Glaciation and the Quaternary of Greenland

Anker Weidick

doi:10.22008/gpub/38221

Glaciation and the Quaternary of Greenland

Anker Weidick

Publikation: Bidrag til bog/rapport/konferenceproceedings › Bogkapitel › Forskning

Resumé

The Tertiary deposits in Greenland are mainly of Paleogene age and are characterised by basalts, intercalated with limnic and marine sandstones and shales. The Neogene period is characterised by faulting and denudation processes which formed the major present landscape features of Greenland.

Originalsprog	Engelsk
Titel	Geology of Greenland
Redaktører	Arthur Escher, W. Stuart Watt
Udgivelsessted	Copenhagen
Forlag	GGU
Sider	430-458
Antal sider	29
ISBN (Trykt)	87-980404-0-5
DOI	https://doi.org/10.22008/gpub/38221
Status	Udgivet - 31 dec. 1976

Emneord

Greenland

Programområde

Programområde 4: Mineralske råstoffer

FN’s Verdensmål

Dette resultat bidrager til følgende verdensmål

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10.22008/gpub/38221Licens: Ikke-specificeret

https://data.geus.dk/pure-pdf/38221_GoG_15_Weidick_Glaciation_and_the_Quaternary_of_Greenland_ocr.pdfLicens: Ikke-specificeret

Citationsformater

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Glaciation and the Quaternary of Greenland

Resumé

Emneord

Programområde

FN’s Verdensmål

Adgang til dokumentet

Fingeraftryk

Citationsformater