Age and chemical composition of altered basalts

Study of morphology of clay minerals formed in altered submarine basalt flow lava has shown that clay-forming process was a continuous-discontinuous one. Basaltic glass was the most readily replaced and laminar-packet aggregates of smectite were produced. Acicular-globular smectites were also formed...

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Bibliographic Details
Main Authors: Kharin, Gennady S, Shevchenko, Alla Ya, Zangalis, K P
Format: Dataset
Language:English
Published: PANGAEA 1979
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.755004
https://doi.org/10.1594/PANGAEA.755004
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.755004
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.755004 2023-05-15T17:31:26+02:00 Age and chemical composition of altered basalts Kharin, Gennady S Shevchenko, Alla Ya Zangalis, K P MEDIAN LATITUDE: 67.354450 * MEDIAN LONGITUDE: -3.289750 * SOUTH-BOUND LATITUDE: 64.871700 * WEST-BOUND LONGITUDE: -5.341800 * NORTH-BOUND LATITUDE: 69.837200 * EAST-BOUND LONGITUDE: -1.237700 * DATE/TIME START: 1974-08-11T00:00:00 * DATE/TIME END: 1974-09-01T00:00:00 1979-12-10 application/zip, 2 datasets https://doi.pangaea.de/10.1594/PANGAEA.755004 https://doi.org/10.1594/PANGAEA.755004 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.755004 https://doi.org/10.1594/PANGAEA.755004 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Kharin, Gennady S; Shevchenko, Alla Ya; Zangalis, K P (1979): Morphology of the smectites in the basalts on the Norwegian Sea floor. Oceanology, 19(3), 284-287 38-337 38-345 Archive of Ocean Data ARCOD Deep Sea Drilling Project DRILL Drilling/drill rig DSDP Glomar Challenger Leg38 North Atlantic/Norwegian Sea/BASIN Dataset 1979 ftpangaea https://doi.org/10.1594/PANGAEA.755004 2023-01-20T07:32:00Z Study of morphology of clay minerals formed in altered submarine basalt flow lava has shown that clay-forming process was a continuous-discontinuous one. Basaltic glass was the most readily replaced and laminar-packet aggregates of smectite were produced. Acicular-globular smectites were also formed from solutions in cavities within basalts. Dataset North Atlantic Norwegian Sea PANGAEA - Data Publisher for Earth & Environmental Science Norwegian Sea ENVELOPE(-5.341800,-1.237700,69.837200,64.871700)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic 38-337
38-345
Archive of Ocean Data
ARCOD
Deep Sea Drilling Project
DRILL
Drilling/drill rig
DSDP
Glomar Challenger
Leg38
North Atlantic/Norwegian Sea/BASIN
spellingShingle 38-337
38-345
Archive of Ocean Data
ARCOD
Deep Sea Drilling Project
DRILL
Drilling/drill rig
DSDP
Glomar Challenger
Leg38
North Atlantic/Norwegian Sea/BASIN
Kharin, Gennady S
Shevchenko, Alla Ya
Zangalis, K P
Age and chemical composition of altered basalts
topic_facet 38-337
38-345
Archive of Ocean Data
ARCOD
Deep Sea Drilling Project
DRILL
Drilling/drill rig
DSDP
Glomar Challenger
Leg38
North Atlantic/Norwegian Sea/BASIN
description Study of morphology of clay minerals formed in altered submarine basalt flow lava has shown that clay-forming process was a continuous-discontinuous one. Basaltic glass was the most readily replaced and laminar-packet aggregates of smectite were produced. Acicular-globular smectites were also formed from solutions in cavities within basalts.
format Dataset
author Kharin, Gennady S
Shevchenko, Alla Ya
Zangalis, K P
author_facet Kharin, Gennady S
Shevchenko, Alla Ya
Zangalis, K P
author_sort Kharin, Gennady S
title Age and chemical composition of altered basalts
title_short Age and chemical composition of altered basalts
title_full Age and chemical composition of altered basalts
title_fullStr Age and chemical composition of altered basalts
title_full_unstemmed Age and chemical composition of altered basalts
title_sort age and chemical composition of altered basalts
publisher PANGAEA
publishDate 1979
url https://doi.pangaea.de/10.1594/PANGAEA.755004
https://doi.org/10.1594/PANGAEA.755004
op_coverage MEDIAN LATITUDE: 67.354450 * MEDIAN LONGITUDE: -3.289750 * SOUTH-BOUND LATITUDE: 64.871700 * WEST-BOUND LONGITUDE: -5.341800 * NORTH-BOUND LATITUDE: 69.837200 * EAST-BOUND LONGITUDE: -1.237700 * DATE/TIME START: 1974-08-11T00:00:00 * DATE/TIME END: 1974-09-01T00:00:00
long_lat ENVELOPE(-5.341800,-1.237700,69.837200,64.871700)
geographic Norwegian Sea
geographic_facet Norwegian Sea
genre North Atlantic
Norwegian Sea
genre_facet North Atlantic
Norwegian Sea
op_source Supplement to: Kharin, Gennady S; Shevchenko, Alla Ya; Zangalis, K P (1979): Morphology of the smectites in the basalts on the Norwegian Sea floor. Oceanology, 19(3), 284-287
op_relation https://doi.pangaea.de/10.1594/PANGAEA.755004
https://doi.org/10.1594/PANGAEA.755004
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/PANGAEA.755004
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