E.D. Dempsey
A revised age, structural model and origin for the North Pennine Orefield in the Alston Block, northern England: intrusion (Whin Sill)-related base metal (Cu–Pb–Zn–F) mineralization
Dempsey, E.D.; Holdsworth, R.E.; Selby, D.; Bird, A.; Young, B.; Le Cornu, C.
Authors
Professor Bob Holdsworth r.e.holdsworth@durham.ac.uk
Professor
Professor David Selby phdjpop@durham.ac.uk
Professor
A. Bird
B. Young
C. Le Cornu
Abstract
Mineralization and associated fluid migration events in the c. 1500 km2 North Pennine Orefield (NPO) are known to be associated with tectonic activity, but the age of these tectonic events and origins of the base metal sulfide mineralization remain unresolved. New fieldwork in the Alston Block shows that mineralization post-dates a weakly developed phase of north–south shortening consistent with far-field Variscan basin inversion during the late Carboniferous. New observations of field relationships, coupled with microstructural observations and stress inversion analyses, together with Re–Os sulfide geochronology show that the vein-hosted mineralization (apart from barium minerals) was synchronous with a phase of north–south extension and east–west shortening coeval with emplacement of the Whin Sill (c. 297–294 Ma). Thus the development of the NPO was related to an early Permian regional phase of transtensional deformation, mantle-sourced hydrothermal mineralization and magmatism in northern Britain. Previously proposed Mississippi Valley Type models, or alternatives relating mineralization to the influx of Mesozoic brines, can no longer be applied to the development of the NPO in the Alston Block. Our findings also mean that existing models for equivalent base metal sulfide fields worldwide (e.g. Zn–Pb districts of Silesia, Poland and Tennessee, USA) may need to be reassessed.
Citation
Dempsey, E., Holdsworth, R., Selby, D., Bird, A., Young, B., & Le Cornu, C. (2021). A revised age, structural model and origin for the North Pennine Orefield in the Alston Block, northern England: intrusion (Whin Sill)-related base metal (Cu–Pb–Zn–F) mineralization. Journal of the Geological Society, 178(4), jgs2020-226. https://doi.org/10.1144/jgs2020-226
Journal Article Type | Article |
---|---|
Acceptance Date | Jan 26, 2021 |
Online Publication Date | Mar 11, 2021 |
Publication Date | 2021-07 |
Deposit Date | Apr 30, 2021 |
Publicly Available Date | Apr 30, 2021 |
Journal | Journal of the Geological Society |
Print ISSN | 0016-7649 |
Electronic ISSN | 2041-479X |
Publisher | The Geological Society |
Peer Reviewed | Peer Reviewed |
Volume | 178 |
Issue | 4 |
Pages | jgs2020-226 |
DOI | https://doi.org/10.1144/jgs2020-226 |
Public URL | https://durham-repository.worktribe.com/output/1276313 |
Files
Published Journal Article
(19.3 Mb)
PDF
You might also like
Intraplate Strike-Slip Deformation Belts.
(2003)
Book
Continental Reactivation and Reworking.
(2001)
Book
Downloadable Citations
About Durham Research Online (DRO)
Administrator e-mail: dro.admin@durham.ac.uk
This application uses the following open-source libraries:
SheetJS Community Edition
Apache License Version 2.0 (http://www.apache.org/licenses/)
PDF.js
Apache License Version 2.0 (http://www.apache.org/licenses/)
Font Awesome
SIL OFL 1.1 (http://scripts.sil.org/OFL)
MIT License (http://opensource.org/licenses/mit-license.html)
CC BY 3.0 ( http://creativecommons.org/licenses/by/3.0/)
Powered by Worktribe © 2024
Advanced Search