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Kruja Zone

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Journal Article
Published: 01 September 2006
Bulletin de la Société Géologique de France (2006) 177 (5): 249-266.
...Grigor Heba; Gilbert Prichonnet Abstract Two sections, respectively in the Kruje-Dajt and Makareshi massifs of the Kruja Zone carbonate platform (located in the Apulian passive margin of Albania), and representing a period which extends from the Late Cretaceous to the Eocene, have been studied from...
Journal Article
Published: 01 September 2009
Bulletin de la Société Géologique de France (2009) 180 (5): 431-448.
... in “the western zone” and neritic external platform in “the eastern zone”. During Paleocene and Middle-Upper Eocene times, the second phase generated new hiatus, identified throughout the Kruja-Gavrovo platform, and polygenic breccias in “the western zone” of Kulmaka massif. The difference in sedimentation...
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Series: AAPG Memoir
Published: 01 January 2004
DOI: 10.1306/M82813C25
EISBN: 9781629810485
... foreland domain in the west (Peri-Adriatic Depression and offshore), frontal thrusts and foothills structures involving the Meso-zoic series of the former Tethyan passive margin (Kruja and Krasta Zones in the north, inverted Ionian Basin in the south), as well as an ophiolitic suture, well preserved...
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Journal Article
Journal: Geosphere
Published: 01 August 2005
Geosphere (2005) 1 (1): 1-22.
... of the Paleogene basins is interpreted to be related to trench rollback along the northern Hellenic trench and lateral spreading of thick hot crust within an arc. The short period of early Neogene shortening is related to the arrival of the small continental Kruja fragment at the subduction zone in Albania...
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Journal Article
Journal: AAPG Bulletin
Published: 01 September 1999
AAPG Bulletin (1999) 83 (9): 1408-1425.
... ). The external Albanides consist of the Kruja, Ionian, and Sazani zones. These zones are characterized by Mesozoic–Cenozoic strata thrust westward onto the Apulian foreland. The first compressive deformation took place in the Eocene within the Kruja zone and in the late Oligocene–Miocene in the Ionian zone...
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Image
Geological sketch-map of the Koman region. Krasta–Cukal <b>zone</b>: 1) Xhan Flysc...
Published: 01 April 2003
. Insert: tectonic sketch-map of Albania (simplified from Shallo et al. 1985 ) showing location (black rectangle) of study area. Tectonic zones: Ko: Korrab; G: Gash; M: Mirdita; K–C: Krasta–Cukal; Kr: Kruja; I: Ionian; S: Sazan; E: evaporite diapirs; A: Alps. Sh–Pe: Shkodra–Pec tectonic alignment.
Image
Heat density map of Albania. Tectonic <b>zones</b>: Al, Alps; KC, Krasta–Cukali; M...
Published: 01 October 2005
Fig. 4 Heat density map of Albania. Tectonic zones: Al, Alps; KC, Krasta–Cukali; Mi, Mirdita; Ko, Korabi; PAD, Peri-Adriatic Depression; Kr, Kruja; I, Ionic; S, Sazani.
Image
(A) Tectonic <b>zones</b> of the Albanides (modified from the  Ministry of Mineral...
Published: 01 August 2006
Albanides showing thrust sheets and their lithology (undifferentiated). (D) Representative idealized stratigraphic sections for the Kruja and Ionian zones (modified from Flores et al., 1991 ; van Geet et al., 2002 ).
Image
—Tectonic map of the Albanides in Albania and Greece showing all major fold...
Published: 01 September 1999
Figure 11 —Tectonic map of the Albanides in Albania and Greece showing all major fold axial traces and major thrust faults in the Ionian and Kruja zones. Data from Industrial and Mining Research Institute (1983) and in Greece after Karakitsios (1995) .
Journal Article
Journal: Geosphere
Published: 01 December 2008
Geosphere (2008) 4 (6): 919-938.
... Greece, and northwestern Turkey. Extensional tectonism began during the final convergence across the Vardar, Intra-Pontide, and Izmir-Ankara suture zones, where oceanic regions closed between continental Europe and continental fragments that make up the Pelagonian, Sakar, and western Anatolian tectonic...
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Journal Article
Published: 01 June 2013
Italian Journal of Geosciences (2013) 132 (2): 203-212.
...-Sazani island offshore segment, where the Sazani Zone comprises the orogenic front; The N-trending Frakulla-Durresi mainly onshore segment, where Ionian zone makes up this orogenic front, and The WNW-trending Lezha-Ulqini segment, where the orogenic front is composed of the Kruja Zone. Fig...
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Series: Geological Society, London, Special Publications
Published: 01 January 2006
DOI: 10.1144/GSL.SP.2006.260.01.23
EISBN: 9781862395084
... reappears some 60 km east of the Kruja thrust. The Ionian Zone is over-thrust by the Kruja unit, corresponding to the Greek Gavrovo and Dalmatian zones ( Meço & Aliaj 2000 ; Robertson & Shallo 2000 ). This unit is characterized by Mid—Upper Cretaceous platform carbonates, Upper Cretaceous...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 2006
AAPG Bulletin (2006) 90 (8): 1227-1249.
... Albanides showing thrust sheets and their lithology (undifferentiated). (D) Representative idealized stratigraphic sections for the Kruja and Ionian zones (modified from Flores et al., 1991 ; van Geet et al., 2002 ). ...
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Series: Geological Society, London, Special Publications
Published: 01 January 2006
DOI: 10.1144/GSL.SP.2006.260.01.12
EISBN: 9781862395084
... , which follows the tectonic zones outlined by Meco & Aliaj (2000 ). The tectonic zones located west and NW of the Albanian (Mirdita) ophiolites comprise a westward-directed stack of thrust sheets related to the Apulian continental platform. The Sazani and the Kruja zones represent the carbonate...
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Journal Article
Published: 01 June 2013
Italian Journal of Geosciences (2013) 132 (2): 228-235.
... the Sazani (Pre-Apulian), Kruja and Ionian zones. The Ionian zone is situated in the footwall of the major west-directed Pindus thrust fault, and has been defined based on different sedimentary facies of exposed Mesozoic and Cainozoic rocks as well as on different tectonic styles. It is composed of carbonate...
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Journal Article
Published: 01 April 2003
The Canadian Mineralogist (2003) 41 (2): 413-427.
... . Insert: tectonic sketch-map of Albania (simplified from Shallo et al. 1985 ) showing location (black rectangle) of study area. Tectonic zones: Ko: Korrab; G: Gash; M: Mirdita; K–C: Krasta–Cukal; Kr: Kruja; I: Ionian; S: Sazan; E: evaporite diapirs; A: Alps. Sh–Pe: Shkodra–Pec tectonic alignment. ...
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Journal Article
Journal: AAPG Bulletin
Published: 01 September 2002
AAPG Bulletin (2002) 86 (9): 1673-1694.
... results in thrust faults, which propagate through deformation zones on the frontlimb and possibly the backlimb. The faults may terminate both up and down section within brittle or ductile deformation zones. Eventually, a throughgoing fault connects one of the major faults with the basal detachment...
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Image
Figure 12. Tectonic setting of the Macedonia-Albania region during late Pal...
in > Geosphere
Published: 01 August 2005
Figure 12. Tectonic setting of the Macedonia-Albania region during late Paleogene time. Tectonic elements active during this time and mentioned in text are shown. Location of Vardar zone is shown by gray shading. In Bulgaria, major faults are shown in red, normal faults by rectangles, and thrust
Image
Geological map of western Greece and adjacent regions. (1) internal Albanid...
Published: 09 July 2013
Figure 1. Geological map of western Greece and adjacent regions. (1) internal Albanides, (2) internal Helenides, (3) Pindos Zone (Krasta), (4) Gavrovo Zone (Kruja), (5a) internal Ionian Zone, (5b) middle Ionian Zone, (5c) external Ionian Zone, (6) Apulian platform
Image
Location of thrust faults (red barbed lines), normal faults (red lines with...
in > Geosphere
Published: 01 December 2008
). Accreted deep-water strata along the north Hellenic trench (blue) and the accreted Kruja continental fragment (yellow) are shown in Albania. The age of the structures in the Thrace basin (TB) and southeastern Bulgaria are poorly known, and their age is bracketed only between late Oligocene–early Miocene