ScholarLens Back to search
2015•Geomorphology RASRequires access

TRANSGRESSIONS ON THE MURMAN AND WHITE SEA COASTS IN THE LATE PLEISTOCENE–HOLOCENE IN CONNECTION WITH DEGLACIATION

V. Yа. Yevzerov

Open publisher page 3 citations

Abstract

Continental ice had blocked the sea advance onto land till the end of the Allerod. Transgression began to the Murmansk coast in the Bolling after deglaciation of south-east part of the Barents Sea shelf. The farthest spread of the sea onto Murmansk coast and in the White Sea Basin took place in the end of the Allerod after deglaciation of the coasts and the White Sea depression. Then, regression took place on the most part of the coasts. The following transgression flooded the previously glaciated area and its vicinity in the Younger Dryas. The subsequent regression began at the end of the Younger Dryas. The third transgression (Tapes) took place in the Holocene.

About this research paper

What this paper is about

Continental ice had blocked the sea advance onto land till the end of the Allerod. Transgression began to the Murmansk coast in the Bolling after deglaciation of south-east part of the Barents Sea shelf. The farthest spread of the sea onto Murmansk coast and in the White Sea Basin took place in the end of the Allerod after deglaciation of the coasts and the White Sea depression. Then, regression took place on the most part of the coasts. The following transgression flooded the previously glaciated area and its vicinity in the Younger Dryas. The subsequent regression began at the end of the Younger Dryas. The third transgression (Tapes) took place in the Holocene.

Why it matters

OpenAlex reports 3 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

Continental ice had blocked the sea advance onto land till the end of the Allerod. Transgression began to the Murmansk coast in the Bolling after deglaciation of south-east part of the Barents Sea shelf. The farthest spread of the sea onto Murmansk coast and in the White Sea Basin took place in the end of the Allerod after deglaciation of the coasts and the White Sea depression. Then, regression took place on the most part of the coasts. The following transgression flooded the previously glaciated area and its vicinity in the Younger Dryas. The subsequent regression began at the end of the Younger Dryas. The third transgression (Tapes) took place in the Holocene.

Key concepts: Deglaciation, Younger Dryas, Marine transgression, Allerød oscillation, Holocene, Geology, Pleistocene, Oceanography

Related papers

Related paper 1Related paper 2Related paper 3
Back to paper searchBrowse research topicsOriginal source
TRANSGRESSIONS ON THE MURMAN AND WHITE SEA COASTS IN THE LATE PLEISTOCENE–HOLOCENE IN CONNECTION WITH DEGLACIATION — Research Paper | ScholarLens