Seafloor authigenic carbonate crusts along the submerged part of the North Anatolian Fault in the Sea of Marmara: Mineralogy, geochemistry, textures and genesis

Çağatay, Memet; Yildiz, Guliz; Bayon, Germain; Ruffine, Livio; Henry, Pierre

doi:10.1016/j.dsr2.2017.09.003

Seafloor authigenic carbonate crusts along the submerged part of the North Anatolian Fault in the Sea of Marmara: Mineralogy, geochemistry, textures and genesis

Atıf İçin Kopyala

Çağatay M. N., Yildiz G., Bayon G., Ruffine L., Henry P.

DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, cilt.153, ss.92-109, 2018 (SCI-Expanded)

Yayın Türü: Makale / Tam Makale
Cilt numarası: 153
Basım Tarihi: 2018
Doi Numarası: 10.1016/j.dsr2.2017.09.003
Dergi Adı: DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY
Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
Sayfa Sayıları: ss.92-109
İstanbul Teknik Üniversitesi Adresli: Evet

Özet

Extensive seafloor authigenic carbonate crusts occur as pavements, mounds and chimneys along the North Anatolian Fault System (NAFS) in the Sea of Marmara. They are often covered or surrounded by patches of black Fe-sulphide-rich sediments, and associated with hydrocarbon-rich gas and brackish-water emissions in the 1250 m-deep deep basins and with deep saline formation waters and hydrocarbons emissions from mud volcanoes and anticlines on the 350-650 m-deep compressional highs.