Chemical characteristics of ash layers from ODP Leg 104 ...

Forty-five volcanic ash horizons cored at Sites 642, 643, and 644 on the Vøring Plateau and ranging in age from early Miocene to Pleistocene, are discussed in terms of their magmatic features as well as their diagenetic evolution. Most of these layers, some centimeters thick, are mainly made of fres...

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Main Authors: Desprairies, Alain, Maury, R C, Joron, Jean Louis, Bohn, Marcel, Tremblay, P
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1989
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.737126
https://doi.pangaea.de/10.1594/PANGAEA.737126
id ftdatacite:10.1594/pangaea.737126
record_format openpolar
spelling ftdatacite:10.1594/pangaea.737126 2024-09-15T18:23:39+00:00 Chemical characteristics of ash layers from ODP Leg 104 ... Desprairies, Alain Maury, R C Joron, Jean Louis Bohn, Marcel Tremblay, P 1989 application/zip https://dx.doi.org/10.1594/pangaea.737126 https://doi.pangaea.de/10.1594/PANGAEA.737126 en eng PANGAEA https://dx.doi.org/10.2973/odp.proc.sr.104.120.1989 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Composite Core Leg81 Leg104 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 1989 ftdatacite https://doi.org/10.1594/pangaea.73712610.2973/odp.proc.sr.104.120.1989 2024-08-01T10:54:23Z Forty-five volcanic ash horizons cored at Sites 642, 643, and 644 on the Vøring Plateau and ranging in age from early Miocene to Pleistocene, are discussed in terms of their magmatic features as well as their diagenetic evolution. Most of these layers, some centimeters thick, are mainly made of fresh rhyolitic glass. Twenty-five percent of the ash layers, however, contain variable amounts of more basic glass shards, ranging in composition from Mg-rich tholeiites to icelandites through Mg-poor basalts, ferrobasalts, and tholeiitic andesites, and are commonly associated with rhyolitic shards.Many chemically heterogeneous ash layers show bimodal acidic (rhyolites to icelandites) - basic (Mg-rich basalts to ferrobasalts) frequency distributions of the glass shards; intermediate compositions are not simple mixtures between acidic and basic endmembers. We suggest these ash layers result from the ejection of the upper (rhyolitic) to intermediate (ferrobasaltic) levels of density-stratified magma chambers intruded ... : Supplement to: Desprairies, Alain; Maury, R C; Joron, Jean Louis; Bohn, Marcel; Tremblay, P (1989): Distribution, chemical characteristics, and origin of ash layers from ODP Leg 104, Vøring Plateau, North Atlantic. In: Eldholm, O; Thiede, J; Taylor, E; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 104, 337-356 ... Article in Journal/Newspaper North Atlantic DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Drilling/drill rig
Composite Core
Leg81
Leg104
Glomar Challenger
Joides Resolution
Deep Sea Drilling Project DSDP
Ocean Drilling Program ODP
spellingShingle Drilling/drill rig
Composite Core
Leg81
Leg104
Glomar Challenger
Joides Resolution
Deep Sea Drilling Project DSDP
Ocean Drilling Program ODP
Desprairies, Alain
Maury, R C
Joron, Jean Louis
Bohn, Marcel
Tremblay, P
Chemical characteristics of ash layers from ODP Leg 104 ...
topic_facet Drilling/drill rig
Composite Core
Leg81
Leg104
Glomar Challenger
Joides Resolution
Deep Sea Drilling Project DSDP
Ocean Drilling Program ODP
description Forty-five volcanic ash horizons cored at Sites 642, 643, and 644 on the Vøring Plateau and ranging in age from early Miocene to Pleistocene, are discussed in terms of their magmatic features as well as their diagenetic evolution. Most of these layers, some centimeters thick, are mainly made of fresh rhyolitic glass. Twenty-five percent of the ash layers, however, contain variable amounts of more basic glass shards, ranging in composition from Mg-rich tholeiites to icelandites through Mg-poor basalts, ferrobasalts, and tholeiitic andesites, and are commonly associated with rhyolitic shards.Many chemically heterogeneous ash layers show bimodal acidic (rhyolites to icelandites) - basic (Mg-rich basalts to ferrobasalts) frequency distributions of the glass shards; intermediate compositions are not simple mixtures between acidic and basic endmembers. We suggest these ash layers result from the ejection of the upper (rhyolitic) to intermediate (ferrobasaltic) levels of density-stratified magma chambers intruded ... : Supplement to: Desprairies, Alain; Maury, R C; Joron, Jean Louis; Bohn, Marcel; Tremblay, P (1989): Distribution, chemical characteristics, and origin of ash layers from ODP Leg 104, Vøring Plateau, North Atlantic. In: Eldholm, O; Thiede, J; Taylor, E; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 104, 337-356 ...
format Article in Journal/Newspaper
author Desprairies, Alain
Maury, R C
Joron, Jean Louis
Bohn, Marcel
Tremblay, P
author_facet Desprairies, Alain
Maury, R C
Joron, Jean Louis
Bohn, Marcel
Tremblay, P
author_sort Desprairies, Alain
title Chemical characteristics of ash layers from ODP Leg 104 ...
title_short Chemical characteristics of ash layers from ODP Leg 104 ...
title_full Chemical characteristics of ash layers from ODP Leg 104 ...
title_fullStr Chemical characteristics of ash layers from ODP Leg 104 ...
title_full_unstemmed Chemical characteristics of ash layers from ODP Leg 104 ...
title_sort chemical characteristics of ash layers from odp leg 104 ...
publisher PANGAEA
publishDate 1989
url https://dx.doi.org/10.1594/pangaea.737126
https://doi.pangaea.de/10.1594/PANGAEA.737126
genre North Atlantic
genre_facet North Atlantic
op_relation https://dx.doi.org/10.2973/odp.proc.sr.104.120.1989
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.73712610.2973/odp.proc.sr.104.120.1989
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