Greenland fold belt is part of a major Caledonian structure which occurs on both sides of the North Atlantic Ocean (fig. 172). It extends from latitudes 70° to 82° N in East Greenland (fig. 173), occupying most of the wide strip of land between the coast and the Inland Ice.

AB - The East Greenland fold belt is part of a major Caledonian structure which occurs on both sides of the North Atlantic Ocean (fig. 172). It extends from latitudes 70° to 82° N in East Greenland (fig. 173), occupying most of the wide strip of land between the coast and the Inland Ice.

KW - Greenland

U2 - 10.22008/gpub/38214

DO - 10.22008/gpub/38214

M3 - Chapter in book

SN - 87-980404-0-5

SP - 182

EP - 246

BT - Geology of Greenland

A2 - Escher, Arthur

A2 - Watt, W. Stuart

PB - GGU

CY - Copenhagen

ER -

East Greenland Caledonian fold belt

Abstract

Keywords

Programme Area

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Cite this