2017
DOI: 10.12681/bgsg.11423
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Development of Lignite in Crete. Comparison of Basins, Possibilities of Exploitation

Abstract: The island of Crete has been thoroughly explored, by various organizations

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Cited by 2 publications
(3 citation statements)
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“…The absence of these characteristic aromatic biomarkers from the vast majority of the calculus samples, and their co-occurrence specifically in the PAH-rich calculus samples, excludes exogenous, pre- or post-excavation, contamination as a possible source. The presence of these biomarkers is particularly significant since Greece has important lignite deposits, all of which are surface deposits mined as opencast resources 30 34 , which would also have made them visible to ancient populations. The main lignite deposits were formed in intermountain basins such as Ptolemais in Macedonia and Megalopolis in the central Peloponnese, while smaller lignite deposits were created in the western Peloponnese at sites such as Olympia and Pyrgos 30 , 31 as well as in Kandanos and Vrysses Apokoronou in western Crete 33 , 34 .…”
Section: Resultsmentioning
confidence: 99%
See 1 more Smart Citation
“…The absence of these characteristic aromatic biomarkers from the vast majority of the calculus samples, and their co-occurrence specifically in the PAH-rich calculus samples, excludes exogenous, pre- or post-excavation, contamination as a possible source. The presence of these biomarkers is particularly significant since Greece has important lignite deposits, all of which are surface deposits mined as opencast resources 30 34 , which would also have made them visible to ancient populations. The main lignite deposits were formed in intermountain basins such as Ptolemais in Macedonia and Megalopolis in the central Peloponnese, while smaller lignite deposits were created in the western Peloponnese at sites such as Olympia and Pyrgos 30 , 31 as well as in Kandanos and Vrysses Apokoronou in western Crete 33 , 34 .…”
Section: Resultsmentioning
confidence: 99%
“…The presence of these biomarkers is particularly significant since Greece has important lignite deposits, all of which are surface deposits mined as opencast resources 30 34 , which would also have made them visible to ancient populations. The main lignite deposits were formed in intermountain basins such as Ptolemais in Macedonia and Megalopolis in the central Peloponnese, while smaller lignite deposits were created in the western Peloponnese at sites such as Olympia and Pyrgos 30 , 31 as well as in Kandanos and Vrysses Apokoronou in western Crete 33 , 34 . Lignite chemistry reflects the plant input of their formation, which can thereby provide clues to potential sources.…”
Section: Resultsmentioning
confidence: 99%
“…Amyntaio (Am; [7,16]; Dimitras (D; [17]). Kastoria (K; [13]), Lavas-Servion (LS; [18]), Prosilio (P; [19,20]) and Ptolemais (Pt; [21,22]).…”
Section: Classification and Geochemical Features Of Fly Ashesmentioning
confidence: 99%