Show/Hide Menu
Hide/Show Apps
Logout
Türkçe
Türkçe
Search
Search
Login
Login
OpenMETU
OpenMETU
About
About
Open Science Policy
Open Science Policy
Open Access Guideline
Open Access Guideline
Postgraduate Thesis Guideline
Postgraduate Thesis Guideline
Communities & Collections
Communities & Collections
Help
Help
Frequently Asked Questions
Frequently Asked Questions
Guides
Guides
Thesis submission
Thesis submission
MS without thesis term project submission
MS without thesis term project submission
Publication submission with DOI
Publication submission with DOI
Publication submission
Publication submission
Supporting Information
Supporting Information
General Information
General Information
Copyright, Embargo and License
Copyright, Embargo and License
Contact us
Contact us
Plio-quaternary sediments,paleo-topography of the messinian evaporities,and salt tectonism in the Cilicia Basin,Northeastern Mediterranean Sea
Download
143707.pdf
Date
2003
Author
Toker, Mustafa
Metadata
Show full item record
Item Usage Stats
205
views
0
downloads
Cite This
Subject Keywords
Marine sediments
,
Submarine valley
URI
https://hdl.handle.net/11511/13459
Collections
Graduate School of Marine Sciences, Thesis
Suggestions
OpenMETU
Core
Electrical impedance tomography using induced currents.
Gençer, Nevzat Güneri; İder, Yusuf Ziya; Department of Electrical and Electronics Engineering (1993)
Studies of waterflooding in low-permeable chalk by use of X-ray CT scanning [J. Pet. Sci. Eng. 32 (2001) 1-10]
Akın, Serhat (2002-10-01)
Sedimentary Records of Past Earthquakes during the Last 2400 Years in Botnsvatn Lake on the Húsavík-Flatey Fault, North Iceland
Avşar, Ulaş; Geirsdttir, Aslaug; Thordarson, Thor; Miller, Gifford (2014-12-19)
The Húsavík-Flatey Fault (HFF), which is a part of the Tjörnes Fracture Zone (TFZ) in North Iceland, is a ~100 km-long dextral strike-slip fault. The fault has produced many magnitude 6-7 earthquakes in the past; however, the historical earthquake record in the region is mostly limited to the past 300 years. Almost 80% of the HFF is offshore. At the on-land part of the fault, glacial morphology and lack of well-developed fluvial systems limit the number of sites having faulting-related sedimentation, which ...
Seismic evidence of shallow gas in the sediment on the shelf off Trabzon, southeastern Black Sea
Okyar, M; Ediger, V (1999-04-01)
High-resolution seismic surveys carried out on the shelf off Trabzon (southeastern Black Sea) show that the sub-bottom stratigraphy consists of two main depositional sequences (A and B) one of which contains zones of acoustic turbidity. Of these, the upper depositional sequence (A) is thought to comprise Holocene sediments, while the lower depositional sequence (B) is interpreted as approximating to the Pleistocene. The boundary between these sequences is defined by a reflector (R), which is interpreted as ...
ELECTRON POLARIZATION IN A QUANTUM-WELL WITH UNIFORM ELECTRIC-FIELD
ILAIWI, KF; Tomak, Mehmet (1991-06-01)
The polarization of a quantum electron confined in a one-dimensional potential well in the presence of a uniform electric field is calculated numerically. We find that the negative polarization of the first excited state in previous calculations is solely due to the neglect of the electric field outside the quantum well.
Citation Formats
IEEE
ACM
APA
CHICAGO
MLA
BibTeX
M. Toker, “Plio-quaternary sediments,paleo-topography of the messinian evaporities,and salt tectonism in the Cilicia Basin,Northeastern Mediterranean Sea ,” M.S. - Master of Science, Middle East Technical University, 2003.