ON THE INFLUENCE OF HOLOCENE TECTONICS ON THE FORMATION OF THE RIVER NETWORK OF THE ALPINE-HIMALAYAN AND PACIFIC MOBILE BELTS OF EURASIA

This article continues the series of publications on the indicators of Holocene activation. Using the examples of the Volga and Amur rivers with their tributaries and the Razdolnaya River, the interaction of the river network with the Holocene orogenic system of the Alpine-Himalayan and Pacific mobile belts of Eurasia was studied. The river network is conformal to their orogenic system. Examples of the control of river valleys by shear systems of active faults are given. The influence of the rivers on the formation of erosional relief was studied. It is shown that loose sediments of the Mesozoic-Cenozoic rifts thrown up in the Holocene are actively destroyed by the river network, with a shear of up to many hundreds of meters. The rises on the riftogen framing and their internal rises, composed of strong pre-Mesozoic rocks, are weakly eroded. Many of them have a contrasting, nonequilibrium relief. The study was conducted within the framework of the pulsatingly expanding Earth model developed by the author.

Authors

Publication Details

Journal
THE LIFE OF THE EARTH
Published
2024-12-04
DOI
https://doi.org/10.29003/m4334.0514-7468.2020_46_4/455-471
Primary Topic
Geological Studies and Exploration
Type
article
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article

ON THE INFLUENCE OF HOLOCENE TECTONICS ON THE FORMATION OF THE RIVER NETWORK OF THE ALPINE-HIMALAYAN AND PACIFIC MOBILE BELTS OF EURASIA

Alexander Alexandrovich Kokovkin
THE LIFE OF THE EARTH
Geological Studies and Exploration
article

ON THE INFLUENCE OF HOLOCENE TECTONICS ON THE FORMATION OF THE RIVER NETWORK OF THE ALPINE-HIMALAYAN AND PACIFIC MOBILE BELTS OF EURASIA

Alexander Alexandrovich Kokovkin
article en

Abstract

This article continues the series of publications on the indicators of Holocene activation. Using the examples of the Volga and Amur rivers with their tributaries and the Razdolnaya River, the interaction of the river network with the Holocene orogenic system of the Alpine-Himalayan and Pacific mobile belts of Eurasia was studied. The river network is conformal to their orogenic system. Examples of the control of river valleys by shear systems of active faults are given. The influence of the rivers on the formation of erosional relief was studied. It is shown that loose sediments of the Mesozoic-Cenozoic rifts thrown up in the Holocene are actively destroyed by the river network, with a shear of up to many hundreds of meters. The rises on the riftogen framing and their internal rises, composed of strong pre-Mesozoic rocks, are weakly eroded. Many of them have a contrasting, nonequilibrium relief. The study was conducted within the framework of the pulsatingly expanding Earth model developed by the author.

THE LIFE OF THE EARTHVol. 46(4)
Openalex Percentile: Top 49%
Geological Studies and Exploration
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