The control of shear‐zone development and electric conductivity by graphite in granulite: An example from the Proterozoic Lofoten‐Vesterålen Complex of northern Norway
Abstract Graphite impacts crustal rheology and electric conductivity in the lower crust. In a combined geophysical and geological study from the Proterozoic Lofoten‐Vesterålen Complex, Norway, we show the enrichment of graphite resulted in zones with strong schistosity and a sharp strain gradient to...
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crwiley:10.1111/ter.12545 2024-09-15T18:17:54+00:00 The control of shear‐zone development and electric conductivity by graphite in granulite: An example from the Proterozoic Lofoten‐Vesterålen Complex of northern Norway Engvik, Ane K. Gautneb, Håvard Baranwal, Vikas C. Rønning, Jan‐Steinar Knežević Solberg, Janja Liu, Yunhe Austrheim, Håkon Norges Geologiske Undersøkelse 2021 http://dx.doi.org/10.1111/ter.12545 https://onlinelibrary.wiley.com/doi/pdf/10.1111/ter.12545 https://onlinelibrary.wiley.com/doi/full-xml/10.1111/ter.12545 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Terra Nova volume 33, issue 5, page 529-539 ISSN 0954-4879 1365-3121 journal-article 2021 crwiley https://doi.org/10.1111/ter.12545 2024-07-25T04:22:37Z Abstract Graphite impacts crustal rheology and electric conductivity in the lower crust. In a combined geophysical and geological study from the Proterozoic Lofoten‐Vesterålen Complex, Norway, we show the enrichment of graphite resulted in zones with strong schistosity and a sharp strain gradient towards host massive granulite gneiss. Increased graphite content resulted in high‐conductivity zones with true resistivity values <10 Ωm compared with a resistivity of >3,000 Ωm in the low‐conductive crust. The regionally distributed graphite zones contain up to 39% graphite with variable amounts of quartz, feldspars, biotite and pyroxenes and where graphite is present in stable assemblage to orthopyroxene. High‐ordered graphite and biotite with a strong‐preferred orientation define the well‐developed foliation. Our results demonstrate that graphite accounts for the high electric conductivity of this former Proterozoic lower‐crustal segment. The presence of graphite causes strain localisation in the granulite facies crust, reducing crustal strength and may thereby influence continental architecture and evolution of collision zones. Article in Journal/Newspaper Lofoten Northern Norway Vesterålen Wiley Online Library Terra Nova |
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Wiley Online Library |
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English |
description |
Abstract Graphite impacts crustal rheology and electric conductivity in the lower crust. In a combined geophysical and geological study from the Proterozoic Lofoten‐Vesterålen Complex, Norway, we show the enrichment of graphite resulted in zones with strong schistosity and a sharp strain gradient towards host massive granulite gneiss. Increased graphite content resulted in high‐conductivity zones with true resistivity values <10 Ωm compared with a resistivity of >3,000 Ωm in the low‐conductive crust. The regionally distributed graphite zones contain up to 39% graphite with variable amounts of quartz, feldspars, biotite and pyroxenes and where graphite is present in stable assemblage to orthopyroxene. High‐ordered graphite and biotite with a strong‐preferred orientation define the well‐developed foliation. Our results demonstrate that graphite accounts for the high electric conductivity of this former Proterozoic lower‐crustal segment. The presence of graphite causes strain localisation in the granulite facies crust, reducing crustal strength and may thereby influence continental architecture and evolution of collision zones. |
author2 |
Norges Geologiske Undersøkelse |
format |
Article in Journal/Newspaper |
author |
Engvik, Ane K. Gautneb, Håvard Baranwal, Vikas C. Rønning, Jan‐Steinar Knežević Solberg, Janja Liu, Yunhe Austrheim, Håkon |
spellingShingle |
Engvik, Ane K. Gautneb, Håvard Baranwal, Vikas C. Rønning, Jan‐Steinar Knežević Solberg, Janja Liu, Yunhe Austrheim, Håkon The control of shear‐zone development and electric conductivity by graphite in granulite: An example from the Proterozoic Lofoten‐Vesterålen Complex of northern Norway |
author_facet |
Engvik, Ane K. Gautneb, Håvard Baranwal, Vikas C. Rønning, Jan‐Steinar Knežević Solberg, Janja Liu, Yunhe Austrheim, Håkon |
author_sort |
Engvik, Ane K. |
title |
The control of shear‐zone development and electric conductivity by graphite in granulite: An example from the Proterozoic Lofoten‐Vesterålen Complex of northern Norway |
title_short |
The control of shear‐zone development and electric conductivity by graphite in granulite: An example from the Proterozoic Lofoten‐Vesterålen Complex of northern Norway |
title_full |
The control of shear‐zone development and electric conductivity by graphite in granulite: An example from the Proterozoic Lofoten‐Vesterålen Complex of northern Norway |
title_fullStr |
The control of shear‐zone development and electric conductivity by graphite in granulite: An example from the Proterozoic Lofoten‐Vesterålen Complex of northern Norway |
title_full_unstemmed |
The control of shear‐zone development and electric conductivity by graphite in granulite: An example from the Proterozoic Lofoten‐Vesterålen Complex of northern Norway |
title_sort |
control of shear‐zone development and electric conductivity by graphite in granulite: an example from the proterozoic lofoten‐vesterålen complex of northern norway |
publisher |
Wiley |
publishDate |
2021 |
url |
http://dx.doi.org/10.1111/ter.12545 https://onlinelibrary.wiley.com/doi/pdf/10.1111/ter.12545 https://onlinelibrary.wiley.com/doi/full-xml/10.1111/ter.12545 |
genre |
Lofoten Northern Norway Vesterålen |
genre_facet |
Lofoten Northern Norway Vesterålen |
op_source |
Terra Nova volume 33, issue 5, page 529-539 ISSN 0954-4879 1365-3121 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/ter.12545 |
container_title |
Terra Nova |
_version_ |
1810456028632842240 |