@article {113,
	title = {Deciphering hemipelagites from homogenites through anisotropy of magnetic susceptibility. Paleoseismic implications (Sea of Marmara and Gulf of Corinth)},
	journal = {Sedimentary Geology},
	volume = {292},
	year = {2013},
	pages = {1-14},
	abstract = {In closed marine basins and large lakes, gravity re-depositional processes often result in specific turbidites with two abruptly separated layers: a coarse graded lower term and an upper homogenous fine-grained term. An additional mixed term generally occurs in between, indicating to and from particle displacements. The later ones are related to oscillating bottom currents responsible for a high increase of the fine fraction segregation, within the reworked wasted mass. The whole sedimentary event is the association {\textquotedblleft}homogenite + turbidite{\textquotedblright} (HmTu), which specific a settling condition area here characterized through Anisotropy of Magnetic Susceptibility (AMS). Homogenites{\textquoteright}s magnetic foliation appears anomalously high with respect to their expected state of compaction, and strikingly higher than hemipelagites{\textquoteright}s values. We applied this approach to Late Pleistocene/Holocene sediments from the Sea of Marmara and from the Gulf of Corinth. Grain-size and other magnetic parameters related to mineralogy are added to better assess the granular array influence on AMS. As HmTu is considered as often related to earthquake-triggering and tsunami/seiche effects, AMS appears as a useful tool for subaqueous paleoseismic investigations. First, it may evidence the signature of paleo-earthquakes; second, it permits to decipher hemipelagic intervals which are inferred to represent the time elapsed between two successive reworking events.},
	issn = {0037-0738},
	doi = {10.1016/j.sedgeo.2013.03.015},
	url = {http://www.sciencedirect.com/science/article/pii/S0037073813000614},
	author = {Campos, Corina and Beck, Christian and Crouzet, Christian and Demory, Fran{\c c}ois and Van Welden, Aur{\'e}lien and Eris, Kadir}
}
@article {159,
	title = {Late-Pleistocene to Holocene sedimentary fills of the {\c C}{\i}narc{\i}k Basin of the Sea of Marmara},
	journal = {Sedimentary Geology},
	volume = {281},
	year = {2012},
	note = {id: 2309},
	pages = {151-165},
	abstract = {A giant RV Marion Dufresne piston core MD01-2425 recovered from the 1276 m-deep {\c C}{\i}narc{\i}k Basin of the Sea of Marmara documents characteristics of deep basin sedimentation influenced by large-scale gravity-controlled mass-wasting processes and associated turbidite deposition during the Late Pleistocene to Holocene. A visual lithological description of the core reveals twenty major seismoturbidite layers (> 20 cm thick), intercalated in hemipelagic-type fine-grained calcareous and slightly siliceous clays. The thickness and frequency of the sesimoturbidite layers deposited during the lacustrine period (prior to 12.3 cal ka BP) is much greater than during the Holocene marine period. The sedimentary processes during deposition of seismoturbidites in the basin have been determined in this study using a combination of grain-size parameters. Often the seismoturbidites show strong grain segregation with a sharp boundary between a coarse lower and a homogeneous upper part. The traction carpet deposits formed at the base of a turbulent suspension and were produced in the lower coarse-grained part, whereas the homogeneous upper part was deposited by uniform suspensions following bedload deposition.},
	issn = {0037-0738},
	doi = {10.1016/j.sedgeo.2012.09.001},
	url = {http://www.sciencedirect.com/science/article/pii/S0037073812002473},
	author = {Eri{\c s}, K. Kadir and {\c C}a{\u g}atay, Nam{\i}k and Beck, Christian and Mercier de Lepinay, Bernard and Corina, Campos}
}
