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Charakoma eclogite, Soufli, Evros, Eastern Macedonia and Thrace, Greecei
Regional Level Types
Charakoma eclogiteOutcrop
SoufliMunicipality
EvrosRegional Unit
Eastern Macedonia and ThraceAdministrative Region
GreeceCountry

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Latitude & Longitude (WGS84):
41° 10' 29'' North , 25° 57' 10'' East
Latitude & Longitude (decimal):
41.17500,25.95278
GRN:
N28E15
Type:
Outcrop
Age:
36 to 41 Ma
Geologic Time:
Eocene
Dating method:
39Ar-40Ar white mica ages from mylonitic orthogneisses
Reference for age:
Baziotis, I.; Mposkos, E. (2017) GEOCHEMISTRY AND TECTONIC SETTING OF ECLOGITE PROTOLITHS FROM KECHROS COMPLEX IN EAST RHODOPE (N.E. GREECE). Bulletin of the Geological Society of Greece, 43 (5). 2522-2531 doi:10.12681/bgsg.11659
Kรถppen climate type:
Csb : Warm-summer Mediterranean climate
Nearest Settlements:
PlacePopulationDistance
Roussa325 (2017)14.9km
Agiochรณri226 (2013)17.7km
Mikrรณ Dรฉreio296 (2013)19.9km
Dadรญa784 (2013)23.3km
Arrianรก1,158 (2013)24.0km
Mindat Locality ID:
458510
Long-form identifier:
mindat:1:2:458510:0
GUID (UUID V4):
0


A lensoid kyanite eclogite body (200 x 40 m) is embedded in a garnetโ€“phengite orthogneiss. The main body of the eclogite is undeformed, but at the margins, the eclogite is completely retrogressed into a foliated and lineated amphibolite. In the main eclogite body, shear zones of post-eclogitic deformation consists of garnet porphyroclasts in a fine-grained hornblende-chlorite-epidote-biotite matrix.

See also Kovalo eclogites.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


15 valid minerals.

Rock Types Recorded

Note: data is currently VERY limited. Please bear with us while we work towards adding this information!

Select Rock List Type

Alphabetical List Tree Diagram

Paragenesis


Pre-eclogite facies assemblage Mposkos et al. (2011)Edit
Albite
Paragonite
Phengite

High pressure ( eclogite facies) assemblage Mposkos et al. (2011)Edit
Garnet Group
Omphacite
Amphibole Supergroup
Kyanite
Quartz
Phengite
Zoisite
Rutile

Retrograde assemblages Mposkos et al. (2011)Edit
Amphibole Supergroup
Plagioclase
Biotite

Detailed Mineral List:

โ“˜ Albite
Formula: Na(AlSi3O8)
Description: Albite has been identified as minute inclusions in garnet cores and has been used as evidence that garnets started to grow before the Pโ€“T conditions reached eclogite facies conditions.
โ“˜ Almandine
Formula: Fe2+3Al2(SiO4)3
Habit: Porphyroblasts
Description: All analytical data of garnet group minerals in the kyanite-eclogite ( see https://www.mindat.org/locentryedit.php?min=1778747 ) corresponds with almandine
โ“˜ 'Amphibole Supergroup'
Formula: AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Description: Amphiboles occur both as prograde and retrograde minerals. It occurs as a prograde mineral in the eclogite matrix and as inclusions in garnets. Amphibole+plagioclase form retrograde symplectites after omphacite, and kelyphitic amphibole replaces garnets. Mposkos et al. (2012) describe a matrix amphibole with actinolite core overgrown by Na-rich tremolite ( corresponding better to winchite in the 2012 amphibole nomenclature) and then rimmed by omphacite + quartz, suggesting a prograde metamorphic path with successive pressure increase. Several different amphibole species has been identified in these rocks.
โ“˜ 'Biotite'
Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Description: Biotite is found as a retrograde alteration producton the rim of phengite flakes.
โ“˜ Clinozoisite
Formula: (CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
Description: Clinozoisite occurs as inclusions in garnets and as a retrogression product in the matrix.
โ“˜ 'Garnet Group'
Formula: X3Z2(SiO4)3
Description: Garnet occurs as porphyroblasts in the kyanite-eclogite. The garnet shows compositional growth zoning with increasing MgO and CaO and decreasing FeO and MnO from the core to the rim.
โ“˜ Kyanite
Formula: Al2(SiO4)O
Description: Kyanite occurs as up to 100ยตm long priems in the kyanite-eclogite matrix. The kyanite is in textural equilibrium with matrix omphacite. Kyanite also occurs as up to 15ยตm prisms inclusions in garnet.
โ“˜ Magnesio-hornblende
Formula: ◻Ca2(Mg4Al)(Si7Al)O22(OH)2
Habit: symplectite
Description: A typical amphibole occurring with plagioclase in a retrograde symplectite after omphacite, corresponds with magnesio-hornblende.
โ“˜ Muscovite
Formula: KAl2(AlSi3O10)(OH)2
โ“˜ Muscovite var. Phengite
Formula: KAl1.5(Mg,Fe)0.5(Al0.5Si3.5O10)(OH)2
Description: Phengite is a common phase with a flake size of 10โ€“50 ยตm. At the rims, it is commonly replaced by biotite.
โ“˜ Omphacite
Formula: (NaaCabFe2+cMgd)(AleFe3+fFe2+gMgh)Si2O6
Description: Fine grained omphacite form the matrix of the kyanite-eclogite. It breaks down to symplectitic aggregates of amphibole and plagioclase. Omphacite is also found as inclusions in garnet.
โ“˜ Paragonite
Formula: NaAl2(AlSi3O10)(OH)2
Description: Paragonite occurs as inclusions in the cores of the garnets, indicating that garnet started to grow before the eclogite stage
โ“˜ 'Plagioclase'
Formula: (Na,Ca)[(Si,Al)AlSi2]O8
Description: Plagioclase and amphibole symplectites replaces matrix omphacite. The plagioclase is oligoclase/andesine with An content ranging from 26 to 36%.
โ“˜ Preiswerkite
Formula: NaMg2Al(Al2Si2O10)(OH)2
Description: Preiswerkite, staurolite and phengite was identified in a single composite grain inclusion in a garnet. These minerals are probably decomposition products of a former K-bearing paragonite+chloritoid composite inclusion that reacted during decompression.
โ“˜ Quartz
Formula: SiO2
Description: Quartz is identified as inclusions in garnet.
โ“˜ Rutile
Formula: TiO2
Description: Rutile occurs as inclusions in garnets
โ“˜ Staurolite
Formula: Fe2+2Al9Si4O23(OH)
Description: Staurolite, preiswerkite and phengite was identified in a single composite grain inclusion in a garnet. These minerals are probably decomposition products of a former K-bearing paragonite+chloritoid composite inclusion that reacted during decompression.
โ“˜ Taramite
Formula: Na(CaNa)(Mg3Al2)(Al2Si6O22)(OH)2
Description: An analysis of a typical retrograde kelyphitic amphibole replacement after garnet corresponds to a taramite composition.
โ“˜ Winchite
Formula: ◻{CaNa}{Mg4Al}(Si8O22)(OH)2
Description: Mposkos et al. (2011) describe Na-rich tremolite/actinolite as the dominant amphibole in the kyanite-eclogite. It occurs as a prograde mineral formed before omphacite, as inclusions in garnet and, most commonly, as replacement of omphacite. The composition of this amphibole is intermediate between tremolite and winchite. Mposkos et al. (2011) named the amphiboles based on the Leake (1997) nomenclature report, in which the name is tremolite. Using the amphibole nomenclature report of Hawthorne et al. (2012), the composition is closest to winchite. Winchite has also been identified from inclusions in garnet.
โ“˜ Zoisite
Formula: (CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
Description: The kyanite-eclogite contains 2-3 modal% zoisite, presumable formed at near peak conditions.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 4 - Oxides and Hydroxides
โ“˜Quartz4.DA.05SiO2
โ“˜Rutile4.DB.05TiO2
Group 9 - Silicates
โ“˜Almandine9.AD.25Fe2+3Al2(SiO4)3
โ“˜Kyanite9.AF.15Al2(SiO4)O
โ“˜Staurolite9.AF.30Fe2+2Al9Si4O23(OH)
โ“˜Clinozoisite9.BG.05a(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
โ“˜Zoisite9.BG.10(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
โ“˜Omphacite9.DA.20(NaaCabFe2+cMgd)(AleFe3+fFe2+gMgh)Si2O6
โ“˜Magnesio-hornblende9.DE.10โ—ปCa2(Mg4Al)(Si7Al)O22(OH)2
โ“˜Winchite9.DE.20โ—ป{CaNa}{Mg4Al}(Si8O22)(OH)2
โ“˜Taramite9.DE.20Na(CaNa)(Mg3Al2)(Al2Si6O22)(OH)2
โ“˜Muscovite9.EC.15KAl2(AlSi3O10)(OH)2
โ“˜Paragonite9.EC.15NaAl2(AlSi3O10)(OH)2
โ“˜Muscovite
var. Phengite		9.EC.15KAl1.5(Mg,Fe)0.5(Al0.5Si3.5O10)(OH)2
โ“˜Preiswerkite9.EC.20NaMg2Al(Al2Si2O10)(OH)2
โ“˜Albite9.FA.35Na(AlSi3O8)
Unclassified
โ“˜'Amphibole Supergroup'-AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
โ“˜'Biotite'-K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
โ“˜'Plagioclase'-(Na,Ca)[(Si,Al)AlSi2]O8
โ“˜'Garnet Group'-X3Z2(SiO4)3

List of minerals for each chemical element

HHydrogen
Hโ“˜ Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Hโ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Hโ“˜ Clinozoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
Hโ“˜ Magnesio-hornblende◻Ca2(Mg4Al)(Si7Al)O22(OH)2
Hโ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Hโ“˜ ParagoniteNaAl2(AlSi3O10)(OH)2
Hโ“˜ Muscovite var. PhengiteKAl1.5(Mg,Fe)0.5(Al0.5Si3.5O10)(OH)2
Hโ“˜ PreiswerkiteNaMg2Al(Al2Si2O10)(OH)2
Hโ“˜ StauroliteFe22+Al9Si4O23(OH)
Hโ“˜ Winchite◻{CaNa}{Mg4Al}(Si8O22)(OH)2
Hโ“˜ Zoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
Hโ“˜ TaramiteNa(CaNa)(Mg3Al2)(Al2Si6O22)(OH)2
OOxygen
Oโ“˜ AlbiteNa(AlSi3O8)
Oโ“˜ Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Oโ“˜ AlmandineFe32+Al2(SiO4)3
Oโ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Oโ“˜ Clinozoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
Oโ“˜ KyaniteAl2(SiO4)O
Oโ“˜ Magnesio-hornblende◻Ca2(Mg4Al)(Si7Al)O22(OH)2
Oโ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Oโ“˜ Omphacite(NaaCabFec2+Mgd)(AleFef3+Feg2+Mgh)Si2O6
Oโ“˜ ParagoniteNaAl2(AlSi3O10)(OH)2
Oโ“˜ Muscovite var. PhengiteKAl1.5(Mg,Fe)0.5(Al0.5Si3.5O10)(OH)2
Oโ“˜ PreiswerkiteNaMg2Al(Al2Si2O10)(OH)2
Oโ“˜ QuartzSiO2
Oโ“˜ RutileTiO2
Oโ“˜ StauroliteFe22+Al9Si4O23(OH)
Oโ“˜ Winchite◻{CaNa}{Mg4Al}(Si8O22)(OH)2
Oโ“˜ Zoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
Oโ“˜ TaramiteNa(CaNa)(Mg3Al2)(Al2Si6O22)(OH)2
Oโ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Oโ“˜ Garnet GroupX3Z2(SiO4)3
FFluorine
Fโ“˜ Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Fโ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
NaSodium
Naโ“˜ AlbiteNa(AlSi3O8)
Naโ“˜ Omphacite(NaaCabFec2+Mgd)(AleFef3+Feg2+Mgh)Si2O6
Naโ“˜ ParagoniteNaAl2(AlSi3O10)(OH)2
Naโ“˜ PreiswerkiteNaMg2Al(Al2Si2O10)(OH)2
Naโ“˜ Winchite◻{CaNa}{Mg4Al}(Si8O22)(OH)2
Naโ“˜ TaramiteNa(CaNa)(Mg3Al2)(Al2Si6O22)(OH)2
Naโ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
MgMagnesium
Mgโ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Mgโ“˜ Magnesio-hornblende◻Ca2(Mg4Al)(Si7Al)O22(OH)2
Mgโ“˜ Omphacite(NaaCabFec2+Mgd)(AleFef3+Feg2+Mgh)Si2O6
Mgโ“˜ Muscovite var. PhengiteKAl1.5(Mg,Fe)0.5(Al0.5Si3.5O10)(OH)2
Mgโ“˜ PreiswerkiteNaMg2Al(Al2Si2O10)(OH)2
Mgโ“˜ Winchite◻{CaNa}{Mg4Al}(Si8O22)(OH)2
Mgโ“˜ TaramiteNa(CaNa)(Mg3Al2)(Al2Si6O22)(OH)2
AlAluminium
Alโ“˜ AlbiteNa(AlSi3O8)
Alโ“˜ Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Alโ“˜ AlmandineFe32+Al2(SiO4)3
Alโ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Alโ“˜ Clinozoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
Alโ“˜ KyaniteAl2(SiO4)O
Alโ“˜ Magnesio-hornblende◻Ca2(Mg4Al)(Si7Al)O22(OH)2
Alโ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Alโ“˜ Omphacite(NaaCabFec2+Mgd)(AleFef3+Feg2+Mgh)Si2O6
Alโ“˜ ParagoniteNaAl2(AlSi3O10)(OH)2
Alโ“˜ Muscovite var. PhengiteKAl1.5(Mg,Fe)0.5(Al0.5Si3.5O10)(OH)2
Alโ“˜ PreiswerkiteNaMg2Al(Al2Si2O10)(OH)2
Alโ“˜ StauroliteFe22+Al9Si4O23(OH)
Alโ“˜ Winchite◻{CaNa}{Mg4Al}(Si8O22)(OH)2
Alโ“˜ Zoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
Alโ“˜ TaramiteNa(CaNa)(Mg3Al2)(Al2Si6O22)(OH)2
Alโ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
SiSilicon
Siโ“˜ AlbiteNa(AlSi3O8)
Siโ“˜ Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Siโ“˜ AlmandineFe32+Al2(SiO4)3
Siโ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Siโ“˜ Clinozoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
Siโ“˜ KyaniteAl2(SiO4)O
Siโ“˜ Magnesio-hornblende◻Ca2(Mg4Al)(Si7Al)O22(OH)2
Siโ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Siโ“˜ Omphacite(NaaCabFec2+Mgd)(AleFef3+Feg2+Mgh)Si2O6
Siโ“˜ ParagoniteNaAl2(AlSi3O10)(OH)2
Siโ“˜ Muscovite var. PhengiteKAl1.5(Mg,Fe)0.5(Al0.5Si3.5O10)(OH)2
Siโ“˜ PreiswerkiteNaMg2Al(Al2Si2O10)(OH)2
Siโ“˜ QuartzSiO2
Siโ“˜ StauroliteFe22+Al9Si4O23(OH)
Siโ“˜ Winchite◻{CaNa}{Mg4Al}(Si8O22)(OH)2
Siโ“˜ Zoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
Siโ“˜ TaramiteNa(CaNa)(Mg3Al2)(Al2Si6O22)(OH)2
Siโ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Siโ“˜ Garnet GroupX3Z2(SiO4)3
ClChlorine
Clโ“˜ Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
KPotassium
Kโ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Kโ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Kโ“˜ Muscovite var. PhengiteKAl1.5(Mg,Fe)0.5(Al0.5Si3.5O10)(OH)2
CaCalcium
Caโ“˜ Clinozoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
Caโ“˜ Magnesio-hornblende◻Ca2(Mg4Al)(Si7Al)O22(OH)2
Caโ“˜ Omphacite(NaaCabFec2+Mgd)(AleFef3+Feg2+Mgh)Si2O6
Caโ“˜ Winchite◻{CaNa}{Mg4Al}(Si8O22)(OH)2
Caโ“˜ Zoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
Caโ“˜ TaramiteNa(CaNa)(Mg3Al2)(Al2Si6O22)(OH)2
Caโ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
TiTitanium
Tiโ“˜ Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Tiโ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Tiโ“˜ RutileTiO2
FeIron
Feโ“˜ AlmandineFe32+Al2(SiO4)3
Feโ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Feโ“˜ Omphacite(NaaCabFec2+Mgd)(AleFef3+Feg2+Mgh)Si2O6
Feโ“˜ Muscovite var. PhengiteKAl1.5(Mg,Fe)0.5(Al0.5Si3.5O10)(OH)2
Feโ“˜ StauroliteFe22+Al9Si4O23(OH)

Other Regions, Features and Areas containing this locality

Eurasian PlateTectonic Plate
EuropeContinent

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References

Mposkos, E.; Baziotis, I.; Proyer, A. (2011) Pressureโ€“temperature evolution of eclogites from the Kechros complex in the Eastern Rhodope (NE Greece). International Journal of Earth Sciences, 101 (4). 973-996 doi:10.1007/s00531-011-0699-2
Baziotis, I.; Mposkos, E. (2017) GEOCHEMISTRY AND TECTONIC SETTING OF ECLOGITE PROTOLITHS FROM KECHROS COMPLEX IN EAST RHODOPE (N.E. GREECE). Bulletin of the Geological Society of Greece, 43 (5). 2522-2531 doi:10.12681/bgsg.11659
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