Zobrazeno 1 - 10
of 59
pro vyhledávání: '"Ali E. Aksu"'
Publikováno v:
Basin Research. 31:709-727
Geologic evidence across orogenic plateau margins enables the discrimination of the relative contributions of orogenic, epeirogenic and/or climatic processes that lead to growth and maintenance of those plateaus and their margins. Here, we discuss th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fd52c237d30ba27d66d2d10dafccbf5c
https://doi.org/10.1111/bre.12341
https://doi.org/10.1111/bre.12341
Publikováno v:
Marine Geology. 407:213-228
The 10 m-thick Holocene succession at core site M02-45 (41°41.17′N, 28°19.08′E, −69 m water depth) has key advantages for investigation of the Sr-isotopic evolution of the Holocene Black Sea. Earlier studies have focussed on thinner successio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ba88298cb07a77cc89c5221f72aafe11
https://doi.org/10.1016/j.margeo.2018.11.004
https://doi.org/10.1016/j.margeo.2018.11.004
Publikováno v:
Sedimentary Geology (0037-0738) (Elsevier BV), 2021-10, Vol. 424, P. 105979 (21p.)
High-resolution multichannel seismic reflection profiles and multibeam mosaic maps of the seafloor are used to document the presence of two prominent regions representing major sediment failure(s) and the subsequent gravity-driven mass transport acro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::46760ebb72dbf02387c533df87cc7e86
https://aperta.ulakbim.gov.tr/record/236944
https://aperta.ulakbim.gov.tr/record/236944
Publikováno v:
Marine and Petroleum Geology. 96:51-70
The existing literature shows that the only saline water source for the eastern Mediterranean during the Messinian was the Atlantic Ocean and that the Sicily sill created a physical barrier between the eastern and western Mediterranean, higher than t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::85ff02e68c10c184812d3b724a5b4f83
https://doi.org/10.1016/j.marpetgeo.2018.05.022
https://doi.org/10.1016/j.marpetgeo.2018.05.022
Publikováno v:
Marine Micropaleontology. 142:48-66
The Holocene replacement of Ponto-Caspian ostracod assemblages by Mediterranean species is studied in two long composite cores, M02-45 (a composite of cores M02-45P, M02-45 T and M05-03P) and M05-50 (a composite of cores M05-50P and M05-51G), acquire
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6d7af8d4222a7687d43ed9c37290bcec
https://doi.org/10.1016/j.marmicro.2018.06.001
https://doi.org/10.1016/j.marmicro.2018.06.001
Publikováno v:
Marine and Petroleum Geology. 91:297-320
A dense grid of high-resolutions multichannel seismic reflection profiles from the northern basins of the eastern Mediterranean (Rhodes, Finike, Antalya, Cilicia, Adana and Latakia basin) allow documenting a Messinian evaporite succession of variable
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ff5d7d81d7a66514eec5d351c0759f43
https://doi.org/10.1016/j.marpetgeo.2018.01.016
https://doi.org/10.1016/j.marpetgeo.2018.01.016
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 490:325-346
High-resolution multibeam mosaics show that the seafloor across the southwestern Marmara Sea is host to remarkably organized near-circular bioherm mounds, which commonly are arranged into large, tightly packed clusters. Grab samples and gravity cores
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e7e3671ad65a80e181fdb6767ba7ad17
https://doi.org/10.1016/j.palaeo.2017.11.010
https://doi.org/10.1016/j.palaeo.2017.11.010
Publikováno v:
Tectonophysics. 814:228952
Multichannel seismic reflection profiles show that the Outer Cilicia Basin evolved mainly during the uppermost Messinian–Quaternary as an asymmetric piggyback basin on the hanging wall of the large south-verging Kyrenia thrust culmination, followin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::be747719232ce31e82c55188e3e85b4c
https://doi.org/10.1016/j.tecto.2021.228952
https://doi.org/10.1016/j.tecto.2021.228952
Publikováno v:
Tectonophysics. 814:228953
The structural evolution of the Larnaka Ridge is studied using high-resolution multichannel seismic reflection profiles and multibeam mosaics of the seafloor. Multibeam maps revealed the presence of two families of en-echelon tension cracks (young an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dbf1febf3d7cba62dc0a59bda0398c0d
https://doi.org/10.1016/j.tecto.2021.228953
https://doi.org/10.1016/j.tecto.2021.228953
Publikováno v:
Marine Geology. 390:147-169
Source-to-sink tracing of very fine sand supplied to a controversial lower Holocene deltaic lobe in the northeastern Marmara Sea was undertaken using SEM backscatter mapping and quantitative ‘mineral liberation analysis’ of very fine sand fractio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::36ca8c8b20cf3bb3a930bb12f8af0dc9
https://doi.org/10.1016/j.margeo.2017.06.008
https://doi.org/10.1016/j.margeo.2017.06.008