Vol. 9 | 2006

Petroleum geochemistry of the deepened Lopra-1/1A re-entry well, Faroe Islands

RESEARCH ARTICLE
Published May 31, 2006
Jørgen A Bojesen-Koefoed
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H Peter Nytoft
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RESEARCH ARTICLE
Published May 31, 2006
A spectral graph.
Abstract
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Keywords

oil traces, organic geochemistry, contamination, Faroes, North Atlantic, Lopra

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GEUS Bulletin is an open-access, peer-reviewed journal published by the Geological Survey of Denmark and Greenland (GEUS). This article is distributed under a CC-BY 4.0 licence, permitting free redistribution and reproduction for any purpose, even commercial, provided proper citation of the original work. Author(s) retain copyright over the article contents. Read the full open access policy.

Abstract

The Lopra-1/1A re-entry well was drilled as a stratigraphic test with no immediate exploration objectives. Hence, petroleum geochemical studies were of limited extent, and restricted to non-destructive analyses. The presence of natural petroleum hydrocarbons could not be confirmed with certainty, but hydrocarbons extracted from the hydrochloric acid solute of a calcite vug present in RSWC #1 (3543 m), may represent indigenous petroleum since hydrocarbon-bearing fluid inclusions have been reported from the same sample. These hydrocarbons show some similarities to petroleum generated from the Upper Jurassic – Lower Cretaceous Kimmeridge Clay type source rocks present in surrounding areas. Except for this sample, the results generally show the presence of a variety of contaminants of different origins such as ‘naturally greasy fingers’ (squalene and cholesterol), cosmetics such as chap stick or hand lotion (e.g. esters such as butyl-stearate, stearyl-palmitate, vitamin A), plasticisers (phthalates), diesel oil and ‘pipe dope’.

Keywords

oil traces, organic geochemistry, contamination, Faroes, North Atlantic, Lopra

License Creative Commons License

This work is licensed under a Creative Commons Attribution 4.0 International License.

GEUS Bulletin is an open-access, peer-reviewed journal published by the Geological Survey of Denmark and Greenland (GEUS). This article is distributed under a CC-BY 4.0 licence, permitting free redistribution and reproduction for any purpose, even commercial, provided proper citation of the original work. Author(s) retain copyright over the article contents. Read the full open access policy.

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Editors: James A. Chalmers and Regin Waagstein

The Faroe Islands in the northern North Altantic consist primarily of Palaeogene eruptive volcanic rocks. Two research boreholes were drilled in 1980 and 1981 on the islands, the deeper of which, Lopra-1, extended 2 km into the unexposed part of the volcanic succession.

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