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  • Research - Τμήμα Γεωλογίας Σχολή Θετικών Επιστημών, Department of Geology, University of Patras

Coal-forming conditions prevailed in Greece since the onset of the Cenozoic era. Thin benches of Permo-Carboniferous hard coal occur in the coastal sediments of Chios Island (#27), on Central Evia (#16) and in Monemvasia (SE Peloponnese; #24).

Thin beds of sapropelic and subbituminous coals occur in the Eocene flysch in the western part of the country, as well as in the molasse of Thrace (#1 and 2). They formed mainly in paralic basins under estuarine or deltaic conditions. Similar conditions prevailed during Oligocene, when thin coal-bearing layers formed in the molasse sediments of the Middle Hellenic trough (#11), as well as in Thrace. Moreover, there are a few coal beds of lacustrine-fluvial origin in eastern Macedonia and Thrace. The Eocene and Oligocene coals generally show high calorific values, but their reserves are limited and thus, exploitation is not profitable.

The intense post-alpine faulting tectogenesis during Neogene and Quaternary times, caused the formation of many intermontane and paralic basins. The sedimentary filling of the basins contains lignite to subbituminous coals, which accumulated in topogenous mires (fens) due to terrestrialization of lakes and/or paludification. In the Miocene, lignite deposits formed in Vevi, Achlada and Lofi in the Florina basin (#6); in Vegora and Komnina in the Ptolemais basin (#7); and in Moschopotamos (#10). All the aforementioned deposits derived mainly from forest swamps located in intermontane basins. The deposits of Ptolemais, Amyntaeo, Lava-Kozani (#7), Elassona (#9), and Rhodos (#28), formed during Pliocene in fens in intermontane basins, while those of Preveza (#13) and Pyrgos-Olympias (#21) are deltaic to estuarine. All were derived from reed-sedge vegetation. Quaternary lignite deposits are these of Drama (#3), Ioannina (#12), Kandanos (#25), and Megalopolis (#23).

The Greek lignite reserves are 6.7 Gt, of which 3.9 Gt are economically recoverable. The Florina-Amyntaeo-Ptolemais-Kozani tectonic graben in western Macedonia (#6-8) includes about 2/3of the reserves. Annualy 66 Mt lignite are produced mainly for power generation.

Schematic map of Greece with the main coal deposits:

1: Orestias, 2: Alexandroupolis, 3: Drama, Kormista, Eliokomi, Proti, 4: Serres, 5: Almopia, 6: Florina basin (Vevi, Achlada, Lofi), 7: Ptolemais basin (Amyntaeo, Anargyri, Vegora, Komnina, Kariochori, Ptolemais), 8: Kozani basin (Trigoniko, Prosilio, Lava, Servia), 9: Elassona, 10: Moschopotamos, Katerini, 11: Middle Hellenic trough, 12: Ioannina, 13: Preveza, 14: Almyros, 15: Zeli, 16: Paliouras, 17: Aliveri, Kymi, 18: Biotia, 19: Attiki, 20: Kalavryta, 21: Pyrgos, Olympia, Vasilaki, 22: Chomatero-Koroni, 23: Megalopolis, 24: Monemvasia, 25: Kandanos, 26: Samos, 27: Chios, 28: Rhodos.

 

The macerals can be distinguished in three groups :

 

The Inertinite group

The Inertinite group

MACERAL GROUP MACERAL MACERAL TYPE
Ι
Ν
Ε
R
Τ
Ι
Ν
Ι
Τ
E

Fusinite

Pyrofusinite (01), (02)

Degradofusinite

Semifusinite

Macrinite

Funginite (01), (02)

Secretinite

Inertodetrinite

Micrinite


Funginite 01

Funginite 01

Funginite 02

Funginite 02

Pyrofusinite 01

Pyrofusinite 01

Pyrofusinite 02

Pyrofusinite 02

The Liptinite group

The Liptinite group

MACERAL GROUP MACERAL

L

I

P

T

I

N

I

T

E

Sporinite
Cutinite (01), (02), (03)
Resinite (01), (02), (03), (04), (05)
Suberinite
Alginite
Bituminite
Liptodetrinite
Chlorophyllinite

Cutinite 01

Cutinite 01

Cutinite 02

Cutinite 02

Cutinite 03

Cutinite 03

Resinite 01

Resinite 01

Resinite 02

Resinite 02

Resinite 03

Resinite 03

Resinite 04

Resinite 04

Resinite 05

Resinite 05

Suberinite

Suberinite

The Huminite group

The Huminite group

MACERAL GROUP

MACERAL SUB-GROUP

MACERAL

MACERAL TYPE

MACERAL VARIETY

H

U

M

N

I

T

E

Humotelinite

Textinite

A

B

Ulminite

Texto-ulminite (01), (02)

A

B

Eu-ulminite (01), (02)

A

B

Humodetrinite

Attrinite

Densinite (01), (02), (03)

Humocollinite

Gelinite

Levigelinite (01), (02)

Porigelinite

Corpohuminite (01), (02)

Phlobaphinite

Pseudophlobaphinite

In 2001, the International Committee for Coal and Organic Petrology (I.C.C.P.) τ modified the above nomenclature as follows (ICCP System 1994):

MACERAL GROUP

MACERAL SUB-GROUP

MACERAL

MACERAL TYPE

MACERAL VARIETY

H

U

M

N

I

T

E

Telohuminite

Textinite

A

B

Ulminite

A

B

Detrohuminite

Attrinite

Densinite (01), (02), (03)

Gelohuminite

Gelinite

Levigelinite (01), (02)

Porigelinite

Corpohuminite (01), (02)

Phlobaphinite

Pseudophlobaphinite


Texto-ulminite 01

Texto-ulminite 01

Texto-ulminite 02

Texto-ulminite 02

Eu-ulminite 01

Eu-ulminite 01

Eu-ulminite 02

Eu-ulminite 02

Maceral Variety A

Maceral Variety A

Attrinite

Attrinite

Densinite 01

Densinite 01

Densinite 02

Densinite 02

Densinite 03

Densinite 03

Levigelinite 01

Levigelinite 01

Levigelinite 02

Levigelinite 02

Porigelinite

Porigelinite

Corpohuminite 01

Corpohuminite 01

Corpohuminite 02

Corpohuminite 02

The Vitrinite group

The Vitrinite group

MACERAL GROUP

MACERAL

MACERAL TYPE

V

T

R

I

N

I

T

E

Telinite

Collinite

Telocollinite

Gelocollinite

Desmocollinite

Corpocollinite

Vitrodetrinite

In 1994, the International Committee for Coal and Organic Petrology I.C.C.Pmodified the vitrinite nomenclature as follows:

MACERAL GROUP

MACERAL SUB-GROUP

MACERAL

V

T

R

I

N

I

T

E

Telovitrinite

Telinite

Collotelinite

Detrovitrinite

Vitrodetrinite

Collodetrinite

Gelovitrinite

Gelinite

Corpogelinite