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D6 ASSEMBLAGE4 Margeol · Fault in the Eastern Marmara Region and its tectonic evolution’’. Marine Geology, 194: 203-208. Altinok, Y., 2004. A general overview of important tsunamis

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  • REFERENCES ***, 1995. Black Sea Bibliography 1974 - 1994. Black Sea Environmental Series, 1.

    United Nations Publications, New York, 364 pp. Abalioglu, I. and Sefunc, A., 1998. Sequence stratigraphic approach to possible

    reservoirs, offshore Black Sea / Turkey. Supplement to GEO-ECO-MARINA, 3(Abstracts): 18.

    Ablia, E.A., Konyukhov, A.I. and Zabanbark, A., 1998. Correlation of organic matter from Black Sea deep water mud volcanoes and some South Caspian onshore volcanoes. Supplement to GEO-ECO-MARINA, 3(Abstracts): 44.

    Abrajano, T., Aksu, A.E., Hiscott, R.N. and Mudie, P.J., 2002. Aspects of carbon isotope biogeochemistry of late Quaternary sediments from the Marmara Sea and Black Sea. Marine Geology, 190(1-2): 151-164.

    Abrantes, F. et al., 1998. Sediment fluxes along the northeastern European Margin: inferring hydrological changes between 20 and 8 kyr. Marine Geology, 152: 7-23.

    Adatepe, F., Demirel, S. and Alpar, B., 2002. Tectonic setting of the southern Marmara Sea region: based on seismic reflection data and gravity modelling. Marine Geology, 190(1-2): 383-395.

    Aksu, A.E. et al., 2002. Last glacial-Holocene paleoceanography of the Black Sea and Marmara Sea: stable isotopic, foraminiferal and coccolith evidence. Marine Geology, 190(1-2): 119-149.

    Aksu, A.E. et al., 2002. Persistent Holocene outflow from the Black Sea to the eastern Mediterranean contradicts Noah's Flood hypothesis. GSA Today(May): 4-10.

    Aksu, A.E., Hiscott, R.N. and Yasar, D., 1999. Oscillating Quaternary water levels of the Marmara Sea and vigorous outflow into the Aegean Sea from the Marmara Sea Black Sea drainage corridor. Marine Geology, 153(1-4): 275-302.

    Aksu, A.E., Hiscott, R.N., Yasar, D., Isler, F.I. and Marsh, S., 2002. Seismic stratigraphy of Late Quaternary deposits from the southwestern Black Sea shelf: evidence for non-catastrophic variations in sea-level during the last ~10000 yr. Marine Geology, 190(1-2): 61-94.

    Aksu, A.E. and Yaltirak, C., 2003. Erratum to ‘‘Quaternary Paleoclimatic-Paleoceanographic and Tectonic Evolution of the Marmara Sea and Environs’’ Edited by Ali E. Aksu and Cenk Yaltirak [Mar. Geol. 190/1-2 (2002)]. Marine Geology, 194: 209.

    Aksu, A.E., Yaltirak, C. and Hiscott, R.N., 2002. Quaternary paleoclimatic-paleoceanographic and tectonic evolution of the Marmara Sea and environs. Marine Geology, 190(1-2): 9-18.

    Albert, D.B., Taylor, C. and Martens, C.S., 1995. Sulfate reduction rates and low molecular weight fatty acid concentrations in the water column and surficial sediments of the Black Sea. Deep-Sea Research, 42(7): 1239-1260.

    Algan, O. et al., 2001. Stratigraphy of the sediment infill in Bosphorus Strait: water exchange between the Black and Mediterranean Seas during the last glacial-Holocene. Geo-Marine Letters, 20(4): 209-218.

    Algan, O. et al., 2002. A high-resolution seismic study in Sakarya Delta and Submarine Canyon, southern Black Sea shelf. Continental Shelf Research, 22(10): 1511-1527.

    Alpar, B. and Yaltirak, C., 2002. Characteristic features of the North Anatolian Fault in the eastern Marmara region and its tectonic evolution. Marine Geology, 190: 329-350.

    Alpar, B. and Yaltirak, C., 2003. Reply:‘‘Characteristic features of the North Anatolian

    1

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