Geology, geography and global energy

Scientific and Technical Journal

CONTINENTAL DEPOSITS LOWER TRIASSIC WEST OF THE SCYTHIAN PLATE

2020. №1, pp. 38-45

Chaetskiy Victor P. - Kuban State University, geoskubsu@mail.ru

Pinchuk Tatyana N. - Kuban State University, geoskubsu@mail.ru

Popkov Vasily I. - Kuban State University, geoskubsu@mail.ru

Popkov Ivan V. - Kuban State University, iv-popkov@mail.ru

Studies have shown that at the base of the Mesozoic section West of the Scythian plate on a large scale lies a coarse - grained red beds and (or) variegated thickness of continental deposits, in formation with respect to meeting the set top molasses product destruction eigenzinnig folded structures. Its presence is established within Azov-Caucasian structural - facies zone in the absence of Arlievsky-Ledovskoy. The age of the deposits is assumed to be Indian. It is proposed to combine this complex of rocks as the leushkov formation by the name of the square of the same name, where the most representative section of sediments was opened by wells.

Key words: нижний триас, верхняя моласса, формация, свита, lower Triassic, upper molasses, formation, Suite

Read