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Ganos Fault

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Journal Article
Journal: Geology
Published: 01 November 2010
Geology (2010) 38 (11): 991–994.
...Murat Ersen Aksoy; Mustapha Meghraoui; Martin Vallée; Ziyadin Çakır Abstract The Ganos fault is the westernmost segment of the North Anatolian fault that generated the 9 August 1912 Mürefte (Ganos) earthquake in western Turkey (M w = 7.4). We study the 1912 earthquake characteristics using...
FIGURES | View All (4)
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<span class="search-highlight">Ganos</span> <span class="search-highlight">fault</span> onshore and A.D. 1912 coseismic slip distribution (in meters). ...
Published: 01 November 2010
Figure 2. Ganos fault onshore and A.D. 1912 coseismic slip distribution (in meters). Yellow boxes correspond to measures of this study. EQ–earthquake.
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<span class="search-highlight">Ganos</span> <span class="search-highlight">fault</span> segment (seg.) and A.D. 1912 coseismic slip distribution. Subse...
Published: 01 November 2010
Figure 4. Ganos fault segment (seg.) and A.D. 1912 coseismic slip distribution. Subsegments along fault zone indicate geometrical complexities. The 150-km-long fault (red lines in upper panel) includes 9 August and 13 September earthquake ruptures. Marmara Sea slip values (two triangles in lower
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Topography and active <span class="search-highlight">faults</span> in northwest Turkey. The contours are at 500, ...
Published: 01 September 2000
, respectively, with respect to a fixed station at Yenice north of the Ganos Fault ( Straub & Kahle, 1995 ). Biga peninsula south of the Ganos fault is moving southwest at a rate of 2 cm/year. The Kazdağ range forms a transpressive ridge in a restraining step-over.
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Tectonic map of the Marmara region showing surface <span class="search-highlight">fault</span> breaks of the İzm...
Published: 01 February 2002
Figure 2. Tectonic map of the Marmara region showing surface fault breaks of the İzmit and Düzce earthquakes. The bar-graph inset shows some of the measured right-lateral offsets along the fault ruptures. Epicenters of the 1912 Ganos earthquake (M s 7.4), 1967 Mudurnu Valley earthquake (M s
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Tentative models proposed to explain development of clockwise and anticlock...
Published: 01 March 2007
that after the restoration the basalt outcrops are aligned N–S. Note also that 60° clockwise rotation of the area between the Tekirdağ and Ganos faults resulted from 30° regional and further 30° local rotation of the area.
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Shear-strain rates along the cross sections in  Figure 4a . Vertical and ho...
Published: 01 February 2002
boundary zone; SR, slip rate along the northern branch of the NAF. (a) AA′, Gulf of Saros; (b) BB′, Ganos fault; (c) CC′, Marmara Sea; (d) DD′, Gulf of İzmit; (e) EE′, near İzmit; (f) FF′, Sapanca Lake; (g) GG′, Düzce Fault; (h) HH′, Bolu-Gerede area.
Journal Article
Published: 01 March 2007
Geological Magazine (2007) 144 (2): 379–392.
... that after the restoration the basalt outcrops are aligned N–S. Note also that 60° clockwise rotation of the area between the Tekirdağ and Ganos faults resulted from 30° regional and further 30° local rotation of the area. ...
FIGURES | View All (7)
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(a) Shear strain rates ( ϵ  12 ) in nstrain/yr (1.0 × 10 9  rad/yr) obtaine...
Published: 01 February 2002
, and vertical axis is shear-strain rate in nstrain/yr. GS, Gulf of Saros; GF, Ganos Fault; MS, Marmara Sea; GI, Gulf of İzmit; I, İzmit; SL, Sapanca Lake; DF, Düzce Fault; BGI, Bolu-Gerede-Ismetpasa area.
Journal Article
Journal: Geology
Published: 01 February 2000
Geology (2000) 28 (2): 187–188.
... on the observation that Mount Ganos and the northern part of Gelibolu Peninsula are the halves of an anticlinal structure sliced by the Ganos fault. The internal structure of Mount Ganos is syncline faulted in the northern limb ( Yaltırak., 1996 ) with the synclinal axis observed along the crest of the mountain...
FIGURES
Journal Article
Journal: Geology
Published: 01 February 2000
Geology (2000) 28 (2): 188–189.
... Anatolian fault. We specifically disagree with the views of Yaltırak et al. on two important points: (1) Despite minor complexities, the Ganos and the Gelibolu folds appear to be two large anticlines that are truncated by the North Anatolian fault; and (2) Concerning the folded structure in the Dardanelles...
FIGURES
Journal Article
Published: 19 March 2024
Bulletin of the Seismological Society of America (2024) 114 (4): 2151–2171.
...‐average shear‐wave velocity at the top 30 m ( V S 30 ), and style of faulting. We use a Generative Adversarial Neural Operator (GANO)—a resolution invariant architecture that guarantees model training independent of the data sampling frequency. We first present the conditional ground‐motion synthesis...
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Profile 84 across the Mt. <span class="search-highlight">Ganos</span> shelf and slope showing the underthrusting ...
Published: 04 February 2014
Fig. 16. Profile 84 across the Mt. Ganos shelf and slope showing the underthrusting of the Tekirdağ Basin floor under the rising pillar of Mr. Ganos and the development of a small marginal fold-thrust belt. This underthrusting activity is probably the reason of the microseismicity seen along
Journal Article
Published: 01 April 2011
Bulletin of the Seismological Society of America (2011) 101 (2): 775–791.
... and the Ganos fault onshore (Fig.  1 ). Water depth reaches over 1.1 km in the basin, while thickness of the sediment infill, estimated from analysis of seismic reflection profiles, is over 4 km ( Okay et al. , 1999 ). This setting is complicated by the presence of compressive deformation affecting the western...
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Series: Geological Society, London, Special Publications
Published: 01 January 2009
DOI: 10.1144/SP316.3
EISBN: 9781862395640
... to the city of Istanbul, one of the largest cities in the Middle East. Across the 1912 rupture of the Ganos strand of the North Anatolian fault west of the Marmara Sea, we excavated 26 trenches to resolve slip and constrain the earthquake history on a channel–fan complex that crosses the fault at a high angle...
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Journal Article
Published: 25 November 2016
Canadian Journal of Earth Sciences (2016) 53 (11): 1416–1439.
... of Marmara, called the Main Marmara Fault (MMF) by Le Pichon et al. (2001) ; the Ganos Fault; the North Aegean Trough (NAT), formed by the Saros Basin to the east and the Sporades Basin to the west; the Grecian Shear Zone (GSZ), a broad zone of shear named by Şengör (1979) ; and finally, joining through...
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Journal Article
Published: 01 February 2002
Bulletin of the Seismological Society of America (2002) 92 (1): 216–229.
... boundary zone; SR, slip rate along the northern branch of the NAF. (a) AA′, Gulf of Saros; (b) BB′, Ganos fault; (c) CC′, Marmara Sea; (d) DD′, Gulf of İzmit; (e) EE′, near İzmit; (f) FF′, Sapanca Lake; (g) GG′, Düzce Fault; (h) HH′, Bolu-Gerede area. ...
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Frequency–magnitude relationships for the three segments of the North Anato...
Published: 19 August 2015
Figure 4. Frequency–magnitude relationships for the three segments of the North Anatolian fault zone ( NAFZ ). In the case of the Ganos segment, the numbers of the larger earthquakes do not follow the distribution relationship of the smaller ones, thus an alternative b ‐value fit based on events
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Tectonic sketch map of Sea of Marmara region. NAF-N and NAF-S are northern ...
Published: 01 January 2012
Figure 1. Tectonic sketch map of Sea of Marmara region. NAF-N and NAF-S are northern and southern segments of the North Anatolian fault ( Seeber et al., 2006 ). Red is the Main Marmara fault (MMF; Le Pichon et al., 2001 ). Red thick lines are the two main segments of the MMF: the Ganos segment
Journal Article
Published: 01 April 2015
Bulletin of the Seismological Society of America (2015) 105 (2A): 622–645.
... Earthquake 1894 August 1766 May 1766 1754 1719 1509 1343 1344 1296 989 860 740 Ambraseys (2002) Izmit Bay Ganos fault Çınarcık basin Çınarcık basin Izmit Bay Çınarcık basin Ganos fault Central basin Çınarcık basin Çınarcık basin South Çınarcık Bertrand et al. (2011...
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