Mineralogy and Geochemistry of Ultramafic Rocks from Rachoni Magnesite Mine, Gerakini (Chalkidiki, Northern Greece)

The importance of magnesite for the EU economy and industry is very high, making the understanding of their genesis for the exploration for new deposits a priority for the raw materials scientific community. In this direction, the study of the magnesite-hosting ultramafic rocks can be proved very us...

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Main Authors: Evangelos Tzamos, Micol Bussolesi, Giovanni Grieco, Pietro Marescotti, Laura Crispini, Andreas Kasinos, Niccolò Storni, Konstantinos Simeonidis, Anastasios Zouboulis
Format: Article
Language:English
Published: MDPI AG 2020-10-01
Series:Minerals
Subjects:
Online Access:https://www.mdpi.com/2075-163X/10/11/934
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spelling doaj-5443d80fcb56454f84abecab4108a43c2020-11-25T03:56:33ZengMDPI AGMinerals2075-163X2020-10-011093493410.3390/min10110934Mineralogy and Geochemistry of Ultramafic Rocks from Rachoni Magnesite Mine, Gerakini (Chalkidiki, Northern Greece)Evangelos Tzamos0Micol Bussolesi1Giovanni Grieco2Pietro Marescotti3Laura Crispini4Andreas Kasinos5Niccolò Storni6Konstantinos Simeonidis7Anastasios Zouboulis8Department of Chemistry, Aristotle University of Thessaloniki, University Campus, 54124 Thessaloniki, GreeceDepartment of Earth Sciences, University of Milan, via S. Botticelli 23, 20133 Milan, ItalyDepartment of Earth Sciences, University of Milan, via S. Botticelli 23, 20133 Milan, ItalyDepartment for Earth, Environment and Life Sciences, University of Genova, C.so Europa, 26, 16132 Genova, ItalyDepartment for Earth, Environment and Life Sciences, University of Genova, C.so Europa, 26, 16132 Genova, ItalyGrecian Magnesite SA, Gerakini, 63100 Chalkidiki, GreeceDepartment of Earth Sciences, University of Milan, via S. Botticelli 23, 20133 Milan, ItalyEcoresources PC, Giannitson and Santarosa str., 15-17, 54627 Thessaloniki, GreeceDepartment of Chemistry, Aristotle University of Thessaloniki, University Campus, 54124 Thessaloniki, GreeceThe importance of magnesite for the EU economy and industry is very high, making the understanding of their genesis for the exploration for new deposits a priority for the raw materials scientific community. In this direction, the study of the magnesite-hosting ultramafic rocks can be proved very useful. For the present study, ultramafic rock samples were collected from the magnesite ore-hosting ophiolite of the Gerakini mining area (Chalkidiki, Greece) to investigate the consecutive alteration events of the rocks which led to the metallogenesis of the significant magnesite ores of the area. All samples were subjected to a series of analytical methods for the determination of their mineralogical and geochemical characteristics: optical microscopy, XRD, SEM, EMPA, ICP–MS/OES and CIPW normalization. The results of these analyses revealed that the ultramafic rocks of the area have not only all been subjected to serpentinization, but these rocks have also undergone carbonation, silification and clay alteration. The latter events are attributed to the circulation of CO<sub>2</sub>-rich fluids responsible for the formation of the magnesite ores and locally, the further alteration of the serpentinites into listvenites. The current mineralogy of these rocks was found to be linked to one or more alteration event that took place, thus a significant contribution to the metallo- and petrogenetic history of the Gerakini ophiolite has been made. Furthermore, for the first time in literature, Fe inclusions in olivines from Greece were reported.https://www.mdpi.com/2075-163X/10/11/934ophiolitesultramaficserpentinizationlistvenitesGerakinimagnesite ore
collection DOAJ
language English
format Article
sources DOAJ
author Evangelos Tzamos
Micol Bussolesi
Giovanni Grieco
Pietro Marescotti
Laura Crispini
Andreas Kasinos
Niccolò Storni
Konstantinos Simeonidis
Anastasios Zouboulis
spellingShingle Evangelos Tzamos
Micol Bussolesi
Giovanni Grieco
Pietro Marescotti
Laura Crispini
Andreas Kasinos
Niccolò Storni
Konstantinos Simeonidis
Anastasios Zouboulis
Mineralogy and Geochemistry of Ultramafic Rocks from Rachoni Magnesite Mine, Gerakini (Chalkidiki, Northern Greece)
Minerals
ophiolites
ultramafic
serpentinization
listvenites
Gerakini
magnesite ore
author_facet Evangelos Tzamos
Micol Bussolesi
Giovanni Grieco
Pietro Marescotti
Laura Crispini
Andreas Kasinos
Niccolò Storni
Konstantinos Simeonidis
Anastasios Zouboulis
author_sort Evangelos Tzamos
title Mineralogy and Geochemistry of Ultramafic Rocks from Rachoni Magnesite Mine, Gerakini (Chalkidiki, Northern Greece)
title_short Mineralogy and Geochemistry of Ultramafic Rocks from Rachoni Magnesite Mine, Gerakini (Chalkidiki, Northern Greece)
title_full Mineralogy and Geochemistry of Ultramafic Rocks from Rachoni Magnesite Mine, Gerakini (Chalkidiki, Northern Greece)
title_fullStr Mineralogy and Geochemistry of Ultramafic Rocks from Rachoni Magnesite Mine, Gerakini (Chalkidiki, Northern Greece)
title_full_unstemmed Mineralogy and Geochemistry of Ultramafic Rocks from Rachoni Magnesite Mine, Gerakini (Chalkidiki, Northern Greece)
title_sort mineralogy and geochemistry of ultramafic rocks from rachoni magnesite mine, gerakini (chalkidiki, northern greece)
publisher MDPI AG
series Minerals
issn 2075-163X
publishDate 2020-10-01
description The importance of magnesite for the EU economy and industry is very high, making the understanding of their genesis for the exploration for new deposits a priority for the raw materials scientific community. In this direction, the study of the magnesite-hosting ultramafic rocks can be proved very useful. For the present study, ultramafic rock samples were collected from the magnesite ore-hosting ophiolite of the Gerakini mining area (Chalkidiki, Greece) to investigate the consecutive alteration events of the rocks which led to the metallogenesis of the significant magnesite ores of the area. All samples were subjected to a series of analytical methods for the determination of their mineralogical and geochemical characteristics: optical microscopy, XRD, SEM, EMPA, ICP–MS/OES and CIPW normalization. The results of these analyses revealed that the ultramafic rocks of the area have not only all been subjected to serpentinization, but these rocks have also undergone carbonation, silification and clay alteration. The latter events are attributed to the circulation of CO<sub>2</sub>-rich fluids responsible for the formation of the magnesite ores and locally, the further alteration of the serpentinites into listvenites. The current mineralogy of these rocks was found to be linked to one or more alteration event that took place, thus a significant contribution to the metallo- and petrogenetic history of the Gerakini ophiolite has been made. Furthermore, for the first time in literature, Fe inclusions in olivines from Greece were reported.
topic ophiolites
ultramafic
serpentinization
listvenites
Gerakini
magnesite ore
url https://www.mdpi.com/2075-163X/10/11/934
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