The Structure and Formation Conditions of the Callovian–Oxfordian Deposits of Sudak Bay (Crimea)

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Abstract

The composition and origin of the Callovian–Oxfordian deposits of the Sudak Bay were characterized on the basis of the generalization and analysis of our own results, as well as published and unpublished data. The botanical future was first implemented for the geological mapping of the Oxfordian deposits.

About the authors

R. R. Gabdullin

Department of Geology

Author for correspondence.
Email: mosgorsun@rambler.ru
Russian Federation, Moscow, 119991

N. V. Badulina

Department of Geology

Email: mosgorsun@rambler.ru
Russian Federation, Moscow, 119991

E. A. Bakai

Department of Geology

Email: mosgorsun@rambler.ru
Russian Federation, Moscow, 119991

E. V. Rubtsova

Department of Geology

Email: mosgorsun@rambler.ru
Russian Federation, Moscow, 119991

A. Yu. Yurchenko

Department of Geology

Email: mosgorsun@rambler.ru
Russian Federation, Moscow, 119991

E. V. Karpova

Department of Geology

Email: mosgorsun@rambler.ru
Russian Federation, Moscow, 119991

A. V. Ivanov

Department of Geology

Email: mosgorsun@rambler.ru
Russian Federation, Moscow, 119991

M. A. Varzanova

Department of Geology

Email: mosgorsun@rambler.ru
Russian Federation, Moscow, 119991

A. V. Sergienko

Department of Geology

Email: mosgorsun@rambler.ru
Russian Federation, Moscow, 119991

T. A. Konovalova

Department of Geology

Email: mosgorsun@rambler.ru
Russian Federation, Moscow, 119991

M. V. Parakhina

Department of Geology

Email: mosgorsun@rambler.ru
Russian Federation, Moscow, 119991

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