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northeastern Greece

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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 15 June 2018
Lithosphere (2018) 10 (5): 582–601.
...Rebecca J. Perkins; Frances J. Cooper; Daniel J. Condon; Brian Tattitch; Jonathan Naden Abstract The Maronia Magmatic Corridor is a NE-trending belt of Oligocene plutons that intrudes the Kechros Dome of the northern Rhodope Core Complex in northeastern Greece. The post-collisional magmatism...
FIGURES | View All (10)
Journal Article
Journal: GSA Bulletin
Published: 01 September 1998
GSA Bulletin (1998) 110 (9): 1208–1230.
...David A. Dinter Abstract The Rhodope metamorphic core complex, exposed beneath the Strymon Valley detachment in northeastern Greece, comprises a platform carbonate sequence >5000 m thick intruded by Tertiary calc-alkaline plutons. The final thickening of the north Aegean Alpine collisional...
Journal Article
Journal: Geology
Published: 01 March 1994
Geology (1994) 22 (3): 283–285.
Journal Article
Journal: Geology
Published: 01 January 1993
Geology (1993) 21 (1): 45–48.
...-angle normal fault—similar to those widely known in core complex settings of the U.S. Basin and Range province—for more than 150 km along strike, from the Aegean Sea coast in northeastern Greece northward into the Struma Valley of southern Bulgaria. Hanging-wall rocks in the Strymon Valley detachment...
Journal Article
Published: 01 July 1981
Canadian Journal of Earth Sciences (1981) 18 (7): 1111–1126.
...Damian Nance Abstract Continental metamorphic rocks and ophiolitic bodies within the Pelagonian zone of the Hellenides in the Livadi area, northeastern Greece, show repeated periods of deformation that accompany thermal events of Early Cretaceous and possibly Late Eocene age. Structures associated...
Image
Simplified regional geologic map of northeastern Greece, modified after Kydonakis et al. (2014), showing the major tectonic units described in the text. The Strymon Valley and Kerdilion detachment faults were adapted from Dinter (1998) and Brun and Sokoutis (2007), respectively. The location of the Athos-Volvi suture zone is after Himmerkus et al. (2005).
Published: 01 November 2019
Fig. 1. Simplified regional geologic map of northeastern Greece, modified after Kydonakis et al. (2014) , showing the major tectonic units described in the text. The Strymon Valley and Kerdilion detachment faults were adapted from Dinter (1998) and Brun and Sokoutis (2007) , respectively
Image
Simplified regional geologic map of northeastern Greece modified after Kydonakis et al. (2014). The Maritza fault lies outside of the figure area and only the tectonic units referenced in the text are displayed. The Strymon Valley detachment fault and the Kavala-Komotini fault are after Dinter (1998), the Thasos detachment fault is after Wawrzenitz and Krohe (1998), and the Kerdilion detachment fault is adapted from Brun and Sokoutis (2007). Inset shows map location.
Published: 01 March 2018
Fig. 1. Simplified regional geologic map of northeastern Greece modified after Kydonakis et al. (2014) . The Maritza fault lies outside of the figure area and only the tectonic units referenced in the text are displayed. The Strymon Valley detachment fault and the Kavala-Komotini fault are after
Journal Article
Published: 04 March 2024
Mineralogical Magazine (2024) 88 (3): 218–227.
...Cristian Biagioni; Panagiotis Voudouris; Yves Moëlo; Jiří Sejkora; Zdeněk Dolníček; Silvia Musetti; Daniela Mauro Abstract Watanabeite from the Pefka epithermal deposit, northeastern Greece, was examined using single-crystal X-ray diffraction and electron microprobe analysis. The empirical formula...
FIGURES | View All (6)
Journal Article
Journal: Geology
Published: 01 October 2009
Geology (2009) 37 (10): 887–890.
... circulation in the North Atlantic. Model simulations and available proxy data suggest that it was strongest in the high to middle latitudes around the North Atlantic. Based on new pollen data from Tenaghi Philippon, northeastern Greece, we provide evidence for a massive climate-induced turnover in terrestrial...
FIGURES
Journal Article
Published: 30 January 2023
Geological Magazine (2023) 160 (1): 198–205.
...Nikolay Bonev; Zornitsa Dotseva; Massimo Chiaradia Abstract We report on the isotopic compositions of the Jurassic supra-subduction zone Evros ophiolite mafic rocks exposed in the eastern Circum-Rhodope Belt of northeastern Greece. These mafic units consist of low-Ti gabbroic and basaltic rocks...
FIGURES
Journal Article
Published: 01 April 2013
The Canadian Mineralogist (2013) 51 (2): 253–284.
...±Au system that is derived from rocks transitional between calc-alkalic and alkalic porphyries. Its similarity with other Re-Au enriched porphyry-style deposits in northeastern Greece indicates that this area may represent a new Au-Re-Te metallogenetic province. § Corresponding author: E...
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Image
A modern house built using clinoptilolite-rich tuff blocks in Metaxades, northeastern Greece.
Published: 01 January 2001
Figure 7. A modern house built using clinoptilolite-rich tuff blocks in Metaxades, northeastern Greece.
Image
A modern church built using clinoptilolite-rich tuff blocks in Metaxades, northeastern Greece.
Published: 01 January 2001
Figure 8. A modern church built using clinoptilolite-rich tuff blocks in Metaxades, northeastern Greece.
Image
Regional tectonic map for the Late Cretaceous–Paleocene deformation within the Balkan orogen. The structures of the fold-thrust belt are the same as those in Figure 10, accompanied by the regions in the Rhodope of Bulgaria and northeastern Greece, where shortening structures of the same age are shown in red. Large areas of the Rhodope and related metamorphic rocks are shown in gray, but structures of Late Cretaceous–Paleocene age (red) within this area are poorly constrained. This is the time when the oceanic region in Vardar zone and its eastern continuation in the Intrapontide zone (IPS) were closing along a north-dipping subduction zone and the fold-thrust belt in northern Bulgaria was antithetic to the subduction. The Balkan orogen at this time was convergent, and shortening across its entire width. AD—Arda dome, KD—Kardamos dome, KeD—Kechros dome, N—Nestos thrust. Light blue are the outlines of major tectonic units as shown in Figure 1. Light green lines are the limits of the Vardar zone in Macedonia and Greece.
Published: 01 April 2015
Figure 16. Regional tectonic map for the Late Cretaceous–Paleocene deformation within the Balkan orogen. The structures of the fold-thrust belt are the same as those in Figure 10 , accompanied by the regions in the Rhodope of Bulgaria and northeastern Greece, where shortening structures
Image
(a,b) Location of the EUROSEISTEST site within the Mygdonian basin in northeastern Greece; (c) total sediment thickness in the basin; thicknesses of (d) shallow layer 1 in the 3D model, (e) layer 2, and (f) deep layer 3 (see Table 2). Note the strong lateral variations and the asymmetries between the northern and southern edges, as well as between the western and eastern sides. The location of the EUROSEISTEST accelerometric array is represented by the purple triangles. The central accelerometric site TST appears as a saddle point, with a maximum of sediment thickness along a north–south profile and a minimum along an east–west profile.
Published: 19 May 2015
Figure 1. (a,b) Location of the EUROSEISTEST site within the Mygdonian basin in northeastern Greece; (c) total sediment thickness in the basin; thicknesses of (d) shallow layer 1 in the 3D model, (e) layer 2, and (f) deep layer 3 (see Table  2 ). Note the strong lateral variations
Image
Figure2—Crusafontina endemica. 1–14, from Masía del Barbo 2A-B and Puente Minero 2, 8, Teruel Basin, northeast-central Spain; 15–21, from Can Llobateres 1, Vallès-Penedès Basin, northeastern Spain; Crusafontina cf. endemicaGibert, 1975; 22, from Biodrak, Greece; Crusafontina cf. kormosi Bachmeyer and Wilson, 1970; 23, 24, from Lefkon 1, Strimon Basin, northeastern Greece. 1, right P4, buccal part, PM8 41; 2, right P4, lingual part, PM8 42; 3, left M1, PM2 151; 4, left M2, PM2 157; 5, left M3, PM2 160; 6, left A2, MBB 3006; 7, right A1, MBA 2010; 8, right a1, MBA 2014; 9, left a1, MBB 3009; 10, right p4, MBA 2015; 11, right m1, MBA 2018; 12, right m2, PM2 171; 13, right m3, PM2 178; 14, right m1, PM2 163; 15, right m1 in buccal view, PM2 163; 16, right P4, CL1 1017; 17 left a1, CL1 1061; 18, right p4, CL1 1066; 19, left A1, CL1 1001; 20, left A1, CL1 1005; 21, left m3, occlusal-buccal view, CL1 2257; 22, right M2, CL1 1053; 23, left m1, BDB 501; 24, right m1, LE1 201; 25, right m2, LE1 202. Enlargement ×19
Published: 01 July 2004
Figure 2 — Crusafontina endemica . 1–14, from Masía del Barbo 2A-B and Puente Minero 2, 8, Teruel Basin, northeast-central Spain; 15–21, from Can Llobateres 1, Vallès-Penedès Basin, northeastern Spain; Crusafontina cf. endemica Gibert, 1975 ; 22, from Biodrak, Greece; Crusafontina
Journal Article
Published: 01 April 1994
Journal of the Geological Society (1994) 151 (2): 413–415.
... in northeastern Greece: Strymon valley detachment system and Rhodope metamorphic core complex Geology 1993 21 45 48 Eleftheriades G. Lippolt H. I. Alterbestimmungen zum oligozanen Vulkanismus der Siid-Rhodopen, Nord-Grieehenland Neues Jahrbuch für Geologie und Paleontologie Mittabteilung...
Journal Article
Journal: Geophysics
Published: 11 June 2015
Geophysics (2015) 80 (4): EN105–EN117.
...George Apostolopoulos; Despina Minos-Minopoulos; Kosmas Pavlopoulos ABSTRACT The area of Lechaion located in the northeastern part of the Peloponnese (Greece) is of great archaeological interest because it represents the western harbor of ancient Corinth and includes the remains of an early...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1961
AAPG Bulletin (1961) 45 (7): 1090–1142.
... with the Po basin gas fields, and an important discovery of gas was made at Ravenna mare. A gas-condensate discovery was made in northeastern Sicily. In The Netherlands production in the western part of the country exceeded for the first time that from the Schoonebeek field in the east. Additional exploratory...
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Journal Article
Published: 01 October 2009
The Canadian Mineralogist (2009) 47 (5): 1013–1036.
.... Geological and geochemical comparisons will be made with the rheniite- and rhenian-molybdenite-bearing sublimates of active fumaroles at Kudriavy volcano ( Korzhinsky et al. 1994 , 1996 , Yudovskaya et al. 2006 ). Porphyry and epithermal prospects in northeastern Greece formed in the Tertiary...
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