(Table T1) Fluid inclusions in siltstone and sandstone grains from ODP Hole 210-1276A ...
Twenty samples of siltstones and sandstones were taken from Ocean Drilling Program Site 1276 during Leg 210 for fluid inclusion studies. With the exception of one sample of vein calcite, all inclusions were in quartz grains. The results of fluid-inclusion petrology and microthermometry indicate the...
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ftdatacite:10.1594/pangaea.776731 2024-09-30T14:38:55+00:00 (Table T1) Fluid inclusions in siltstone and sandstone grains from ODP Hole 210-1276A ... Shryane, Thérèse Feely, Martin 2007 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.776731 https://doi.pangaea.de/10.1594/PANGAEA.776731 en eng PANGAEA https://dx.doi.org/10.2973/odp.proc.sr.210.108.2007 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Sample code/label Number Length Area in square milimeter Ratio Salinity Melting temperature Homogenization temperature Sample comment Host Drilling/drill rig DSDP/ODP/IODP sample designation Estimated Leg210 Joides Resolution Ocean Drilling Program ODP Supplementary Dataset Dataset dataset 2007 ftdatacite https://doi.org/10.1594/pangaea.77673110.2973/odp.proc.sr.210.108.2007 2024-09-02T08:36:09Z Twenty samples of siltstones and sandstones were taken from Ocean Drilling Program Site 1276 during Leg 210 for fluid inclusion studies. With the exception of one sample of vein calcite, all inclusions were in quartz grains. The results of fluid-inclusion petrology and microthermometry indicate the presence of three fluid inclusion types (Types 1, 2, and 3). Type 1 fluid inclusions are two-phase (liquid + vapor) aqueous inclusions, and Type 2 inclusions are monophase fluid inclusions (liquid or vapor). These are common in all samples and are formed either as primary isolated inclusions or as secondary inclusions as trails along annealed fractures in the grain. Type 3 fluid inclusions are three-phase (liquid + vapor + solid) inclusions. Type 3 inclusions are rare and are observed as isolated inclusions or in a cluster with other types (i.e., Types 1 and 2). The predominant population throughout the different units sampled is two-phase (liquid + vapor) aqueous fluid inclusions (i.e., Type 1). The temperature ... : Supplement to: Shryane, Thérèse; Feely, Martin (2007): Data report: Fluid inclusion studies of detrital quartz from the Newfoundland Basin, ODP Leg 210, Site 1276. In: Tucholke, BE; Sibuet, J-C; Klaus, A (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 210, 1-21 ... Dataset Newfoundland DataCite Klaus ENVELOPE(24.117,24.117,65.717,65.717) |
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ftdatacite |
language |
English |
topic |
Sample code/label Number Length Area in square milimeter Ratio Salinity Melting temperature Homogenization temperature Sample comment Host Drilling/drill rig DSDP/ODP/IODP sample designation Estimated Leg210 Joides Resolution Ocean Drilling Program ODP |
spellingShingle |
Sample code/label Number Length Area in square milimeter Ratio Salinity Melting temperature Homogenization temperature Sample comment Host Drilling/drill rig DSDP/ODP/IODP sample designation Estimated Leg210 Joides Resolution Ocean Drilling Program ODP Shryane, Thérèse Feely, Martin (Table T1) Fluid inclusions in siltstone and sandstone grains from ODP Hole 210-1276A ... |
topic_facet |
Sample code/label Number Length Area in square milimeter Ratio Salinity Melting temperature Homogenization temperature Sample comment Host Drilling/drill rig DSDP/ODP/IODP sample designation Estimated Leg210 Joides Resolution Ocean Drilling Program ODP |
description |
Twenty samples of siltstones and sandstones were taken from Ocean Drilling Program Site 1276 during Leg 210 for fluid inclusion studies. With the exception of one sample of vein calcite, all inclusions were in quartz grains. The results of fluid-inclusion petrology and microthermometry indicate the presence of three fluid inclusion types (Types 1, 2, and 3). Type 1 fluid inclusions are two-phase (liquid + vapor) aqueous inclusions, and Type 2 inclusions are monophase fluid inclusions (liquid or vapor). These are common in all samples and are formed either as primary isolated inclusions or as secondary inclusions as trails along annealed fractures in the grain. Type 3 fluid inclusions are three-phase (liquid + vapor + solid) inclusions. Type 3 inclusions are rare and are observed as isolated inclusions or in a cluster with other types (i.e., Types 1 and 2). The predominant population throughout the different units sampled is two-phase (liquid + vapor) aqueous fluid inclusions (i.e., Type 1). The temperature ... : Supplement to: Shryane, Thérèse; Feely, Martin (2007): Data report: Fluid inclusion studies of detrital quartz from the Newfoundland Basin, ODP Leg 210, Site 1276. In: Tucholke, BE; Sibuet, J-C; Klaus, A (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 210, 1-21 ... |
format |
Dataset |
author |
Shryane, Thérèse Feely, Martin |
author_facet |
Shryane, Thérèse Feely, Martin |
author_sort |
Shryane, Thérèse |
title |
(Table T1) Fluid inclusions in siltstone and sandstone grains from ODP Hole 210-1276A ... |
title_short |
(Table T1) Fluid inclusions in siltstone and sandstone grains from ODP Hole 210-1276A ... |
title_full |
(Table T1) Fluid inclusions in siltstone and sandstone grains from ODP Hole 210-1276A ... |
title_fullStr |
(Table T1) Fluid inclusions in siltstone and sandstone grains from ODP Hole 210-1276A ... |
title_full_unstemmed |
(Table T1) Fluid inclusions in siltstone and sandstone grains from ODP Hole 210-1276A ... |
title_sort |
(table t1) fluid inclusions in siltstone and sandstone grains from odp hole 210-1276a ... |
publisher |
PANGAEA |
publishDate |
2007 |
url |
https://dx.doi.org/10.1594/pangaea.776731 https://doi.pangaea.de/10.1594/PANGAEA.776731 |
long_lat |
ENVELOPE(24.117,24.117,65.717,65.717) |
geographic |
Klaus |
geographic_facet |
Klaus |
genre |
Newfoundland |
genre_facet |
Newfoundland |
op_relation |
https://dx.doi.org/10.2973/odp.proc.sr.210.108.2007 |
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.77673110.2973/odp.proc.sr.210.108.2007 |
_version_ |
1811641509164875776 |