BIVALVE FAUNAS OF THE OLIGOCENE KHOLMSKAYA FORMATION (SOUTHWESTERN SAKHALIN) AND THE AGE VALIDITY OF THE HOST SEDIMENTS ...

The results of studying the remains of the Oligocene faunas of bivalves from the sedimentary deposits of the Kholmskaya Formation, developed in southwestern Sakhalin, are considered. As part of the fauna of the stratotype suite along the river Pravda the presence of Bivalve mollusks Mya grewingki (M...

Full description

Bibliographic Details
Main Author: Khudik, V.D.
Format: Text
Language:English
Published: Инфинити 2024
Subjects:
Online Access:https://dx.doi.org/10.34660/inf.2024.16.70.014
http://search.rads-doi.org/project/14060/object/205516
id ftdatacite:10.34660/inf.2024.16.70.014
record_format openpolar
spelling ftdatacite:10.34660/inf.2024.16.70.014 2024-02-27T08:45:09+00:00 BIVALVE FAUNAS OF THE OLIGOCENE KHOLMSKAYA FORMATION (SOUTHWESTERN SAKHALIN) AND THE AGE VALIDITY OF THE HOST SEDIMENTS ... Khudik, V.D. 2024 https://dx.doi.org/10.34660/inf.2024.16.70.014 http://search.rads-doi.org/project/14060/object/205516 en eng Инфинити http://search.rads-doi.org/project/14060 Bivalve mollusks Oligocene southwestern Sakhalin article-journal ScholarlyArticle Text Conference Paper 2024 ftdatacite https://doi.org/10.34660/inf.2024.16.70.014 2024-02-01T15:48:05Z The results of studying the remains of the Oligocene faunas of bivalves from the sedimentary deposits of the Kholmskaya Formation, developed in southwestern Sakhalin, are considered. As part of the fauna of the stratotype suite along the river Pravda the presence of Bivalve mollusks Mya grewingki (Makiyama) was established throughout the section. This circumstance, taking into account the geological age of the taxon, made it possible to confirm the Upper Oligocene age for the strata of the Kholmskaya Formation hosting the fauna. ... Text Sakhalin DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Bivalve mollusks
Oligocene
southwestern Sakhalin
spellingShingle Bivalve mollusks
Oligocene
southwestern Sakhalin
Khudik, V.D.
BIVALVE FAUNAS OF THE OLIGOCENE KHOLMSKAYA FORMATION (SOUTHWESTERN SAKHALIN) AND THE AGE VALIDITY OF THE HOST SEDIMENTS ...
topic_facet Bivalve mollusks
Oligocene
southwestern Sakhalin
description The results of studying the remains of the Oligocene faunas of bivalves from the sedimentary deposits of the Kholmskaya Formation, developed in southwestern Sakhalin, are considered. As part of the fauna of the stratotype suite along the river Pravda the presence of Bivalve mollusks Mya grewingki (Makiyama) was established throughout the section. This circumstance, taking into account the geological age of the taxon, made it possible to confirm the Upper Oligocene age for the strata of the Kholmskaya Formation hosting the fauna. ...
format Text
author Khudik, V.D.
author_facet Khudik, V.D.
author_sort Khudik, V.D.
title BIVALVE FAUNAS OF THE OLIGOCENE KHOLMSKAYA FORMATION (SOUTHWESTERN SAKHALIN) AND THE AGE VALIDITY OF THE HOST SEDIMENTS ...
title_short BIVALVE FAUNAS OF THE OLIGOCENE KHOLMSKAYA FORMATION (SOUTHWESTERN SAKHALIN) AND THE AGE VALIDITY OF THE HOST SEDIMENTS ...
title_full BIVALVE FAUNAS OF THE OLIGOCENE KHOLMSKAYA FORMATION (SOUTHWESTERN SAKHALIN) AND THE AGE VALIDITY OF THE HOST SEDIMENTS ...
title_fullStr BIVALVE FAUNAS OF THE OLIGOCENE KHOLMSKAYA FORMATION (SOUTHWESTERN SAKHALIN) AND THE AGE VALIDITY OF THE HOST SEDIMENTS ...
title_full_unstemmed BIVALVE FAUNAS OF THE OLIGOCENE KHOLMSKAYA FORMATION (SOUTHWESTERN SAKHALIN) AND THE AGE VALIDITY OF THE HOST SEDIMENTS ...
title_sort bivalve faunas of the oligocene kholmskaya formation (southwestern sakhalin) and the age validity of the host sediments ...
publisher Инфинити
publishDate 2024
url https://dx.doi.org/10.34660/inf.2024.16.70.014
http://search.rads-doi.org/project/14060/object/205516
genre Sakhalin
genre_facet Sakhalin
op_relation http://search.rads-doi.org/project/14060
op_doi https://doi.org/10.34660/inf.2024.16.70.014
_version_ 1792054240529612800