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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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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