Upper Oligocene-Lower Miocene diatom assemblages of the submarine Vityaz Ridge (Island slope of the Kuril-Kamchatka trench)

2014 ◽  
Vol 22 (6) ◽  
pp. 618-631 ◽  
Author(s):  
I. B. Tsoy
Keyword(s):  
Diatom Assemblages ◽  
Lower Miocene ◽  
Upper Oligocene ◽  
Submarine Vityaz Ridge ◽  
Vityaz Ridge ◽  
Island Slope

Late Mesozoic and Cenozoic volcanosedimentary complexes from the submarine Vityaz Ridge, the Island Arc slope of the Kuril-Kamchatka trench, and its evolution

2012 ◽  
Vol 6 (3) ◽  
pp. 209-216 ◽  
Author(s):  
E. P. Terekhov ◽  
A. V. Mozherovsky ◽  
I. B. Tsoy ◽  
E. P. Lelikov ◽  
N. G. Vashchenkova ◽  
...  
Keyword(s):  
Island Arc ◽  
Late Mesozoic ◽  
Submarine Vityaz Ridge ◽  
Vityaz Ridge

Geological structure of the submarine Vityaz Ridge within the Seismic Gap area (Pacific slope of the Kurile island arc)

2008 ◽  
Vol 2 (2) ◽  
pp. 99-109 ◽  
Author(s):  
E. P. Lelikov ◽  
I. B. Tsoy ◽  
T. A. Emel’yanova ◽  
E. P. Terekhov ◽  
N. G. Vashchenkova ◽  
...  
Keyword(s):  
Geological Structure ◽  
Island Arc ◽  
Kurile Island ◽  
Seismic Gap ◽  
Submarine Vityaz Ridge ◽  
Vityaz Ridge ◽  
Kurile Island Arc ◽  
Pacific Slope

Foraminiferal Faunas from the Lapithos Group of Cyprus

1961 ◽  
Vol 98 (3) ◽  
pp. 177-194
Author(s):  
A. E. Cockbain
Keyword(s):  
Upper Cretaceous ◽  
Planktonic Foraminifera ◽  
Faunal Assemblage ◽  
Lower Miocene ◽  
Lower Upper ◽  
Upper Oligocene

AbstractThis paper reviews the stratigraphic micropalaeontology of the Lapithos Group of Cyprus, which is now known to be Upper Cretaceous to Lower Miocene in age. A three-fold subdivision, on the basis of planktonic foraminifera, into Lower (Upper Cretaceous) Middle (Danian to Eocene) and Upper (Oligocene to Lower Miocene) Lapithos Formations is suggested and a summary of the outcrops of each formation is given. The foraminiferal faunas of the Lapithos Group are discussed and it can be shown that a planktonic and a neritic faunal assemblage is present in each formation. The Terra Limestone, hitherto considered as part of the Dhali Group, shows faunal affinities with the Upper Lapithos neritic facies and is therefore placed in the Lapithos Group.

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