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Misis-Andirin Range

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Image
(A) Geology map of the <b>Andırın</b> region (the map location in  Fig. 10A ). The...
Published: 11 March 2021
the MisisAndırın Range. The arrows of WB and EB show the axes of the western and eastern belts (modified after Yılmaz and Gürer 1996 , fig. 2). (B) Schematic geological cross-section along direction indicated in Fig. 11A , showing structural positions and ordering of the major rock units within tectonic
Image
(A) Tectonic map of Anatolia and the surrounding showing locations of Cypru...
Published: 11 March 2021
Latakia–Antakya link; DSF, Dead Sea Fault zone; EF, Ecemiş Fault; Eratos SM, Eratosthenes sea mount; Kyrenia R, Kyrenia Range; KMAF, Kyrenia/Misis/Andırın Fault; KZO, Kızıldağ Ophiolite; LAR, Latakia Ridge; LB, Latakia Basin; LR, Larnaca Ridge; Lt, Latakia city; Mam, Mammonia region; MB, Mesoria Basin
Journal Article
Published: 11 March 2021
Canadian Journal of Earth Sciences (2021) 58 (7): 640–657.
... the MisisAndırın Range. The arrows of WB and EB show the axes of the western and eastern belts (modified after Yılmaz and Gürer 1996 , fig. 2). (B) Schematic geological cross-section along direction indicated in Fig. 11A , showing structural positions and ordering of the major rock units within tectonic...
FIGURES | View All (16)
Image
Correlations of the rock-stratigraphic units from the Kyrenia <b>Range</b> in Cypr...
Published: 11 March 2021
Fig. 12. Correlations of the rock-stratigraphic units from the Kyrenia Range in Cyprus to the MisisAndırın and Amanos ranges in southern Anatolia. [Colour online.]
Journal Article
Published: 01 December 1990
Journal of the Geological Society (1990) 147 (6): 1023–1034.
... East Anatolian fault and a fold-thrust belt termed the Engizek zone, equivalent to the Bitlis suture further east. The African-Anatolian boundary lies along the Cyprus-Misis-Andirin trend and is expressed near the triple junction as the Aslantaº-Iskenderun zone, now undergoing slow left-lateral...
Journal Article
Published: 31 August 2011
Geological Magazine (2012) 149 (2): 264–290.
...ALASTAIR H. F. ROBERTSON; KEMAL TASLI; NURDAN İNAN Abstract Sedimentary geology and planktonic foraminiferal biostratigraphy have shed light on the geological development of the northern, active continental margin of the Southern Neotethys in the Kyrenia Range. Following regional Triassic rifting...
Image
A simplified tectonic setting of the northeastern corner of the East Medite...
Published: 01 June 2004
Basin (stippled); DSF, Dead Sea Fault; EAFZ, East Anatolian Fault Zone; EF, Ecemiş Fault; EHF, East Hatay Fault; GFZ, Göksun Fault Zone; IB, Iskenderun Bay; KF, Kozan Fault; KT, Kyrenea Thrust (cross-hatched); MAR, Misis-Andirin Mauntain Range (cross-hatched); and YF, Yumurtalik Fault.
Journal Article
Published: 01 May 2004
Geological Magazine (2004) 141 (3): 379–387.
... & Yildiz (1991) and Şafak (1993 b ) in the Antakya Basin, Misis-Andirin area by Gökçen, Gökçen & Kelling (1991) (Fig. 3 ). Category . Interval zone. Age . Late Burdigalian. Author . Jenkins (1966) . Definition . Interval from first occurrence of Praeorbulina glomerosa...
FIGURES
Journal Article
Published: 01 June 2004
Bulletin of the Seismological Society of America (2004) 94 (3): 930–939.
... Basin (stippled); DSF, Dead Sea Fault; EAFZ, East Anatolian Fault Zone; EF, Ecemiş Fault; EHF, East Hatay Fault; GFZ, Göksun Fault Zone; IB, Iskenderun Bay; KF, Kozan Fault; KT, Kyrenea Thrust (cross-hatched); MAR, Misis-Andirin Mauntain Range (cross-hatched); and YF, Yumurtalik Fault. ...
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Journal Article
Published: 25 September 2013
Geological Magazine (2014) 151 (4): 692–731.
..., metamorphic and tectonic processes related to ocean basin closure and continental collision. The Kyrenia Range in the north of Cyprus ( Fig. 1 ) provides useful insights into such processes. The range is here loosely divided into Western, Central and Eastern ranges, plus the Karpas...
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Journal Article
Published: 15 October 2018
Canadian Journal of Earth Sciences (2019) 56 (11): 1163–1180.
... before thrusting are firmly established when the litho-stratigraphic contents of the thrust sheets are compared and correlated ( Yılmaz 1993 ). The geological map together with an accompanying stratigraphic section and the geological cross-section of the mountain range are displayed in Figs. 1 – 3...
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Journal Article
Published: 01 July 2002
Geological Magazine (2002) 139 (4): 473–487.
... . Adana Turkey Miocene extension tectonics depositional fault palaeogeography The Neogene history of south-central Turkey is marked by the development and subsequent deformation of several large sedimentary basins (Adana, Mut, Misis-Andirin, Maraş, etc.) with predominantly marine fill...
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Journal Article
Published: 01 November 2012
Petroleum Geoscience (2012) 18 (4): 381–404.
... slices and blocks of ophiolitic rocks occur within Paleogene melange in the Misis Mountains on the adjacent Turkish mainland ( Floyd et al . 1991 ; Robertson et al . 2004 ). Larger slices of ophiolitic rocks characterize the northeastward continuation of this structural lineament through the Andırın...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/GSL.SP.2000.173.01.05
EISBN: 9781862394216
... Mountains) in the north, and associated ophiolites and ophiolitic mélange, the Miocene Mut and Adana Basins, in the east, and further south the Misis Mountains (westerly) and the Andırın Mountains (easterly). Offshore areas are the Adana–Cilicia Basin and the submerged Kyrenia–Misis Lineament connecting...
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Journal Article
Published: 20 April 2018
Journal of Foraminiferal Research (2018) 48 (2): 121–141.
...-basin lies in the northwest of Adana basin, which is one of the largest Neogene basins in the Middle Taurid zone, southern Turkey. The Adana basin is limited by the Taurus Mountains to the north and the Mediterranean to the south. The Misis-Andırın fault, which forms the boundary between the Arabian...
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Journal Article
Journal: Palynology
Published: 02 October 2018
Palynology (2018) 42 (4): 516–539.
..., and the established biozones were calibrated to those based on planktonic foraminifera and calcareous nannofossils. This approach reveals possible deviations from the standard ranges of dinoflagellate cyst taxa known in the literature from other areas. The observed differences in occurrences will be discussed...
Journal Article
Journal: GSA Bulletin
Published: 01 January 2012
GSA Bulletin (2012) 124 (1-2): 133–145.
.... , 2004 , The Misis-Andirin complex: A mid-Tertiary mélange related to late-stage subduction of the southern Neotethys in S Turkey : Journal of Asian Earth Sciences , v. 22 , no. 5 , p. 413 – 453 , doi:10.1016/S1367-9120(03)00062-2 . Robertson A.H.F. Dixon J.E. Brown S. Collins S...
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Journal Article
Published: 29 October 2012
Geological Magazine (2013) 150 (2): 333–359.
...) results. However, the commonly sparse or abraded nature of the planktonic foraminifera means that only rather general age ranges could be assigned in some cases. Table 3 shows the maximum and minimum possible ages for each sample as determined by the Sr dating (i.e. from...
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Journal Article
Published: 07 January 2019
Canadian Journal of Earth Sciences (2019) 56 (11): 1119–1143.
... from the middle Liassic to Middle Jurassic — reliable isotopic ages ranging from 190 to 160 Ma (see the discussion in Picard and Hirsch 1987 , pp. 72–74). Rifting stopped at the end of the Middle Jurassic during the Callovian (163 Ma) after a hinge belt had appeared in the Middle Jurassic along...
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Journal Article
Journal: Geosphere
Published: 02 April 2021
Geosphere (2021) 17 (3): 739–765.
... of internal lakes and sediment production from intervening ranges, while the latter can affect water and sediment fluxes on an orogenic plateau. CORRESPONDENCE: gilles.brocard@mom.fr 24 02 2020 26 10 2020 28 01 2021 © 2021 The Authors 2021 Gold Open Access: This paper...
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