Hysteresis characteristics of subaeral deposits in the Baikal region


Дәйексөз келтіру

Толық мәтін

Ашық рұқсат Ашық рұқсат
Рұқсат жабық Рұқсат берілді
Рұқсат жабық Тек жазылушылар үшін

Аннотация

The results of rock magnetic studies in four subaeral cis-Baikalian sections of different ages and geneses are described in detail. The similarities and distinctions in the formation of the magnetic properties of the sediments are established based on the analysis of the magnetic hysteresis parameters. The mechanisms responsible for the dissimilarity of the magnetic characteristics of the rocks in the different sections are identified. The variations in the composition, concentration, and particle size of the grains of magnetic fraction as a function of climate, geomorphologic factors, and volcanism are demonstrated.

Авторлар туралы

A. Kazanskii

Faculty of Geology

Хат алмасуға жауапты Автор.
Email: kazansky-alex@mail.ru
Ресей, Moscow, 119991

G. Matasova

Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch

Email: kazansky-alex@mail.ru
Ресей, Novosibirsk, 630090

A. Shchetnikov

Institute of the Earth’s Crust, Siberian Branch

Email: kazansky-alex@mail.ru
Ресей, Irkutsk, 664033

I. Filinov

Institute of the Earth’s Crust, Siberian Branch

Email: kazansky-alex@mail.ru
Ресей, Irkutsk, 664033

V. Chegis

Faculty of Geology

Email: kazansky-alex@mail.ru
Ресей, Moscow, 119991

Қосымша файлдар

Қосымша файлдар
Әрекет
1. JATS XML

© Pleiades Publishing, Ltd., 2017