In:
Океанология, The Russian Academy of Sciences, Vol. 59, No. 4 ( 2019-09-17), p. 617-640
Abstract:
The data on mineralogical analysis of fine sand fractions in sediments accumulated in the southern part of the Chukchi Plateau during the Quaternary are presented. The associations and downcore distribution of the rock-forming and accessory minerals in relation to other characteristics are considered. The established climatically controlled mineralogical features, i. e. periodicity of warmings and coolings, can be used in solving a number of genetic problems, stratigraphic subdivision of sediments and paleoreconstructions.
Type of Medium:
Online Resource
ISSN:
0030-1574
DOI:
10.31857/S0030-1574594
DOI:
10.31857/S0030-1574594617-640
DOI:
10.31857/S0030-1574594617-640-14784
DOI:
10.31857/S0030-1574594617-640-14785
DOI:
10.31857/S0030-1574594617-640-14786
DOI:
10.31857/S0030-1574594617-640-14787
Language:
Unknown
Publisher:
The Russian Academy of Sciences
Publication Date:
2019
detail.hit.zdb_id:
3001842-0
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