Enregistré dans:
Détails bibliographiques
Auteurs principaux: Tikhomirov, P L, Akinin, V V, Ispolatov, V O, Alexander, P, Cherepanova, I Yu, Zagoskin, V V
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 2006
Sujets:
Accès en ligne:https://doi.org/10.1594/PANGAEA.745668
Tags: Ajouter un tag
Pas de tags, Soyez le premier à ajouter un tag!
_version_ 1867172221877747712
author Tikhomirov, P L
Akinin, V V
Ispolatov, V O
Alexander, P
Cherepanova, I Yu
Zagoskin, V V
author_facet Tikhomirov, P L
Akinin, V V
Ispolatov, V O
Alexander, P
Cherepanova, I Yu
Zagoskin, V V
collection Datos científicos de ciencias marinas y ambientales
contents Current geochronological data on the Okhotsk-Chukotka volcanic belt (OCVB) and relevant problems are discussed. The belt evolution is suggested to be modeled based on 40Ar/39Ar and U-Pb dates more useful in several aspects than common K-Ar or Rb-Sr dates and methods of paleobotanical correlation. Based on new40Ar/39Ar and U-Pb dates obtained for volcanic rocks in the OCVB northern part, the younger (Coniacian) age is established for lower stratigraphic units in the Central Chukotka segment of the belt, and eastward migration of volcanic activity is shown for terminal stages of this structure evolution.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_745668
institution PANGAEA
language en
publishDate 2006
publisher PANGAEA
record_format pangaea
spellingShingle Ages of rocks and minerals from the Okhotsk-Chukotka volcanic belt
Tikhomirov, P L
Akinin, V V
Ispolatov, V O
Alexander, P
Cherepanova, I Yu
Zagoskin, V V
Archive of Ocean Data; ARCOD; OCVB-03-10; OCVB-03-11; OCVB-03-12; OCVB-03-137; OCVB-2403; OCVB-2465; OCVB-2584
Current geochronological data on the Okhotsk-Chukotka volcanic belt (OCVB) and relevant problems are discussed. The belt evolution is suggested to be modeled based on 40Ar/39Ar and U-Pb dates more useful in several aspects than common K-Ar or Rb-Sr dates and methods of paleobotanical correlation. Based on new40Ar/39Ar and U-Pb dates obtained for volcanic rocks in the OCVB northern part, the younger (Coniacian) age is established for lower stratigraphic units in the Central Chukotka segment of the belt, and eastward migration of volcanic activity is shown for terminal stages of this structure evolution.
title Ages of rocks and minerals from the Okhotsk-Chukotka volcanic belt
topic Archive of Ocean Data; ARCOD; OCVB-03-10; OCVB-03-11; OCVB-03-12; OCVB-03-137; OCVB-2403; OCVB-2465; OCVB-2584
url https://doi.org/10.1594/PANGAEA.745668