Add to ORKGThe aim of this study is to establish the planktonic foraminiferal biozonation, to construct the sequence stratigraphical framework and to determine the foraminiferal response to sedimentary cyclicity in the sedimentary sequence spanning Upper Cretaceous-Paleocene in the Haymana basin (Central Anatolia, Turkey)
The Paleocene-Eocene sequences are widely distributed around onshore and offshore Black Sea. When th...
Larger foraminifera are recognized from the middle Tertiary (Oligocene-Miocene) carbonate sediments,...
WOS: 000371939000010The uppermost Cretaceous (upper Campanian-Maastrichtian) pelagic successions fro...
The aim of this study is to establish the planktonic foraminiferal biozonation, to construct the seq...
The aim of this study is to establish the planktonic foraminiferal biozonation, to construct the se...
The Cretaceous-Paleogene (K/Pg) boundary in the Haymana Basin, Central Anatolia, Turkey, was delinea...
The Haymana Basin, Turkey, hosts complete record of sedimentation across the Cretaceous-Paleogene (K...
Abundance and diversity patterns in planktonic foraminifera are important for paleoenvironmental and...
WOS: 000085050300006Planktonic and larger benthonic foraminifers of the Upper Cretaceous (Santonian-...
Larger foraminifera of the late Cretaceous (late Campanian) to middle Eocene (Lutetian) are recogniz...
In order to establish the taxonomy of deep-sea (small) benthic foraminifera and to evaluate their pa...
The Haymana basin in Central Anatolia (Turkey) formed on a Late Cretaceous to Middle Eocene fore ar...
Bu çalışmada Bilecik'in Doğusundaki Geç Jura-Kretase yaşlı birimleri oluşturan yamaç-havza çökelleri...
The Middle Eocene sequence in the Darende-Balaban Basin (Eastern Turkey) characterized by shallow an...
The Baskil section, located to the west of Elazığ in eastern Turkey, represents deep-marine facies o...
The Paleocene-Eocene sequences are widely distributed around onshore and offshore Black Sea. When th...
Larger foraminifera are recognized from the middle Tertiary (Oligocene-Miocene) carbonate sediments,...
WOS: 000371939000010The uppermost Cretaceous (upper Campanian-Maastrichtian) pelagic successions fro...
The aim of this study is to establish the planktonic foraminiferal biozonation, to construct the seq...
The aim of this study is to establish the planktonic foraminiferal biozonation, to construct the se...
The Cretaceous-Paleogene (K/Pg) boundary in the Haymana Basin, Central Anatolia, Turkey, was delinea...
The Haymana Basin, Turkey, hosts complete record of sedimentation across the Cretaceous-Paleogene (K...
Abundance and diversity patterns in planktonic foraminifera are important for paleoenvironmental and...
WOS: 000085050300006Planktonic and larger benthonic foraminifers of the Upper Cretaceous (Santonian-...
Larger foraminifera of the late Cretaceous (late Campanian) to middle Eocene (Lutetian) are recogniz...
In order to establish the taxonomy of deep-sea (small) benthic foraminifera and to evaluate their pa...
The Haymana basin in Central Anatolia (Turkey) formed on a Late Cretaceous to Middle Eocene fore ar...
Bu çalışmada Bilecik'in Doğusundaki Geç Jura-Kretase yaşlı birimleri oluşturan yamaç-havza çökelleri...
The Middle Eocene sequence in the Darende-Balaban Basin (Eastern Turkey) characterized by shallow an...
The Baskil section, located to the west of Elazığ in eastern Turkey, represents deep-marine facies o...
The Paleocene-Eocene sequences are widely distributed around onshore and offshore Black Sea. When th...
Larger foraminifera are recognized from the middle Tertiary (Oligocene-Miocene) carbonate sediments,...
WOS: 000371939000010The uppermost Cretaceous (upper Campanian-Maastrichtian) pelagic successions fro...