Zobrazeno 1 - 10
of 55
pro vyhledávání: '"K. St. Seymour"'
Publikováno v:
Tectonophysics. 674:1-19
Exposure of the forearc region of the North Aegean Sea, Greece, offers insight into evolving convergent margins. The sedimentary fill of the Thrace Basin during the Late Eocene to Oligocene time provides a record of subduction-driven processes, such
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e5edddc1e62c542dd3d4b27ae488033f
https://doi.org/10.1016/j.tecto.2016.02.003
https://doi.org/10.1016/j.tecto.2016.02.003
Autor:
Dimitrios Zouzias, K. St. Seymour
Publikováno v:
Δελτίο της Ελληνικής Γεωλογικής Εταιρείας; Τόμ. 40 Αρ. 1 (2007): 11o διεθνές Συνέδριο της ΕΓΕ; 512-522
Bulletin of the Geological Society of Greece; Vol. 40 No. 1 (2007): 11th International Conference of the Geological Society of Greece; 512-522
Bulletin of the Geological Society of Greece; Vol. 40 No. 1 (2007): 11th International Conference of the Geological Society of Greece; 512-522
Στην αμοιβαία σχέση ηφαιστειότητας και τεκτονικής έχει εστιαστεί η προσοχή των ερευνητών την τελευταία δεκαετία λόγω του αυξανομένου ό
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::58e482bb76f26819d5a27f40467b29e9
https://doi.org/10.12681/bgsg.16660
https://doi.org/10.12681/bgsg.16660
Publikováno v:
Environmental Earth Sciences. 62:717-723
The Hellenic Peninsula and the adjacent Aegean and Ionian seas are segmented into regions on the basis of Terra satellite-MODIS instrument derived land surface temperatures (LST) to test if they can be used in the field reconnaissance for potential g
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::071609da175dfe1e41f511eaffabc02c
https://doi.org/10.1007/s12665-010-0560-0
https://doi.org/10.1007/s12665-010-0560-0
Publikováno v:
Mineralogy and Petrology. 94:175-194
Precious metals accompany all types of epithermal deposits. In general, the largest of these deposits occur in intrusive or extrusive rocks of alkaline or calc-alkaline affinity. The Apigania Bay vein system and Au–Ag mineralization is hosted in Me
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d73b4cfac0323691e3be238ad789783c
https://doi.org/10.1007/s00710-008-0019-0
https://doi.org/10.1007/s00710-008-0019-0
Autor:
Maria Kouli, K. St. Seymour, R. Mavrantza, Georges Dénès, H. Paraskevas, I. Karfakis, S. Lamera, D. Rokos, Demetre Argialas, C. Vamvoukakis
Publikováno v:
Natural Resources Research. 9:277-293
Exploration for epithermal Au has been active lately in the Aegean Sea of the eastern Mediterranean Basin, both in the islands of the Quaternary arc and in those of the back-arc region. The purpose of this study was the structural mapping and analysi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ce3c510be4605b164997dac44f9f40a8
https://doi.org/10.1023/a:1011505326148
https://doi.org/10.1023/a:1011505326148
Publikováno v:
Mineralogy and Petrology. 56:251-272
The island of Samothrace, northeastern Aegean Sea, consists of five main geological units: (i) A basement unit consisting of low grade metamorphic rocks (metapelites, marbles, metavolcanic rocks, and a metaconglomerate); (ii) an ‘ophiolitic complex
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::838ce648b3d52cc7e495c7982d23dfdd
https://doi.org/10.1007/bf01162606
https://doi.org/10.1007/bf01162606
Spectro-imaging and radar measurements by the Cassini-Huygens mission suggest that some of the Saturnian satellites may be geologically active and could support tectonic processes. In particular Titan, Saturn's largest moon, possesses a complex and d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2127::c5a5608de86665d15a9d46caaa271991
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3070330
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3070330
Autor:
Stylianos Tombros, K. St. Seymour
Publikováno v:
Δελτίο της Ελληνικής Γεωλογικής Εταιρείας; Τόμ. 40 Αρ. 2 (2007): 11o διεθνές Συνέδριο της ΕΓΕ; 996-1008
Bulletin of the Geological Society of Greece; Vol. 40 No. 2 (2007): 11th International Conference of the Geological Society of Greece; 996-1008
Bulletin of the Geological Society of Greece; Vol. 40 No. 2 (2007): 11th International Conference of the Geological Society of Greece; 996-1008
Τα κοιτάσματα Cu-Te σιδηροπυρίτη της Ερμιόνης, Αργολίδας φιλοξενούνται σε οφιόλιθους Μειοκαινικής ηλικίας. Οι οφιόλιθοι υπόκεινται σε έν
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d0e7c9e8fa32eb38727f81986ecbd918
https://ejournals.epublishing.ekt.gr/index.php/geosociety/article/view/16782
https://ejournals.epublishing.ekt.gr/index.php/geosociety/article/view/16782
The island of Lesvos, located in the northeastern Aegean, just offshore Asia Minor, is mostly covered by Miocene calkalkaline, and predominantly shoshonitic volcanic products. Pyroclastic deposits are voluminous, indicating intense explosive activity
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5f2c48ac1a26f884e16098de27d513f7
https://doi.org/10.1016/s1871-644x(05)80048-8
https://doi.org/10.1016/s1871-644x(05)80048-8
Publikováno v:
Δελτίο της Ελληνικής Γεωλογικής Εταιρείας; Τόμ. 34 Αρ. 3 (2001): 9o διεθνές Συνέδριο της ΕΓΕ; 917-921
Bulletin of the Geological Society of Greece; Vol. 34 No. 3 (2001): 9th International Conference of the Geological Society of Greece; 917-921
Bulletin of the Geological Society of Greece; Vol. 34 No. 3 (2001): 9th International Conference of the Geological Society of Greece; 917-921
Miocene volcanism on Lesvos was particularly explosive giving rise to two extensive pyroclastic formations, the Sigri pyroclastics to the west and the Polychnitos ignimbrite to the east of the island. The Polychnitos ignimbrite at 17.2±0.5 Ma (Borsi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7c711cf34db1a7ec71cee0ed47545172
https://ejournals.epublishing.ekt.gr/index.php/geosociety/article/view/17118
https://ejournals.epublishing.ekt.gr/index.php/geosociety/article/view/17118