Published 1981 | Version v1
Journal article Metadata-only

On the polychroism of river terraces in mountain areas

Creators

Description

Using the method of 14C isotope dating the age of alluvial deposits of river terraces in mountain areas in Fergana is studied. It is shown that the age of the deposits varies from 16 to 10 thousand years. Their formation as dynamically independent, self-developing systems is pointed out. The role of endo- and exogenous factors in the process of terrace-formation evidently comes to the trigger effect

Additional details

Additional titles

Original title (Russian)
О полихронности горных речных террас

Publishing Information

Journal Title
Dokl. Akad. Nauk SSSR
Journal Volume
257
Journal Issue
6
Series
Dokl. Akad. Nauk SSSR.
Journal Page Range
1430-1432
ISSN
0002-3264

INIS

Country of Publication
Russian Federation
Country of Input or Organization
USSR
INIS RN
14717096
Subject category
S58: GEOSCIENCES;
Descriptors DEI
ALLUVIAL DEPOSITS; CARBON 14; ISOTOPE DATING; SEDIMENTATION
Descriptors DEC
AGE ESTIMATION; BETA DECAY RADIOISOTOPES; BETA-MINUS DECAY RADIOISOTOPES; CARBON ISOTOPES; EVEN-EVEN NUCLEI; GEOLOGIC DEPOSITS; ISOTOPES; LIGHT NUCLEI; NUCLEI; RADIOISOTOPES; YEARS LIVING RADIOISOTOPES