Vol. 33 | 2015

Relationship between groundwater chemistry and the Precambrian basement rocks on eastern Bornholm, Denmark

RESEARCH ARTICLE | SHORT
Published July 7, 2015
Peter Gravesen
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Rasmus Jakobsen
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Bertel Nilsson
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RESEARCH ARTICLE | SHORT
Published July 7, 2015
Close up of rocks.
Abstract
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Keywords

Bornholm

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Copyright (c) 2015 Peter Gravesen, Rasmus Jakobsen, Bertel Nilsson

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.

Abstract

Bornholm is situated south of Sweden, in the Sorgenfrei–Tornquist Zone (Fig. 1). The Precambrian basement on northern and eastern Bornholm consists of different types of granitic and gneissic rocks with pegmatites, aplites and dolerite dykes (Callisen 1934). The age of the granite and gneiss is c. 1455 Ma (Waight et al. 2012).

Keywords

Bornholm

License

Copyright (c) 2015 Peter Gravesen, Rasmus Jakobsen, Bertel Nilsson

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 Ole Bennike, Adam A. Garde and W. Stuart Watt

This Review of Survey activities presents a selection of 20 papers reflecting the wide spectrum of activities of the Geological Survey of Denmark and Greenland, from the microscopic to the plate-tectonic level.

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