1-20 OF 46 RESULTS FOR

Cinarcik Basin

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Image
Reconstruction of the incremental displacements of the <b>Çınarcık</b> <b>Basin</b> depoc...
Published: 16 April 2019
Fig. 9. Reconstruction of the incremental displacements of the Çınarcık Basin depocenter, where the left column represents the minimum and the right one shows the maximum offsets for each vertical thickness (isochore) maps between different seismic horizons. Isochore maps between each seismic
Image
(a) Daily seismicity rate in the <b>Çınarcık</b> <b>basin</b> from  PIRES  recordings: A ...
Published: 01 August 2011
Figure 2. (a) Daily seismicity rate in the Çınarcık basin from PIRES recordings: A high number of events compared to the background seismicity is observed for particular time periods indicating temporal clustering of earthquakes along the Princes Islands segments of the NAFZ . The squares mark
Image
Figure 2. Relief and bathymetry of <b>Cinarcik</b> <b>Basin</b> ( Rangin et al., 2001 ). ...
in > Geology
Published: 01 November 2006
Figure 2. Relief and bathymetry of Cinarcik Basin ( Rangin et al., 2001 ). This triangular half graben is bordered on north by arcuate transtensional segment of northern North Anatolian transform fault between Tuzla and Istanbul bends. This fault forms south-facing monocline on horizontal “bench
Journal Article
Published: 01 April 2015
Bulletin of the Seismological Society of America (2015) 105 (2A): 622-645.
... of the NAF . Klg04 was collected from a berm north of the fault, and Klg03 was positioned in the Çınarcık basin, south of the fault. The cores were correlated using long‐term geochemical variations in the sediment, and turbidites deposited simultaneously at both sites were then identified. Radionuclide...
FIGURES | View All (18)
Journal Article
Journal: Geology
Published: 01 November 2006
Geology (2006) 34 (11): 933-936.
...Figure 2. Relief and bathymetry of Cinarcik Basin ( Rangin et al., 2001 ). This triangular half graben is bordered on north by arcuate transtensional segment of northern North Anatolian transform fault between Tuzla and Istanbul bends. This fault forms south-facing monocline on horizontal “bench...
FIGURES | View All (5)
Journal Article
Published: 01 July 2014
Bulletin of the Seismological Society of America (2014) 104 (4): 1954-1963.
... velocities between ∼1.5 and 1.8 km/s, which is well explained by the 3–4 km‐deep Çınarcık basin, located between the two major fault branches, the Princes Islands and Armutlu fault segments. In contrast, ray paths restricted to within the mainland of Istanbul and the Armutlu peninsulas (primarily trending...
FIGURES | View All (7)
Series: Geological Society, London, Special Publications
Published: 01 January 2006
DOI: 10.1144/GSL.SP.2006.253.01.21
EISBN: 9781862395015
... Marmara fault favours continuous propagation of westward rupture. This scenario would result in a cumulative rupture length of at least 80 km before the rupture intersected the Central Marmara basin. In contrast, rupture of the Çinarcik fault would not be likely to exceed 50–60 km, based on its isolated...
FIGURES | View All (14)
Journal Article
Journal: Geology
Published: 01 January 2012
Geology (2012) 40 (1): 3-6.
... in the location of the main depocenter in Çınarcık Basin ( Carton et al., 2007 ). In the Central Basin, interpretation of seismic reflectors in terms of glacio-eustatic sequencing suggests a minimum age of 3 Ma for the onset of subsidence ( Laigle et al., 2008 ). However, seismic surveys reveal that the basin...
FIGURES
Journal Article
Journal: Geology
Published: 01 May 2012
Geology (2012) 40 (5): 439-442.
... of sedimentary layers themselves by extension and contraction ( Figs. 2 and 3B ). In some regions of creep, the mode of deformation changes from folding to faulting along strike (e.g., southern Çınarcık basin; see the Data Repository figures). Additionally, it is likely that shear is more prevalent than can...
FIGURES
Journal Article
Journal: Lithosphere
Published: 01 June 2010
Lithosphere (2010) 2 (3): 199-206.
..., Taşova-Erbaa, Yeniçağa, Bolu, Pamukova, Yenişehir, Çınarcık, Central, and Tekirdağ Basins along the North Anatolian fault zone have depths of 3.9, 1.8, 1.7, 2.4, 0.8, 3, 2.5, 2.7, 4.4, 1.1, and 2 km, respectively ( Table 1 ). As I mentioned already, there are deviations on the third dimensions...
FIGURES | View All (7)
Image
(a) Global geodynamic context of the Anatolian plate with Global Positionin...
Published: 01 April 2015
with rupture dates and dots. (c) The map of Çınarcık basin. Location of the two studied cores is represented with respect to the Çınarcık fault segment. Arrows show sediment paths for turbidite deposits ( Altınok et al. , 2011 ). The line crossing the two cores represents the topographic profile presented
Journal Article
Journal: Geosphere
Published: 01 December 2015
Geosphere (2015) 11 (6): 2067-2129.
... in Sumatra, we collected 144 deep-sea sediment cores in the trench and in lower slope piggyback basins of the Sumatra accretionary prism. We used multibeam bathymetry and seismic reflection data to develop an understanding of catchment basins, turbidity current pathways, and depositional styles, as well...
FIGURES | View All (20)
Image
(a) and (b) are stations pairs (left panel) and resulting cross correlation...
Published: 01 July 2014
of Marmara, including the Çınarcık basin; and (g, h) the Armutlu peninsula (southern block).
Series: Geological Society, London, Special Publications
Published: 01 January 2007
DOI: 10.1144/SP290.2
EISBN: 9781862395381
... (California) San Andreas R. Brown & Vedder (1967) ; Shedlock et al. (1990) ; Graymer et al. (2007) 64 Rhomboidal pull-apart Active Miocene–Pliocene Cinarcik Basin Turkey North Anatolian Okay et al. (2000) ; Le Pichon et al. (2001) ; Seeber et al. (2006) 65 Rhomboidal pull...
FIGURES | View All (67)
Image
Figure 1. Tectonic sketch map of Marmara Sea region. West of 32°E, North An...
in > Geology
Published: 01 November 2006
early Eocene suture ( Yılmaz et al., 1997 ). Cinarcik Basin (boxed) is on extensional side of prominent south-pointing bend along NAF-N. P—Peninsula; G—Gulf; B—Basin.
Image
Seismotectonic map of the eastern Sea of Marmara. Shown is microseismic act...
Published: 01 April 2013
Figure 2. Seismotectonic map of the eastern Sea of Marmara. Shown is microseismic activity throughout the Çınarcık Basin as located by seismic networks (Fig.  1b ) between October 2006 and October 2010. Fault traces are taken from Armijo et al. (2005) . Black focal mechanisms indicate
Series: Geological Society, London, Memoirs
Published: 01 January 2006
DOI: 10.1144/GSL.MEM.2006.032.01.14
EISBN: 9781862394070
... of ophiolites onto former passive continental margins (Oman-type model). A second setting relates to ophiolite emplacement along active continental margins (‘Cordilleran-type’ model) by processes including subduction-accretion or the collapse of back-arc marginal basins. Because the ophiolites of the Eastern...
FIGURES | View All (25)
Image
Map of the Sea of Marmara based on bathymetric data collected with R/V Le S...
Published: 01 April 2011
–August 2007. The exact OBS coordinates are listed in Appendix A . Abbreviations: TB , Tekirdag basin; WH , Western high; CB , Central basin; KB , Kumburgaz basin; CH , Central high; ÇB , Çinarcik basin; IB , Imrali basin; Is .: Island ; NAFZ , North Anatolian Fault Zone. The inset shows
Image
(a) Seismic stations used in this study, framing the Princes Islands segmen...
Published: 01 July 2014
[ARNET]; yellow, Turkish Disaster and Emergency Presidency in Ankara [AFAD], respectively. See text for details.). Orange rectangle illustrates the position of the depth section shown in (b). (b) Depth section in which gray shading denotes the sediments of the Çınarcık basin (after Carton et al. , 2007
Journal Article
Published: 01 April 2011
Bulletin of the Seismological Society of America (2011) 101 (2): 775-791.
...–August 2007. The exact OBS coordinates are listed in Appendix A . Abbreviations: TB , Tekirdag basin; WH , Western high; CB , Central basin; KB , Kumburgaz basin; CH , Central high; ÇB , Çinarcik basin; IB , Imrali basin; Is .: Island ; NAFZ , North Anatolian Fault Zone. The inset shows...
FIGURES | View All (17)