Skip to main navigation Skip to search Skip to main content

Franklinian Composite Tectono-Sedimentary Element, North Greenland

Research output: Chapter in Book/Report/Conference proceedingChapter in bookResearchpeer-review

3 Citations (Scopus)

Abstract

The Franklinian Composite Tectono-Sedimentary Element (CTSE) in North Greenland is dominated by Neoproterozoic–lowermost Devonian sedimentary strata and includes early synrift through to passive-margin TSEs of mixed carbonate and siliciclastic facies. The sedimentary successions are well exposed in much of northern Greenland, but in parts were strongly affected by the Ellesmerian Orogeny, resulting in a fold and thrust belt that deformed the northernmost exposures. An exposed palaeo-oilfield attests to the petroleum potential of the basin. Several formations have good source potential and several others have good reservoir properties. Palaeoheat-flow indicators show that temperatures increase to the north, where much of the basin is over-mature. Because of the remoteness of the area and the restricted locations where there is likely to remain petroleum potential, the basin is not currently a target for exploration.

Original languageEnglish
Title of host publicationSedimentary successions of the Arctic region and their hydrocarbon prospectivity
EditorsS.S. Drachev, H. Brekke, E. Henriksen, T. Moore
PublisherGeological Society of London
Pages908-920
Number of pages13
Volume57
Edition1
DOIs
Publication statusPublished - 13 Nov 2025

Publication series

SeriesGeological Society, London, Memoirs
Volume57

Programme Area

  • Programme Area 3: Energy Resources

Fingerprint

Dive into the research topics of 'Franklinian Composite Tectono-Sedimentary Element, North Greenland'. Together they form a unique fingerprint.

Cite this