Egs-Relevant Review Of Metallogenesis, Chpm2030 Deliverable D1.1

In the provisioned CHPM technology an enhanced geothermal system would be established on a deep metal-bearing geological formation, which would be conducted in a way that the co-production of energy and metals could be possible. The aim of this study is to provide a metallogenic background for the p...

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Main Authors: Hartai, Éva, Németh, Norbert, Földessy, János
Format: Text
Language:English
Published: Zenodo 2016
Subjects:
EGS
Online Access:https://dx.doi.org/10.5281/zenodo.1204359
https://zenodo.org/record/1204359
id ftdatacite:10.5281/zenodo.1204359
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spelling ftdatacite:10.5281/zenodo.1204359 2023-05-15T16:12:59+02:00 Egs-Relevant Review Of Metallogenesis, Chpm2030 Deliverable D1.1 Hartai, Éva Németh, Norbert Földessy, János 2016 https://dx.doi.org/10.5281/zenodo.1204359 https://zenodo.org/record/1204359 en eng Zenodo https://dx.doi.org/10.5281/zenodo.1204360 Open Access info:eu-repo/semantics/openAccess geothermal energy geochemistry europe metallogenesis EGS production Text Project deliverable article-journal ScholarlyArticle 2016 ftdatacite https://doi.org/10.5281/zenodo.1204359 https://doi.org/10.5281/zenodo.1204360 2021-11-05T12:55:41Z In the provisioned CHPM technology an enhanced geothermal system would be established on a deep metal-bearing geological formation, which would be conducted in a way that the co-production of energy and metals could be possible. The aim of this study is to provide a metallogenic background for the potential development of this technology. In the document the ore formation processes and the metallogenic provinces of Europe are reviewed, considering the relevancy with the EGS application, in order to identify the possible zones where the CHPM technology can be applied. As the distribution of metallogenic provinces strongly correlates with the tectonic setting, four large metallogenic provinces can be identified within Europe: (1) Precambrian Fennoscandian Shield province, (2) Early Paleozoic Caledonian province, (3) Late Paleozoic Variscan province, (4) Mesozoic-Cenozoic Alpine province. The prospective zones or formations for the CHPM technology are assessed in each metallogenic province. Additionally to the mineralised intrusive bodies, thick sedimentary successions in extensional structures and deep-rooted regional fault zones can be also target areas both for the elevated heat flow and mineralisation potential from deep, fertile zones. : H2020 Text Fennoscandian DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic geothermal energy
geochemistry
europe
metallogenesis
EGS
production
spellingShingle geothermal energy
geochemistry
europe
metallogenesis
EGS
production
Hartai, Éva
Németh, Norbert
Földessy, János
Egs-Relevant Review Of Metallogenesis, Chpm2030 Deliverable D1.1
topic_facet geothermal energy
geochemistry
europe
metallogenesis
EGS
production
description In the provisioned CHPM technology an enhanced geothermal system would be established on a deep metal-bearing geological formation, which would be conducted in a way that the co-production of energy and metals could be possible. The aim of this study is to provide a metallogenic background for the potential development of this technology. In the document the ore formation processes and the metallogenic provinces of Europe are reviewed, considering the relevancy with the EGS application, in order to identify the possible zones where the CHPM technology can be applied. As the distribution of metallogenic provinces strongly correlates with the tectonic setting, four large metallogenic provinces can be identified within Europe: (1) Precambrian Fennoscandian Shield province, (2) Early Paleozoic Caledonian province, (3) Late Paleozoic Variscan province, (4) Mesozoic-Cenozoic Alpine province. The prospective zones or formations for the CHPM technology are assessed in each metallogenic province. Additionally to the mineralised intrusive bodies, thick sedimentary successions in extensional structures and deep-rooted regional fault zones can be also target areas both for the elevated heat flow and mineralisation potential from deep, fertile zones. : H2020
format Text
author Hartai, Éva
Németh, Norbert
Földessy, János
author_facet Hartai, Éva
Németh, Norbert
Földessy, János
author_sort Hartai, Éva
title Egs-Relevant Review Of Metallogenesis, Chpm2030 Deliverable D1.1
title_short Egs-Relevant Review Of Metallogenesis, Chpm2030 Deliverable D1.1
title_full Egs-Relevant Review Of Metallogenesis, Chpm2030 Deliverable D1.1
title_fullStr Egs-Relevant Review Of Metallogenesis, Chpm2030 Deliverable D1.1
title_full_unstemmed Egs-Relevant Review Of Metallogenesis, Chpm2030 Deliverable D1.1
title_sort egs-relevant review of metallogenesis, chpm2030 deliverable d1.1
publisher Zenodo
publishDate 2016
url https://dx.doi.org/10.5281/zenodo.1204359
https://zenodo.org/record/1204359
genre Fennoscandian
genre_facet Fennoscandian
op_relation https://dx.doi.org/10.5281/zenodo.1204360
op_rights Open Access
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.5281/zenodo.1204359
https://doi.org/10.5281/zenodo.1204360
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