Traces of the last earthquake sequence (1939-1944) along NAF from lacustrine sediments

2008-04-18
Avşar, Ulaş
Hubert-ferrari, Aurelia
Fagel, Nathalie
King, Jeofrey

Suggestions

Evidence of orbital forcing in lake level fluctuations in the Middle Eocene oilshale bearing lacustrine successions in the Mudurnu Göynük Basin NW Anatolia Turkey
Ocakoğlu, Faruk; Sanem, Acikalin; Yılmaz, İsmail Ömer; Şafak, Ümit (2012-01-01)
Mudurnu-Göynük basin of the Sakarya Zone in NW Anatolia comprises ca. 1500 m thick Paleocene–Eocene terrestrial to shallow marine succession overlying the Late Cretaceous deeper marine progradational fore-arc sediments. Formed in a foreland setting in relation to southerly situated İzmir–Ankara suture zone, this terrestrial succession (regionally known as Kızılçay group) comprises a thin (<200 m) oil shale-bearing lacustrine section with very good cyclic patterns that potentially serves the quantification o...
Evidence of orbital forcing in lake-level fluctuations in the Middle Eocene oil shale-bearing lacustrine successions in the Mudurnu-Goynuk Basin, NW Anatolia (Turkey)
OCAKOĞLU, FARUK; Acikalin, S.; Yılmaz, İsmail Ömer; ŞAFAK, ÜMİT; GÖKÇEOĞLU, CANDAN (2012-08-29)
Mudurnu-Goynuk basin of the Sakarya Zone in NW Anatolia comprises ca. 1500 m thick Paleocene-Eocene terrestrial to shallow marine succession overlying the Late Cretaceous deeper marine progradational fore-arc sediments. Formed in a foreland setting in relation to southerly situated izmir-Ankara suture zone, this terrestrial succession (regionally known as Kizilcay group) comprises a thin (<200 m) oil shale-bearing lacustrine section with very good cyclic patterns that potentially serves the quantification o...
Evidence for similar to 80-75 Ma subduction jump during Anatolide-Tauride-Armenian block accretion and similar to 48 Ma Arabia-Eurasia collision in Lesser Caucasus-East Anatolia
Rolland, Yann; PERİNÇEK, DOĞAN; Kaymakcı, Nuretdin; Sosson, Marc; Barrier, Eric; Avagyan, Ara (2012-05-01)
Orogens formed by a combination of subduction and accretion are featured by a short-lived collisional history. They preserve crustal geometries acquired prior to the collisional event. These geometries comprise obducted oceanic crust sequences that may propagate somewhat far away from the suture zone, preserved accretionary prism and subduction channel at the interplate boundary. The cessation of deformation is ascribed to rapid jump of the subduction zone at the passive margin rim of the opposite side of t...
Evidence from the Gediz graben for episodic two-stage extension in western Turkey
Kocyigit, A; Yusufoglu, H; Bozkurt, Erdin (1999-05-01)
Western Turkey falls within a wide belt of NNE-SSW-directed, active continental extension, generally similar to the Basin and Range Province of the USA It comprises a zone of WNW-ESE-trending major grabens. Derailed study of the Gediz graben reveals two contrasting infills that represent two distinct extensional stages, separated by a short phase of compression. The older infill consists of an 800m thick, folded and exhumed continental sedimentary sequence with intercalated calc-alkaline volcanics. It accum...
Evidence for long-term gamma-ray and X-ray variability from the unidentified TeV source HESS J0632+057
Acciari, V. A.; et. al. (IOP Publishing, 2009-06-20)
HESS J0632+057 is one of only two unidentified very-high-energy gamma-ray sources which appear to be point-like within experimental resolution. It is possibly associated with the massive Be star MWC 148 and has been suggested to resemble known TeV binary systems like LS I + 61 303 or LS 5039. HESS J0632+057 was observed by VERITAS for 31 hr in 2006, 2008, and 2009. During these observations, no significant signal in gamma rays with energies above 1 TeV was detected from the direction of HESS J0632+057. A fl...
Citation Formats
U. Avşar, A. Hubert-ferrari, N. Fagel, and J. King, “Traces of the last earthquake sequence (1939-1944) along NAF from lacustrine sediments,” 2008, Accessed: 00, 2021. [Online]. Available: https://hdl.handle.net/11511/81498.