Estimation of cooling of lavas from Serocki volcano
A dynamic crystallization study was undertaken to provide a framework for linking the textural variations observed in the Hole 648B lavas with the size and morphology of cooling units inferred from drilling and submersible observation. The textures produced in cooling rate experiments carried out us...
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1990
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.745880 2024-09-15T18:23:34+00:00 Estimation of cooling of lavas from Serocki volcano Grove, Timothy L MEDIAN LATITUDE: 22.919350 * MEDIAN LONGITUDE: -44.948550 * SOUTH-BOUND LATITUDE: 22.916700 * WEST-BOUND LONGITUDE: -44.950000 * NORTH-BOUND LATITUDE: 22.922000 * EAST-BOUND LONGITUDE: -44.947100 * DATE/TIME START: 1986-04-29T04:00:00 * DATE/TIME END: 1986-05-31T04:30:00 1990 application/zip, 2 datasets https://doi.pangaea.de/10.1594/PANGAEA.745880 https://doi.org/10.1594/PANGAEA.745880 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.745880 https://doi.org/10.1594/PANGAEA.745880 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Grove, Timothy L (1990): Cooling histories of lavas from Serocki Volcano. In: Detrick, R; Honnorez, J; Bryan, WB; Juteau, T; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 106/109, 3-8, https://doi.org/10.2973/odp.proc.sr.106109.113.1990 109-648B Alv_dive_1690 DRILL Drilling/drill rig Joides Resolution Leg109 Mid-Atlantic Ridge North Atlantic Ocean Ocean Drilling Program ODP Serocki Volcano dataset publication series 1990 ftpangaea https://doi.org/10.1594/PANGAEA.74588010.2973/odp.proc.sr.106109.113.1990 2024-08-21T00:02:25Z A dynamic crystallization study was undertaken to provide a framework for linking the textural variations observed in the Hole 648B lavas with the size and morphology of cooling units inferred from drilling and submersible observation. The textures produced in cooling rate experiments carried out using a Serocki lava (ALV-1690-20) are comparable to the groundmass textural characteristics of lavas from Serocki volcano. The results of the dynamic crystallization study provide a quantitative link between texture, cooling rate, and eruption temperature. The maximum half-width of cooling units estimated from textural characteristics is on the order of 3 m, a value consistent with constraints from drilling and submersible observation. Textural characteristics indicate that the temperature from which cooling began was slightly above the liquidus. The relation between cooling rate and texture are also tested on a drill core sample of basalt of similar composition from a 9-m-thick flow in DSDP Hole 396B. Other/Unknown Material North Atlantic PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-44.950000,-44.947100,22.922000,22.916700) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
109-648B Alv_dive_1690 DRILL Drilling/drill rig Joides Resolution Leg109 Mid-Atlantic Ridge North Atlantic Ocean Ocean Drilling Program ODP Serocki Volcano |
spellingShingle |
109-648B Alv_dive_1690 DRILL Drilling/drill rig Joides Resolution Leg109 Mid-Atlantic Ridge North Atlantic Ocean Ocean Drilling Program ODP Serocki Volcano Grove, Timothy L Estimation of cooling of lavas from Serocki volcano |
topic_facet |
109-648B Alv_dive_1690 DRILL Drilling/drill rig Joides Resolution Leg109 Mid-Atlantic Ridge North Atlantic Ocean Ocean Drilling Program ODP Serocki Volcano |
description |
A dynamic crystallization study was undertaken to provide a framework for linking the textural variations observed in the Hole 648B lavas with the size and morphology of cooling units inferred from drilling and submersible observation. The textures produced in cooling rate experiments carried out using a Serocki lava (ALV-1690-20) are comparable to the groundmass textural characteristics of lavas from Serocki volcano. The results of the dynamic crystallization study provide a quantitative link between texture, cooling rate, and eruption temperature. The maximum half-width of cooling units estimated from textural characteristics is on the order of 3 m, a value consistent with constraints from drilling and submersible observation. Textural characteristics indicate that the temperature from which cooling began was slightly above the liquidus. The relation between cooling rate and texture are also tested on a drill core sample of basalt of similar composition from a 9-m-thick flow in DSDP Hole 396B. |
format |
Other/Unknown Material |
author |
Grove, Timothy L |
author_facet |
Grove, Timothy L |
author_sort |
Grove, Timothy L |
title |
Estimation of cooling of lavas from Serocki volcano |
title_short |
Estimation of cooling of lavas from Serocki volcano |
title_full |
Estimation of cooling of lavas from Serocki volcano |
title_fullStr |
Estimation of cooling of lavas from Serocki volcano |
title_full_unstemmed |
Estimation of cooling of lavas from Serocki volcano |
title_sort |
estimation of cooling of lavas from serocki volcano |
publisher |
PANGAEA |
publishDate |
1990 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.745880 https://doi.org/10.1594/PANGAEA.745880 |
op_coverage |
MEDIAN LATITUDE: 22.919350 * MEDIAN LONGITUDE: -44.948550 * SOUTH-BOUND LATITUDE: 22.916700 * WEST-BOUND LONGITUDE: -44.950000 * NORTH-BOUND LATITUDE: 22.922000 * EAST-BOUND LONGITUDE: -44.947100 * DATE/TIME START: 1986-04-29T04:00:00 * DATE/TIME END: 1986-05-31T04:30:00 |
long_lat |
ENVELOPE(-44.950000,-44.947100,22.922000,22.916700) |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Supplement to: Grove, Timothy L (1990): Cooling histories of lavas from Serocki Volcano. In: Detrick, R; Honnorez, J; Bryan, WB; Juteau, T; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 106/109, 3-8, https://doi.org/10.2973/odp.proc.sr.106109.113.1990 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.745880 https://doi.org/10.1594/PANGAEA.745880 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.74588010.2973/odp.proc.sr.106109.113.1990 |
_version_ |
1810463805083222016 |