Next Article in Journal / Special Issue
Major- and Trace-Element Compositions of Indicator Minerals that Occur as Macro- and Megacrysts, and of Xenoliths, from Kimberlites in Northeastern Angola
Previous Article in Journal
Transmission X-ray Microscopy—A New Tool in Clay Mineral Floccules Characterization
Previous Article in Special Issue
Textural Evidence of Episodic Introduction of Metallic Nanoparticles into Bonanza Epithermal Ores
 
 
Search for Articles:
Title / Keyword
Author / Affiliation / Email
Journal
Article Type
 
 
Advanced Search
 
Section
Special Issue
Volume
Issue
Number
Page
 
Journals
Minerals
Volume 2
Issue 4
10.3390/min2040300
minerals-logo
Submit to this Journal Review for this Journal Propose a Special Issue
► Article Menu

Article Menu

share Share announcement Help format_quote Cite question_answer Discuss in SciProfiles thumb_up
...
Endorse textsms
...
Comment
first_page
settings
Order Article Reprints
Font Type:
Arial Georgia Verdana
Font Size:
Aa Aa Aa
Line Spacing:
Column Width:
Background:
Review

Geological, Mineralogical and Geochemical Aspects for Critical and Rare Metals in Greece

by
Vasilios Melfos
1,* and
Panagiotis Ch. Voudouris
2
1
Department of Mineralogy, Petrology and Economic Geology, Aristotle University of Thessaloniki, Thessaloniki 54124, Greece
2
Department of Mineralogy-Petrology, University of Athens, Athens 15784, Greece
*
Author to whom correspondence should be addressed.
Minerals 2012, 2(4), 300-317; https://doi.org/10.3390/min2040300
Submission received: 4 September 2012 / Revised: 9 October 2012 / Accepted: 10 October 2012 / Published: 19 October 2012
(This article belongs to the Special Issue Advances in Economic Minerals)
Browse Figures
Versions Notes

Abstract

:
The European Union (EU) is highly dependent on critical and rare metals which are very important for a sustainable development. However, European industry is not able to cover its demands from native sources and it imports commodities from third countries. Greece is one of the EU countries with the most potential for supplying these strategic metallic raw materials in the future, since it hosts a large number of ore deposits. The epithermal- and porphyry-type deposits and the reduced intrusion related systems of the Serbomacedonian and the Rhodope metallogenic provinces in Northeastern Greece are promising targets for a future exploitation and exploration in Sb, Te, Mo, Re, Ga, In, REE and PGE. Greece is the leading producer of Ni and Al in the EU from laterites and bauxites of central and northern Greece. These deposits also contain significant amounts of Co or REE which should be considered in the future plans of the processing industries. REE are found in high contents at the placer deposits between Chalkidiki and Kavala (North Greece) and elevated PGE concentrations are associated with the chromitites of northwestern Greece. Therefore, the mineral wealth of Greece can contribute significantly to a sustainable and a competitive economy of Europe.

1. Introduction

Raw materials, particularly metals, are very important for sustainable functioning, since they are essential for the high-tech products such as electrical and electronic devices, photovoltaic systems, batteries, catalysts, optical fiber cables, synthetic fuels, etc. European industry needs sufficient access to certain mineral raw materials for the sound functioning of the EU’s economy. However, the European Union (EU) is highly dependent on imports from third countries of strategically important metals, which are considered to be critical because of their economic value, the high supply risks affected by market distortions and the continuously decrease of their availability. An expert group under the auspices of the European Commission published in 2010, a list of 14 metal raw materials which are considered to be “critical” for the future sustainable development of EU: antimony, beryllium, cobalt, fluorine, gallium, germanium, graphite, indium, magnesium, niobium, platinum group metals, rare earths, tantalum and tungsten [1]. Due to their low concentrations in earth’s crust, the critical metals are produced as by-products of other metals which are mined.
During the last years issues concerning the EU policy on securing raw material supplies by improving resource efficiency and recycling, have been high on the political agenda. In November 2008 the new European policy entitled: “The Initiative for raw materials to meet critical needs for growth and employment in Europe” was adopted and promulgated by the EU [2]. This initiative refers to the need of the EU to follow a comprehensive policy for ensuring access to mineral raw materials in order to enhance competitiveness and to achieve the Lisbon partnership for growth and employment.
The EU has many ore mineral deposits, even if their exploration and extraction are facing increased competition for different land uses and a highly protected environment, as well as several limitations in access to these deposits. Greece is one of the most significant metallogenic provinces of EU hosting a large number of ore deposits, which may provide an essential mineral wealth, including critical metals.
Mining has been part of the Greek civilization since prehistoric times, when Greeks began extracting non-metallic minerals and metals for use. Ancient underground mines and ruins of metallurgical furnaces throughout Greece are witnesses of the intense exploitation of the metallic mineral resources, mainly gold, silver, copper, lead and iron. Especially during the Classical and Hellenistic times, famous mining centers operated in Lavrion (Attica), Sifnos and Milos Islands (Aegean sea), Pangeon Mt, Palea Kavala, Chalkidiki and Thasos Island (northern Greece) (Figure 1).
In the last 70 years significant mining operations in Greece have focused on nickel, aluminum, chromium and iron-manganese deposits, as well as lead-zinc-(±Cu, ±Au, ±Ag) sulfide occurrences. However, several of these operations have been stopped in the last years due to various reasons. Recent investigations, especially in northern Greece (Macedonia and western Thrace), have revealed new prospects of gold-silver, copper, molybdenum-rhenium, antimony, tungsten and tellurium ore mineralization. According to [3] the total value of the indicated metallic mineral reserves of Greece exceeds €72 billion. It should be mentioned that Greece is the only country in the EU with large deposits of manganese, chromite, aluminum and nickel. It is the leading producing country in the EU for aluminum (from bauxite) and nickel (from laterite). Significant production of magnesium (from magnesite) is also reported. Greece has a comparative advantage in relation to other European countries due to the presence of a significant mineral wealth.
Minerals 02 00300 g001 1024
Figure 1. Map of Greece with the distribution of the most significant ore deposits. The ore deposits of Thrace are displayed in Figure 3.
Figure 1. Map of Greece with the distribution of the most significant ore deposits. The ore deposits of Thrace are displayed in Figure 3.
Minerals 02 00300 g001
In the last decades, the metal mining industry of Greece operated far below its productive capacity, with an exception of bauxite and laterite. This was affected also by the relatively reduced industrial activities, the long distance from the central European markets which restricted the export potential of the country, and the lack of considerable investments.
In this contribution we present briefly some new data, mainly on Te, In, La and Ce obtained from selected mineralizations (Pagoni Rachi, Perama Hill, Pangeon Mt., Pefka, Vathi/Kilkis) using ICP-MS bulk rock analyses in ACME Laboratories, of Canada. These data are combined with published information on the geology, mineralogy and geochemistry of several critical and rare metallic elements found in Greece, being necessary for the future sustainable development of the EU. We focus mainly on the less investigated metals Sb, Co, Te, Re, Mo, Ga, Ge, In, REE and Platinum Group Elements, because for other commodities like Mn, Cr, Ni, Al and Mg, there is a broad knowledge and experience with mining in Greece. These data will contribute significantly to the knowledge about the presence of critical metals in specific regions of Greece, for a possible future exploration and exploitation.

2. Geological Overview and Various Ore Deposit Styles in Greece

Geological setting of Greece consists of various elongated geotectonic terrains which represent successive episodes of oceanic riftings, spreadings, subductions and collisions in the region of Neotethys, known as Hellenide orogen [4]. The evolution of the Neotethys Ocean and the related lithosphere plates caused magmatic processes which led to the formation of considerable ore mineralizations.
Large magmatic Cr-(±PGE) deposits (Vourinos, Xerolivado, Milia, Korydallos/Pindos, Eretria, Domokos/Othrys, Chalkidiki and eastern Thessaly) (Table 1) are related with Mesozoic ophiolitic chains along the Pindos and Vardar ocean sutured zones. Ni-Fe laterites (Lokris, Evia, Kastoria) and Al bauxites (Parnassos Mt, Gkiona Mt) are also associated with these ophiolites, although most of these deposits are allochthonous, being incorporated among various karstified limestones due to the subsequent sedimentary processes. Only few, mostly uneconomic, VMS-type mineralizations (Table 1) are also in close association with the Mesozoic ophiolitic sequences within meta-volcanosedimentary rocks of basic affinity. They are mainly of Cu-pyrite Cyprus-, Kuroko Zn-Pb-Ag- and Fe-Cu-Ni-Co-type, forming stratabound and stratiform ore bodies in Xylagani (Thrace), in Vermio (Veria), in Perivoli (Pindos), in Agioi Theodoroi, Limogardi (Othrys), Eretria (Evia) and in Ermioni and Molaoi/Lakonia (Peloponnesos) (Table 1, Figure 1).
Significant precious and base metal sulfide ore deposits are widespread in Attic-Cycladic ore belt (south Evia, Sifnos, Mykonos, Tinos, Kythnos), along the South Aegean Active Volcanic Arc (Milos) and in Attica (Lavrion), of Lower Pliocene to Miocene age [5]. However, the most promising regions for future critical- and rare-metal exploration projects are the Serbomacedonian and Rhodope metallogenic provinces (Figure 2 and Figure 3), in northeastern Greece [6]. These provinces include skarn-(Kimmeria/Xanthi), carbonate-replacement-(Olympias, Stratoni/NE Chalkidki), reduced intrusion-related-(Palea Kavala), epithermal (Perama Hill, Mavrokoryfi, Kassiteres, Sapes, Agios Philippos/Kirki, Pefka/Evros) and porphyry-(Pagoni Rachi/Kirki, Kassiteres-Sapes, Maronia, Skouries/Chalkidiki, Vathi and Gerakario/Kilkis) deposit styles, as well as placer gold occurrences and supergene fault/karst-controlled manganese oxides (Drama, NE Chalkidiki) and gold-bearing iron oxides (Palea Kavala, Thasos) [6,7]. These deposits are characterized by Pb, Zn, Sb, Bi, Cu and Mo ores with, less commonly, economic concentrations of Fe and Sn. They also include minor Au, Ag, PGE, Te, U, W, Re and As occurrences [7].
Table
Table 1. Characteristics of critical- and rare metal-bearing mineralization in Greece (data sources in text).
Table 1. Characteristics of critical- and rare metal-bearing mineralization in Greece (data sources in text).
Mineralization-typeProvinceAreaMain metalsCritical and rare metals
Magmatic Cr-(±PGE) PindosVourinosCrPGE
PindosXerolivadoCrPGE
PindosMiliaCrPGE (Os, Ir, Ru)
PindosKorydallosCrPGE (Pt, Pd, Ru, Rh)
Evia EretriaCr–
OthrysDomokosCr–
ThessalonikiTriadi-VassilikaCrPGE
ChalkidikiVavdosCrPGE
ChalkidikiGerakini-OrmyliaCrPGE
Eastern ThessalyKallipefki, AgiaCr–
Aegean seaSkyrosCrPGE (Ru)
VeriaVermioCrPGE (Os, Ir, Ru, Rh, Pt, Pd)
VMS (Cyprus- and Kuroko-type)ThraceXylaganiCu, Fe, Au–
SerresLagadiCu, FeCo
VeriaVermioFe, Cu, Ni, CoCo
KilkisPolykastroPb, Zn, AgIn, Ge, Ga
PindosPerivoliFe, CuCo
OthrysAgioi TheodoroiFe, Cu, Ni, CoCo
OthrysLimogardiFe, Cu, Ni, CoCo
PeloponnesosErmioniCu, FeCo
PeloponnesosMolaoi/LakoniaZn, Pb, AgIn, Ge, Ga
Ni-Fe lateritesLokrisLarymnaNi, FeCo
Evia Ni, FeCo
KastoriaIeropigiNi, FeCo
GrevenaPaleochoriNi, FeCo
VeriaVermioNi, FeCo
Al bauxitesParnassos AlREE
Gkiona AlREE
Shear-zone related ChalkidikiStanosCu, Au, Bi, MoTe
LachanasRizanaSb, WSb
ThessalonikiPhiladelphiaSb, Fe, AuSb
Carbonate replacement ChalkidikiOlympiasPb, Zn, Au, AgIn, Ge, Ga
ChalkidikiStratoniPb, Zn, AgTe
XanthiThermesPb, Zn, AgIn, Ge, Ga
AtticaKamariza/LavrionPb, Zn, Ag, AuIn
Reduced intrusion-hosted KilkisPigi MoW
ThraceKimmeria/XanthiFe, Cu, Mo, BiW
KavalaPalea KavalaAu, BiTe
Kavala-DramaPangeon MtAu, BiTe
AtticaPlaka/LavrionCu, Pb, ZnGa, REE (La, Ce)
Epithermal ThracePerama HillCu, As, Au, BiTe
MavrokoryfiCu, Sb, Ag, AuTe
St. Demetrios/SapesCu, As, Au, AgTe
St. Barbara/ KassiteresCu, Au, AgTe
Agios Philippos/KirkiPb, As, Cu, Ag, Bi In, Ga, Ge
Pefka/EvrosCu, As, Ag, AuTe, In,
KalotychoFe, Cu–
KallyntirionPb, Zn, Cu, Au, AgSb
Aegean SeaTinos IslandCu, Pb, Au, AgTe
Limnos IslandPb, Zn, Cu, Au, AgTe
Porphyry ThracePagoni Rachi/KirkiCu, Au, MoTe, Re
Konos/SapesCu, Au, MoTe, Re
MaroniaCu, Au, MoRe
Myli/EsymiCu, Au, Mo–
MelitenaCu, MoRe
ChalkidikiSkouriesCu, Au, MoPGE (Pd, Pt)
KilkisVathiCu, Au, MoREE (La, Ce)
GerakarioCu, AuSb
AtticaPlaka/LavrionMoW
Aegean SeaSardes/Limnos IslandMo–
Fakos/Limnos IslandCu, Mo–
Stypsi/Lesvos IslandMo, Bi–
Supergene fault /karst-controlled Mn-oxidesDrama Mn–
NE Chalkidki Mn–
Fe-oxidesKavalaPalea KavalaAu–
Thasos Au–
Sediment-hosted, placersVeriaVegoraPGa
Aegean SeaChios Island–Sb
Chalkidiki-KavalaCoastal zone–REE (Ce, La, Nd, Pr)
The Serbomacedonian and Rhodope metamorphic massifs comprise the crystalline basement of the Alpine orogenic belt in the Balkan peninsula and consist of amphibolite facies metamorphic rocks of continental and oceanic origin (Figure 2 and Figure 3). They demonstrate a structural record of a late Mesozoic deformation episode overprinted by an early Cenozoic extensional deformation [8]. The deposits of the Serbomacedonian and Rhodope metallogenic provinces were formed during the final stage of the Tertiary orogenic collapse, which led to the formation of widespread Oligocene-Miocene silicic to intermediate magmatism [7,9,10,11]. This magmatism, considered to be part of the Cretaceous to Miocene Alpine-Balkan-Carpathian-Dinaride orogen [11], resulted from subduction and collision of the Pelagonian and Apulian microcontinents, detached from Africa in Triassic, with the European plate [12]. Slab detachment and/or roll-back was the principal mechanism, which resulted in the local ascent of asthenospheric mantle into the metasomatized mantle lithosphere and to magma generation [9,13]. Magmas were intruded to shallow depths along deep seated detachment faults, forming mafic to intermediate mantle-derived plutonic, subvolcanic and volcanic rocks of calc-alkaline, high-K calc-alkaline and shoshonitic to ultra-potassic (lamprophyric) affinities.
Minerals 02 00300 g002 1024
Figure 2. Simplified geological map of the Serbomacedonian metallogenic province in Greece, displaying the major ore deposits and prospects.
Figure 2. Simplified geological map of the Serbomacedonian metallogenic province in Greece, displaying the major ore deposits and prospects.
Minerals 02 00300 g002
Minerals 02 00300 g003 1024
Figure 3. Simplified geological map of the Rhodope metallogenic province in Greece displaying the major Tertiary ore deposits and prospects [5,6 with modifications]. KmX: Kimmeria/Xanthi; Me: Melitena; Mr: Maronia; Ko: Konos/Sapes; SB: St. Barbara/Kassiteres; SD: St. Demetrios/Sapes; V: Viper; PH: Perama Hill; Mk: Mavrokoryfi; PR: Pagoni Rachi/Kirki; SPh: Agios Philippos/Kirki; Pf: Pefka; Ltr: Loutros; Kl: Kallyntirion; M-E: Myli/Esymi.
Figure 3. Simplified geological map of the Rhodope metallogenic province in Greece displaying the major Tertiary ore deposits and prospects [5,6 with modifications]. KmX: Kimmeria/Xanthi; Me: Melitena; Mr: Maronia; Ko: Konos/Sapes; SB: St. Barbara/Kassiteres; SD: St. Demetrios/Sapes; V: Viper; PH: Perama Hill; Mk: Mavrokoryfi; PR: Pagoni Rachi/Kirki; SPh: Agios Philippos/Kirki; Pf: Pefka; Ltr: Loutros; Kl: Kallyntirion; M-E: Myli/Esymi.
Minerals 02 00300 g003

3. Critical and Rare Metals in Greece

3.1. Antimony (Sb)

Antimony is used for a number of industrial applications, as diodes and infrared detectors in the semiconductor manufacturing. It is alloyed with lead to increase its hardness. Antimony compounds are used in batteries, low friction metals, paints, ceramics, glass and pottery, as flame retardants in adhesives, plastics, rubber and textiles. Stibnite (Sb2S3) is the predominant ore mineral of antimony. China supplies over 75% of the total world production and in 2010 introduced quantitative and export licensing restrictions. Therefore antimony was recently placed in the highest risk category for future supply disruption.
In Greece, antimony is found in quartz veins mainly in the form of stibnite. One of the most important Sb occurrences is the low-sulfidation epithermal system of Kallyntirion prospect at the Rhodope metallogenic province (Figure 3), also including Pb, Zn, Cu, Au and Ag. Another significant stibnite mineralization is the shear zone-related Rizana/Lachanas deposit, Serbomacedonian province, which is related to sheeted quartz veins crosscutting gneisses and amphibolites. The mineralization is spread over an area 10 km long and 2–4 km wide, and is potential for future exploitation. In the years 1931–1938 mining operations produced 2.3 × 10−6 kg of ore consisting more than 30% Sb [14]. The estimated reserves are over 5.0 × 10−7 kg with 30%–35% Sb, in addition to small tungsten concentrations, associated with wolframite [14]. According to [15] the chemical analyses of enriched samples from Rizana/Lachanas revealed Sb content between 71.73 and 83.87 wt % (average 75.77 wt %). Other stibnite occurrences with relatively low Sb contents are located in Philadelphia/Thessaloniki, Chios Island and Gerakario/Kilkis [14].
Except from stibnite, antimony is also incorporated in numerous sulfosalts (tetrahedrite, famatinite, chalcostibite, zinkenite, bournonite, boulangerite) which are common in porphyry-, epithermal- and intrusion-related systems at the Rhodope metallogenic province, such as in Maronia, Pagoni Rachi/Kirki, Agios Philippos/Kirki, Mavrokoryfi, Pefka, Perama Hill, Sapes, Kapsalina/Thasos, Pangeon Mt. In some cases mineralized samples contain over 0.2 wt % Sb [6,7,16,17]. In addition, the galena concentrates from Lavrion, Attica, contain from 0.3 to 0.7 wt % Sb [18].

3.2. Cobalt (Co)

Cobalt has been used for a long time as a pigment in glass and porcelain industry. Recently it was classified as one of the critical metals due to its unique applications in lithium ion batteries, in resistant superalloys, in green-energy systems and in magnets [19]. Globally, cobalt is mined as a by-product of copper and nickel deposits in the Republic of the Congo-DRC (40%), in Zambia (20%), in Canada, in Australia, in Cuba, etc. China imports large amounts of cobalt (almost all the DRC’s production) in order to produce refined cobalt which is exported to the USA and the EU.
Greece is the major nickel supplier in EU and produces 2%–3% of the world total Ni. Nickel is mined from the laterite deposits in Lokris, Evia and Kastoria and is recovered by pyrometallurgical methods. These Fe-Ni laterites, which also contain cobalt, are mainly allochthonous and are associated with Mesozoic ophiolites. They are intercalated in Mesozoic limestones and show multistage transportation and re-deposition, responsible for a post-sedimentary redistribution of metals, resulting in Mn, Co, Ni-rich zones [20,21]. Chemical composition of different laterite occurrences in Greece shows that cobalt is mainly concentrated in the Fe-Ni-rich zones, demonstrating elevated contents which reach 0.10% in Paleochori, Grevena, 0.14% in Vermio, 0.16% in Kastoria and 0.22% in Lokris [20,21,22]. Co in these deposits is concentrated mainly in the mineral asbolane [22]. The metallurgical process of the Greek laterites in Larymna by LARCO, which produces Fe-Ni alloy, does not allow any Co recovering, which can be separated by hydrometallurgical treatment [23]. Consequently, Greece remains a potential region to supply the EU with significant amounts of cobalt in the future.
It should be also mentioned here that the non-economic sulfide ores hosted in the ophiolite complexes in Greece, including Cyprus-type and Fe-Cu-Ni-Co type, at Pindos and Othrys contain up to 2300 ppm Co [24].

3.3. Tellurium (Te)

Tellurium, a relatively rare metalloid, is used in manufacturing alloys and semiconductors, as well in vulcanizing rubber and in catalysts for petroleum. In alloys it improves properties like ductility and tensile strength or increase the durability and flexibility. It is added to lead to decrease the corrosive action of sulfuric acid in batteries and to improve the lead’s strength and hardness. It is also used in making various types of detectors. Compounds made of Te, Cd and Hg, are excellent infrared sensitive semiconductors [25]. The use of high-purity tellurium enhances the effectiveness of the solar cell electric power generations and is very promising for future applications. Tellurium is extensively used as a coloring agent in ceramics and glasses. It is also used as a gasoline additive to reduce engine knocks in automobiles.
Almost all tellurium currently produced is obtained as a by-product of copper refining. It is estimated that the Cu deposits globally contain approximately 2.2 × 10−7 kg of tellurium reserves worldwide [25]. However, the high-grade ores are being exhausted and this may result in limitations in future tellurium supply.
In Greece tellurium is a common constituent of Cu-Au epithermal high-intermediate sulfidation type mineralizations (St. Barbara/Kassiteres, St. Demetrios/Sapes, Perama Hill, Mavrokoryfi, Pefka) and spatially associated porphyry Cu-Mo systems (Pagoni Rachi/Kirki, Konos/Sapes), in intrusion-related Au-Bi-Te systems (Palea Kavala, Pangeon Mt) of Oligocene-Miocene age at the Rhodope province, as well as in Limnos and Tinos Islands, Aegean sea (Fakos porphyry-epithermal- and Panormos intrusion-related Cu-Au-Te prospects respectively) [7,26,27,28]. Tellurium in these prospects is incorporated in various telluride phases, such as hessite, stützite, petzite, altaite, sylvanite, melonite, calaverite, coloradoite and tetradymite, as well as in the sulfosalt goldfieldite (tetrahedrite-group). In rare cases native tellurium is present in minor concentrations (Pefka, Tinos, Palea Kavala). The tellurium content in the mineralized samples is variable and is related with the distribution of Te-bearing minerals. According to new chemical analyses, provided here for the first time, the richest samples contain up to 40 ppm in Pagoni Rachi, 45 ppm in Perama Hill, 60 ppm in Pangeon Mt, and >1000 ppm in Pefka. Comparing with other potential Te-rich ore deposits worldwide (Boliden mining company will produce Te from the Kankberg gold mine, Sweden, with reserves of 2.8 Mt which contains 186 ppm Te in average [29]), the Pefka area is the most promising prospect for future Te exploration and exploitation in Greece.
The source rocks of the tellurides in northeastern Greek mineralizations are mantle-derived calc-alkaline (Thrace) to shoshonitic (Limnos) subvolcanic intrusions. Magmas were likely enriched in Te as a result of previous subduction of Te-bearing sediments [7].

3.4. Rhenium (Re) and Molybdenum (Mo)

Rhenium is very resistant against corrosion and is used in high-temperature superalloys for jet engines and industrial gas turbine engines. It improves the properties of tungsten and alloys in X-ray sources and in thermocouples to measure temperatures up to 2200 °C. Rhenium is also used in filaments, in chemical catalysts at petroleum industry, in space craft thrusters, in electrical contacts, in coatings, in flash lamps for photography. Radioactive rhenium is used in prevention and treatment of restenosis and liver cancer.
Molybdenum has various applications in the construction of grade and stainless steel, in chemicals such as lubricants, in the manufacturing of tool and high-speed steels, in the manufacture industry of cast iron and molybdenum metals, as well as in super alloys.
The world’s highest grade molybdenum-rhenium deposit is located in Merlin at the Mount Dore ore prospect, consisting mainly of molybdenite, with minor chalcopyrite and pyrite, and is hosted within a series of altered carbonaceous metapelites and phyllites [30]. The mineralization exceeds over 1 km in length and is up to 40 m thick, to approximately 550 m from the surface. The current resources average 0.6% Mo and 10 ppm Re.
Molybdenite occurs mainly in three mineralization styles in Greece [31]: (1) Porphyry Cu-Mo and Mo ± Cu (Pagoni Rachi/Kirki, Ktismata/Maronia, Myli/Esymi, Konos/Sapes, Skouries/Chalkidiki, Melitena, Sardes/Limnos, Fakos/Limnos, Stypsi/Lesvos); (2) Reduced intrusion-hosted Mo-W systems (Kimmeria/Xanthi, Pigi/Kilkis, PlakaP/Lavrion, Serifos Island); (3) Shear zone related Cu-Au-Bi-Mo (Stanos/Chalkidiki).
A small molybdenite production was operated in Pigi in 1940–1944 with variable Mo grade, from 0.3% to 1.3% (rarely up to 10%) with an average of 0.6%–0.7% [14]. There is not any estimation about the current Mo reserves.
The porphyry Cu-Mo and Mo ± -Cu prospects of Pagoni Rachi, Maronia and Melitena, in western Thrace contain molybdenite with high to ultrahigh Re content (reaching 4.7 wt %), which are the highest concentrations of Re-in-molybdenites ever measured [31,32,33]. The microprobe analyses demonstrate that there is a positive correlation between Mo and Re supporting the concept that Re substitutes for Mo in the structure of molybdenite. Moreover, the very rare mineral rheniite (ReS2) is found in the porphyry systems of the Pagoni Rachi and Konos/Sapes prospects [31,33].
Rheniite and high-Re molybdenite in these deposits precipitated under oxidizing conditions and from relatively acid hydrothermal solutions. The extremely high contents of rhenium in molybdenite at the Greek porphyry prospects could be explained by a rhenium release from the asthenospheric mantle wedge by subduction-related fluids and melts [33]. The Re-enrichment in the western Thrace molybdenites, suggest that this region should be a potential target for future Re- and Mo exploration and exploitation.

3.5. Gallium (Ga), Germanium (Ge) and Indium (In)

The rare metals gallium, germanium and indium are the most important commodities in the high-technology society, essential for electronic components. They are critical metals for the efficiency of utilization of recourses that are used and consumed in the order of millions of tones [34]. Moreover, germanium has major applications in optical materials and indium in liquid crystal displays (LCD). Presently gallium is produced as a by-product of bauxite processing and from the zinc processing residues, although the largest reserves are associated with phosphate ores [19]. Germanium and indium are recovered during the zinc production process.
The epithermal polymetallic veins of the Rhodope province are the most promising ore types for Ga, Ge and In exploitation in Greece. The Agios Philippos mine at Kirki, western Thrace, is a polymetallic vein deposit with intermediate-high sulfidation epithermal affinities and contains an unusual mineralogy consisting of several Pb-As-Cu-Bi-Sn sulfosalts. It is hosted within Eocene sediments and displays spatial relationships to Upper Oligocene rhyolite porphyry exposed at the northern part of the mining area. Wurtzite is the dominant Zn-ore mineral in Agios Philippos, along with sphalerite, and is found in the form of veinlets and granular masses. It contains considerable amounts of In (reaching 3.5 wt %) and Ga (reaching 1.6 wt %), whereas Ge is present in smaller amount (below 0.3 wt %) [35].
In Pefka/Evros the high-intermediate sulfidation epithermal mineralization is related to quartz veins hosted within andesitic and dacitic volcanic rocks. Bulk ore analyses (present study) revealed relatively high In content (up to 675 ppm), whereas Ga and Ge are low (max 17 ppm and 16 ppm respectively). Another potential deposit for future Ga exploration is the Lavrion intrusion-related deposit, especially the Pb-Zn-Cu bearing granitic dikes from Plaka deposit, where Ga reaches 326 ppm [36].
Relatively lower contents of In are indicated for the Lavrion carbonate-replacement ore bodies where sphalerite concentrates contain up to 43 ppm and the bulk Cu-pyritic ores up to 72 ppm [18]. The Polykastro/Kilkis and Molaoi/Peloponessos (Kuroko-type) and the Thermes/Xanthi and Olympias/Chalkidiki (carbonate-replacement) deposits should be also evaluated for their In, Ge and Ga potential [3].
Phosphate ores represent the largest reserves of several million tons, generally with a low Ga-content of 0.01%–0.1% [19]. The Neogene phosphate deposits of Greece contain low Ga content in general. The highest concentrations have been referred in the Vegora lacustrine basins of Vegora (Vegora-Komnina), 40 km northwest from Veria, where Ga in the phosphatic rocks reaches 15.9 ppm [37], and they cannot be considered as potential sources for future exploitation.

3.6. Rare Earth Elements (REE)

The demand for rare earth elements (REE) has been increased in the last years due to their applications in a wide range of consumer products such as automotive catalytic converters, photovoltaic systems, wind turbines, flat panel displays (cell phones, screen TVs, computers, portable DVDs), permanent magnets, hybrid and electric vehicles. They are also strategic raw materials with important defense uses in jet fighter engines, space-based satellites and communication systems. China controls approximately 95% of the global supply of rare earths and recently imposed quotas on exports in order to preserve its resources for domestic consumption. This has caused concerns in the EU, USA and Japanese markets regarding future REE supplies.
Recently it was announced that by 2013 USA will be able to meet a majority of its demands from North American sources [38]. European industry imports more than 90% of its REE needs and consumes about 30% of the global annual production [38]. The abandoned mines in Greece could relieve European industry problems [39] and this is in accordance with the recent investigation results in several areas of Greece.
Significant reserves of REE are found in the placer deposits along the coast of Northeastern Greece between the peninsula of Chalkidiki and Kavala, with 240 km coastal length [40,41,42]. Geochemical investigations revealed up to 8000 ppm in REE with 93.5% consisting of the light REE mainly Ce, La, Nd and Pr, with allanite being the main REE-bearing mineral phase [40]. It is very probable that the primary sources of these LREE bearing placers are located at the nearby Kavala or Pangeon Mt. intrusion-related systems. Recently, one metallurgical scoria from old smelting furnaces (possibly from Ottoman period) at the Pangeon Mt., revealed 6171 ppm La, 10,883 ppm Ce, 1062 ppm Pr, 3249 ppm Nd, 334 ppm Sm and 214 ppm Eu [43]. Further geological and geochemical research could help locate the extremely high LREE-enriched source rocks, possibly on Pangeon Mt. It should be however mentioned that the heavy REE are the more highly sought after in the world industry.
Of major importance for future REE exploration-exploitation can also be considered the bauxite deposits of Parnasos Mt, with REE contents reaching 6300 ppm [3], the Pb-Zn-Cu bearing granitic dikes from Plaka deposit in Lavrion with 428 ppm La and 976 ppm Ce [36], and the porphyry Cu-Au system of Vathi/Kilkis with relatively high content of La (500 ppm) and Ce (715 ppm) [this study].

3.7. Platinum Group Elements (PGE)

An increased worldwide usage of platinum group elements (PGE = Pt, Os, Ir, Pd, Ru, Rh) has been observed during the last decades, due to their unique physical and chemical properties that make them critical to many emerging technologies. Consequently they have become essential commodities and are considered as strategic metals because of their specialized applications in chemical, petroleum, high-tech, electrical, medical, and aerospace industries [19]. They also have important uses in environmentally related technologies, such as automobile catalytic converters and fuel cells. The global reserves of PGE are mainly concentrated in South Africa, followed by Russia and Canada, where they are by-products of nickel processing [19].
In Greece there are two target mineralization groups that contain elevated PGE grades: Porphyry-type deposits and chromite ores. A significant Pd-Pt enrichment has been determined in the Skouries porphyry Cu-Au deposit of NE Chalkidiki peninsula, in the copper ore, as well as and in the flotation concentrates [44,45]. The Pd content in the mineralized samples (stockwork veinlets from the potassic alteration and from the oxidation zones) ranges from 45 to 490 ppb and up to 3300 ppb in chalcopyrite concentrates, suggesting that Pd (in the form of the telluride merenskyite) is mainly associated with chalcopyrite [44]. The leaching process of the final concentrate (21 wt % Cu, 22 ppm Au, 2.4 ppm Pd, 0.04 ppm Pt) resulted in the recovery of 96.6% Au, 97.7% Pd and 100% Pt [45]. Since the intended investment in the Skouries deposit focuses on gold and copper mining and metallurgy, the recovery of Pd and Pt has a positive economic potential for a future sustainable development.
The second target mineralization group for PGE exploration in Greece is associated with the ophiolites of Veria, Pindos and Skyros Island. High PGE concentrations, reaching 25 ppm total PGE’s (Os = 7400, Ir = 6020, Ru = 9700, Rh = 310, Pt = 760, Pd = 750, all in ppb) were determined in chromitites hosted in the Veria ophiolites, northern Greece [46,47]. These elevated PGE contents are associated with a great number (>100) of different PGM grains, mainly Os-Ru-Ir-Fe alloys, reaching 1 mm in size [47]. They are concentrated along a shear zone of strongly brecciated chromite ore. In Korydallos area, Pindos the PGE-mineralization is associated with several PGM grains (Pd-Cu alloys, sperrylite, Pt-Fe-Ni alloys, naldrettite, bismuthotelluride, native Au, etc.) [48]. The total PGE + Au content in the chromitites with low Cr# chromian spinel is 28 ppm (Pt = 17100, Pd = 7860, Ru = 2100, Rh = 1140, all in ppb) among the highest ever measured in ophiolitic chromitites worldwide, and the highest ever mentioned for chromitites from Greece [48]. It is assumed that a sulfur bearing melt played an important role in scavenging the PGE + Au content of the silicate magma from which chromian spinel had already started to crystallize [48].
The ophiolitic complexes of Thessaloniki (Triadi, Vassilika) and Chalkidiki (Vavdos, Gerakini-Ormylia) contain relatively low PGE contents (<0.5 ppm) and so they are not of economic significance [49].

4. Conclusions

The Serbomacedonian and Rhodope metallogenic districts in Greece (Figure 2 and Figure 3) are among the richest ore provinces in Europe, and can be an exploration target in the near future, especially for critical and rare metals. The epithermal- and porphyry-type mineralizations, and the reduced intrusion-related systems of Northeastern Greece could produce Sb, Te, Mo, Re, Ga, In and PGE as by-products, along with base metals, Au and Ag, if the mining and extractive activities will start. In addition, laterites and bauxites of central and northern Greece which are mined for Ni and Al respectively, contain significant amounts of Co or REE and the processing industries should focus on the probability for a future exploitation. The chromitites of northwestern Greece contain significant concentrations of PGE, whereas the coastal sediments between Chalkidiki and Kavala are characterized by REE geochemical anomalies which may be related with the Kavala and Pangeon Mt reduced intrusion-related system, although this has to be clarified.
The mineral wealth of Greece can provide solutions to the challenge of a sustainable and a competitive economy. The rational exploitation of the ore deposits will offer significant developmental benefits and it will enable Greece to strengthen its global role in the mining industry. A new mining policy must focus on the more effective exploitation of the mineral resources, the improvement of the environmental performance, the safe operation of the mines and the accidents prevention, the mining waste management and the recycling process. However, when considering the exploitation of critical and rare metals, we have to keep in mind that this process is long, entails a high risk and requires large investments.

Acknowledgments

Special thanks are due to Basilios Tsikouras and two anonymous reviewers for carefully reviewing the manuscript and for their constructive comments and suggestions, resulting in significant improvement of this paper.

References

  1. Commission of the European Communities. Critical Raw Materials for the EU:Report of the ad-hoc Working Group on Defining Critical Raw Materials. Available online: http://ec.europa.eu/enterprise/policies/raw-materials/documents/index_en.htm (accessed on 16 October 2012).
  2. Commission of the European Communities. Commission Staff Working Document. Available online: http://ec.europa.eu/enterprise/sectors/metals-minerals/files/sec_2741_en.pdf (accessed on 16 October 2012).
  3. Tsirambides, A.; Filippidis, A. Exploration key to growing Greek industry. Ind. Miner. 2012, 44–47. [Google Scholar]
  4. Pe-Piper, G.; Piper, D.J. The Igneous Rocks of Greece; Gebroder Borntraeger: Berlin, Germany, 2002. [Google Scholar]
  5. Skarpelis, N. Geodynamics and evolution of the miocene mineralization in the Cycladic-Pelagonian belt, Hellenides. Bull. Geol. Soc. Greece 2002, 34, 2191–2206. [Google Scholar]
  6. Melfos, V.; Vavelidis, M.; Christofides, G.; Seidel, E. Origin and evolution of the tertiary Maronia porphyry copper-molybdenum deposit, Thrace, Greece. Miner. Deposita 2002, 37, 648–668. [Google Scholar] [CrossRef]
  7. Voudouris, P. Comparative mineralogical study of tertiary Te-rich epithermal and porphyry systems in northeastern Greece. Mineral. Petrol. 2006, 87, 241–275. [Google Scholar] [CrossRef]
  8. Bonev, N.; Dilek, Y.; Hanchar, J.M.; Bogdanov, K.; Klain, L. Nd-Sr-Pb isotopic composition and mantle sources of triassic rift units in the Serbo-Macedonian and the western Rhodope massifs (Bulgaria–Greece). Geol. Mag. 2012, 149, 146–152. [Google Scholar] [CrossRef]
  9. De Boorder, H.; Spakman, W.; White, S.H.; Wortel, M.J.R. Late cenozoic mineralization, orogenic collapse and slab detachment in the European Alpine belt. Earth Planet. Sci. Lett. 1998, 164, 569–575. [Google Scholar] [CrossRef]
  10. Marchev, P.; Kaiser-Rohrmeier, M.; Heinrich, Ch.; Ovtcharova, M.; von Quadt, A.; Raicheva, R. Hydrothermal ore deposits related to post-orogenic extentional magmatism and core complex formation: The Rhodope Massif of Bulgaria and Greece. Ore Geol. Rev. 2005, 27, 53–89. [Google Scholar] [CrossRef]
  11. Heinrich, C.A.; Neubauer, F. Cu-Au-Pb-Zn-Ag metallogeny of the Alpine-Balkan-Carpathian-Dinaride geodynamic province. Miner. Deposita 2002, 37, 533–540. [Google Scholar] [CrossRef]
  12. Pe-Piper, G.; Christofides, G.; Eleftheriadis, G. Lead and neodymium isotopic composition of Tertiary igneous rocks of northeastern Greece and their regional significance. Acta Vulcanol. 1995, 10, 255–263. [Google Scholar]
  13. Blundell, D.; Arndt, N.; Cobblod, P.R.; Heinrich, C. Processes of tectonism, magmatism and mineralization: Lessons from Europe. Ore Geol. Rev. 2005, 27, 333–349. [Google Scholar] [CrossRef]
  14. Maben, B.F.; Zigdis, I.G. The Mineral Wealth of Greece; UNRRA: Athens, Greece, 1947. [Google Scholar]
  15. Vasilatos, Ch.; Mparlas, K.; Stamatakis, M.; Tsivilis, S. Wolframite-stibnite mineral assemblages from Rizana Lachanas, Macedonia, Greece, and their possible use as flux agent in the manufacturing of clinker. Bull. Geol. Soc. Greece 2001, 3, 827–834. [Google Scholar]
  16. Voudouris, P.; Papavasiliou, C.; Melfos, V. Silver mineralogy of St Philippos deposit (NE Greece) and its relationship to a Te-bearing porphyry-Cu-Mo mineralization. Geoch. Mineral. Petrol. 2005, 43, 155–160. [Google Scholar]
  17. Eliopoulos, D.G.; Kilias, S.P. Marble-hosted submicroscopic gold mineralization at Asimotrypes area, mount Pangeon, southern Rhodope core complex, Greece. Econ. Geol. 2001, 106, 751–780. [Google Scholar] [CrossRef]
  18. Skarpelis, N. The Lavrion deposit (SE Attika, Greece): Geology, mineralogy and minor elements chemistry. N. Jb. Miner. Abh. 2007, 183, 227–249. [Google Scholar] [CrossRef]
  19. Buchert, M.; Schüler, D.; Bleher, D. Critical metals for future sustainable technologies and their recycling potential. Available online: http://resourcefever.com/detail/items/critical-metals-for-sustainable-technologies-and-their-recycling.html (accessed on 11 October 2012).
  20. Eliopoulos, D.G.; Economou-Eliopoulos, M. Geochemical and mineralogical characteristics of Fe-Ni- and bauxitic-laterite deposits of Greece. Ore Geol. Rev. 2000, 16, 41–58. [Google Scholar] [CrossRef]
  21. Eliopoulos, D.G.; Economou-Eliopoulos, M.; Apostolikas, A.; Golightly, J.P. Geochemical features of nickel-laterite deposits from the Balkan peninsula and Gordes, Turkey: The genetic and environmental significance of arsenic. Ore Geol. Rev. 2012, 48, 413–427. [Google Scholar] [CrossRef]
  22. Apostolikas, A.; Frogoudakis, E.; Maglaras, K. Nickel-bearing deposits in Western Macedonia, Greece: Present and perspectives. In Proceedings of the 1st Conference of the Committee of Economic Geology, Mineralogy and Geochemistry of the Geological Society of Greece, Kozani, Greece, 11–14 May 2000.
  23. Herrington, R. Potential for cobalt recovery from lateritic ores in Europe. In Geophysical Research Abstracts; European Geosciences Union: Vienna, Austria, 2012. [Google Scholar]
  24. Economou-Eliopoulos, M.; Eliopoulos, D.; Chryssoulis, S. A comparison of high-Au massive sulfide ores hosted in ophiolite complexes of the Balkan Peninsula with modern analogues: Genetic significance. Ore Geol. Rev. 2008, 33, 81–100. [Google Scholar] [CrossRef]
  25. Moss, R.L.; Tzimas, E.; Kara, H.; Willis, P.; Kooroshy, J. Critical metals in strategic energy technologies—assessing rare metals as supply-chain bottlenecks in low-carbon energy technologies. Available online: http://publications.jrc.ec.europa.eu/repository/handle/111111111/22726 (accessed on 11 October 2012).
  26. Fornadel, A.P.; Spry, P.G.; Melfos, V.; Vavelidis, M.; Voudouris, P. Is the Palea Kavala Bi-Te-Pb-Sb ± Au district, northeastern Greece, an intrusion-related system? Ore Geo. Rev. 2011, 39, 119–133. [Google Scholar] [CrossRef]
  27. Fornadel, A.P.; Voudouris, P.; Paul, G.S.; Melfos, V. Mineralogical, stable isotope, and fluid inclusion studies of spatially related porphyry Cu and epithermal Au-Te mineralization, Fakos Peninsula, Limnos Island, Greece. Mineral. Petrol. 2012, 105, 85–111. [Google Scholar] [CrossRef]
  28. Tombros, S.; Seymour, K.St.; Williams-Jones, A.E. Controls on Tellurium in Base, Precious, and Telluride minerals in the Panormos bay Ag-Au-Te Deposits, Tinos Island, Cyclades, Greece. Econ. Geol. 2010, 105, 1097–1111. [Google Scholar] [CrossRef]
  29. Wellstead, J. Finding Tellurium. Available online: http://telluriuminvestingnews.com/222-finding-tellurium-production-canada-china-sweden-deer-horn-jet-gold/ (accessed on 11 October 2012).
  30. Brown, M.; Lazo, F.; Carter, P.; Goss, B.; Kirwin, D. The geology and discovery of the Merlin Mo-Re zone of the mount Dore deposit, mount Isa Inlier, NW Queensland, Australia. SGA News 2010, 9–15. [Google Scholar]
  31. Voudouris, P.; Melfos, V.; Moritz, R.; Spry, P.G.; Ortelli, M.; Kartal, T. Molybdenite occurrences in Greece: Mineralogy, geochemistry and rhenium content. In Scientific Annals of the School of Geology AUTH, Proceedings of the XIX Congress of the Carpathian-Balkan Geological Association, Thessaloniki, Greece, 23–26 September 2010; pp. 369–378.
  32. Melfos, V.; Voudouris, P.; Arikas, K.; Vavelidis, M. Rhenium-rich molybdenites in Thracian Μο ± Cu porphyry occurrences, NE Greece. Bull. Geol. Soc. Greece 2001, 34, 1015–1022. [Google Scholar]
  33. Voudouris, P.C.; Melfos, V.; Spry, P.G.; Bindi, L.; Kartal, T.; Arikas, K.; Moritz, R.; Ortelli, M. Rhenium-rich molybdenite and rheniite (ReS2) in the Pagoni Rachi-Kirki Mo-Cu-Te-Ag-Au deposit, Northern Greece: Implications for the rhenium geochemistry of porphyry style Cu-Mo and Mo mineralization. Can. Mineral. 2009, 47, 1013–1036. [Google Scholar] [CrossRef]
  34. Wellmer, F.-W.; Becker-Platen, J. Sustainable development and the exploitation of mineral and energy resources: A review. Int. J. Earth Sci. 2002, 91, 723–745. [Google Scholar] [CrossRef]
  35. Driesner, T.; Pintea, I. Constraints on the conditions of wurtzite formation at the Agios Philippos Pb-Zn deposit, NE-Greece. Berichte der Deutschen Mineralogischen Gesellschaft. Beihefte zum European Journal of Mineralogy 1994, 6, 54. [Google Scholar]
  36. Bonsall, T.A.; Spry, P.G.; Voudouris, P.; Tombros, S.; Seymour, K.; Melfos, V. The geochemistry of carbonate-replacement Pb-Zn-Ag mineralization in the Lavrion district, Attica, Greece: Fluid inclusion, stable isotope, and rare earth element studies. Econ. Geol. 2011, 106, 619–651. [Google Scholar] [CrossRef]
  37. Stamatakis, M.G. Phosphate deposits of Neogene age in Greece: Mineralogy, geochemistry and genetic implications. Chem. Erde-Geochem. 2004, 64, 329–337. [Google Scholar] [CrossRef]
  38. Humphries, M. Rare Earth Elements: The Global Supply Chain; Congressional Research Service: Washington, DC, USA, 2012. [Google Scholar]
  39. Tirone, J. Greek, Nordic rare earths could save European industry. Available online: http://www.bloomberg.com/news/2012-04-26/greek-nordic-rare-earths-could-save-european-industry.html (accessed on 11 October 2012).
  40. Perissoratis, C.; Moorby, S.A.; Angelopoulos, I.; Cronan, D.S.; Papavasiliou, C.; Konispoliatis, N.; Sakellariadou, F.; Mitropoulos, D. Mineral concentrations in the recent sediments of Eastern Macedonia, Northern Greece: Geological and geochemical considerations. In Mineral Deposits within the European Community; Boissonnas, J., Omenetto, P., Eds.; Springer: Berlin, Germany, 1988; pp. 530–552. [Google Scholar]
  41. Pergamalis, F.; Karageorgiou, D.E.; Koukoulis, A.; Katsikis, I. Mineralogical and chemical composition of sand ore deposits in the seashore zone Nea Peramos—Loutra Eleftheron Kavala (N. Greece). Bull. Geol. Soc. Greece 2001, 34, 845–850. [Google Scholar]
  42. Pergamalis, F.; Karageorgiou, D.E.; Koukoulis, A. The location of Tl, REE, Th, U, Au deposits in the seafront zones of Nea Peramos-Loutra Eleftheron area, Kavala (N. Greece) using γ radiation. Bull. Geol. Soc. Greece 2001, 34, 1023–1029. [Google Scholar]
  43. Vaxevanopoulos, M. Aristotle University of Thessaloniki, Thessaloniki, Greece. Personal communication, 2012. [Google Scholar]
  44. Economou-Eliopoulos, M.; Eliopoulos, D. Palladium, platinum and gold concentration in porphyry copper systems of Greece and their genetic significance. Ore Geol. Rev. 2000, 16, 28–40. [Google Scholar]
  45. Kiousis, G.; Economou-Eliopoulos, M.; Paspaliaris, I.; Mitsis, I. Gold, palladium and platinum recovery, as by-products, from the Skouries porphyry Cu-Au deposit, Chalkidiki area, northeastern Greece—preliminary results. In Mineral Deposit Research: Meeting the Global Challenge, Proceedings of the Eighth Biennial SGA Meeting, Beijing, China, 18–21 August 2005; pp. 991–994.
  46. Economou-Eliopoulos, M. Platinum-group element distribution in chromite ores from ophiolite complexes: implications for their exploration. Ore Geol. Rev. 1996, 11, 363–381. [Google Scholar] [CrossRef]
  47. Tsoupas, G.; Economou-Eliopoulos, M. High PGE contents and extremely abundant PGE-minerals hosted in chromitites from the Veria ophiolite complex, Northern Greece. Ore Geol. Rev. 2008, 33, 3–19. [Google Scholar] [CrossRef]
  48. Kapsiotis, A.; Grammatikopoulos, T.A.; Tsikouras, B.; Hatzipanagiotou, K. Platinum-Group mineral characterization in concentrates from high-grade PGE Al-rich chromitites of Korydallos area in the Pindos ophiolite complex (NW Greece). Resour. Geol. 2010, 60, 178–191. [Google Scholar] [CrossRef]
  49. Michailidis, K.; Tarkian, M.; Bandi, A. Platinum group elements and gold (PGEs + Au) geochemistry of chromite ores from the western Chalkidiki ophiolite complex, Greece. In Proceedings of the 2nd Conference of the Committee of Economic Geology, Mineralogy and Geochemistry of the Geological Society of Greece, Thessaloniki, Greece, 7–9 October 2005; pp. 219–228.

Share and Cite

MDPI and ACS Style

Melfos, V.; Voudouris, P.C. Geological, Mineralogical and Geochemical Aspects for Critical and Rare Metals in Greece. Minerals 2012, 2, 300-317. https://doi.org/10.3390/min2040300

AMA Style

Melfos V, Voudouris PC. Geological, Mineralogical and Geochemical Aspects for Critical and Rare Metals in Greece. Minerals. 2012; 2(4):300-317. https://doi.org/10.3390/min2040300

Chicago/Turabian Style

Melfos, Vasilios, and Panagiotis Ch. Voudouris. 2012. "Geological, Mineralogical and Geochemical Aspects for Critical and Rare Metals in Greece" Minerals 2, no. 4: 300-317. https://doi.org/10.3390/min2040300

APA Style

Melfos, V., & Voudouris, P. C. (2012). Geological, Mineralogical and Geochemical Aspects for Critical and Rare Metals in Greece. Minerals, 2(4), 300-317. https://doi.org/10.3390/min2040300

Article Metrics

Back to TopTop