(Table 1) Suspected gas hydrate occurrence on DSDP Leg 66 Holes ...

Evidence for naturally occurring methane hydrates was collected at three drill sites off the southern Mexico continental margin. The hydrates are manifested either by ice inclusions or, more often, as frozen porous volcanic ash and fine sands interlayered with muds. Gas generation from the ice inclu...

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Bibliographic Details
Main Authors: Shipley, Thomas H, Didyk, Borys M
Format: Dataset
Language:English
Published: PANGAEA 1982
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.817733
https://doi.pangaea.de/10.1594/PANGAEA.817733
id ftdatacite:10.1594/pangaea.817733
record_format openpolar
spelling ftdatacite:10.1594/pangaea.817733 2024-09-15T18:18:41+00:00 (Table 1) Suspected gas hydrate occurrence on DSDP Leg 66 Holes ... Shipley, Thomas H Didyk, Borys M 1982 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.817733 https://doi.pangaea.de/10.1594/PANGAEA.817733 en eng PANGAEA https://dx.doi.org/10.2973/dsdp.proc.66.120.1982 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label Latitude of event Longitude of event Elevation of event Sample code/label Depth, top/min Depth, bottom/max DEPTH, sediment/rock Lithology/composition/facies Pressure Temperature, in rock/sediment Ratio Carbon dioxide C1 hydrocarbons C2 hydrocarbons C3 hydrocarbons C4 hydrocarbons C5 hydrocarbons C1/C2+C3 hydrocarbon ratio Description Drilling/drill rig Estimated Leg66 Glomar Challenger Deep Sea Drilling Project DSDP dataset Supplementary Dataset Dataset 1982 ftdatacite https://doi.org/10.1594/pangaea.81773310.2973/dsdp.proc.66.120.1982 2024-08-01T10:51:52Z Evidence for naturally occurring methane hydrates was collected at three drill sites off the southern Mexico continental margin. The hydrates are manifested either by ice inclusions or, more often, as frozen porous volcanic ash and fine sands interlayered with muds. Gas generation from the ice inclusions and interstitial water of the frozen sediment was as high as about 7 ml of gas/ml of water. One large sample immediately placed in a sealed container released about 20 ml of gas/ml of water. All of these values are higher than may be accounted for by gas solubility at in situ conditions. Measured thermal gradients place the bottom-simulating reflection (BSR) in this area very near the phase boundary for the methane hydrate system. This is consistent with earlier interpretations that the BSR is related to the hydrate/gas phase boundary. ... : Sediment depth is given in mbsf. H2S was not detected in any of the samples. ... Dataset Methane hydrate DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Event label
Latitude of event
Longitude of event
Elevation of event
Sample code/label
Depth, top/min
Depth, bottom/max
DEPTH, sediment/rock
Lithology/composition/facies
Pressure
Temperature, in rock/sediment
Ratio
Carbon dioxide
C1 hydrocarbons
C2 hydrocarbons
C3 hydrocarbons
C4 hydrocarbons
C5 hydrocarbons
C1/C2+C3 hydrocarbon ratio
Description
Drilling/drill rig
Estimated
Leg66
Glomar Challenger
Deep Sea Drilling Project DSDP
spellingShingle Event label
Latitude of event
Longitude of event
Elevation of event
Sample code/label
Depth, top/min
Depth, bottom/max
DEPTH, sediment/rock
Lithology/composition/facies
Pressure
Temperature, in rock/sediment
Ratio
Carbon dioxide
C1 hydrocarbons
C2 hydrocarbons
C3 hydrocarbons
C4 hydrocarbons
C5 hydrocarbons
C1/C2+C3 hydrocarbon ratio
Description
Drilling/drill rig
Estimated
Leg66
Glomar Challenger
Deep Sea Drilling Project DSDP
Shipley, Thomas H
Didyk, Borys M
(Table 1) Suspected gas hydrate occurrence on DSDP Leg 66 Holes ...
topic_facet Event label
Latitude of event
Longitude of event
Elevation of event
Sample code/label
Depth, top/min
Depth, bottom/max
DEPTH, sediment/rock
Lithology/composition/facies
Pressure
Temperature, in rock/sediment
Ratio
Carbon dioxide
C1 hydrocarbons
C2 hydrocarbons
C3 hydrocarbons
C4 hydrocarbons
C5 hydrocarbons
C1/C2+C3 hydrocarbon ratio
Description
Drilling/drill rig
Estimated
Leg66
Glomar Challenger
Deep Sea Drilling Project DSDP
description Evidence for naturally occurring methane hydrates was collected at three drill sites off the southern Mexico continental margin. The hydrates are manifested either by ice inclusions or, more often, as frozen porous volcanic ash and fine sands interlayered with muds. Gas generation from the ice inclusions and interstitial water of the frozen sediment was as high as about 7 ml of gas/ml of water. One large sample immediately placed in a sealed container released about 20 ml of gas/ml of water. All of these values are higher than may be accounted for by gas solubility at in situ conditions. Measured thermal gradients place the bottom-simulating reflection (BSR) in this area very near the phase boundary for the methane hydrate system. This is consistent with earlier interpretations that the BSR is related to the hydrate/gas phase boundary. ... : Sediment depth is given in mbsf. H2S was not detected in any of the samples. ...
format Dataset
author Shipley, Thomas H
Didyk, Borys M
author_facet Shipley, Thomas H
Didyk, Borys M
author_sort Shipley, Thomas H
title (Table 1) Suspected gas hydrate occurrence on DSDP Leg 66 Holes ...
title_short (Table 1) Suspected gas hydrate occurrence on DSDP Leg 66 Holes ...
title_full (Table 1) Suspected gas hydrate occurrence on DSDP Leg 66 Holes ...
title_fullStr (Table 1) Suspected gas hydrate occurrence on DSDP Leg 66 Holes ...
title_full_unstemmed (Table 1) Suspected gas hydrate occurrence on DSDP Leg 66 Holes ...
title_sort (table 1) suspected gas hydrate occurrence on dsdp leg 66 holes ...
publisher PANGAEA
publishDate 1982
url https://dx.doi.org/10.1594/pangaea.817733
https://doi.pangaea.de/10.1594/PANGAEA.817733
genre Methane hydrate
genre_facet Methane hydrate
op_relation https://dx.doi.org/10.2973/dsdp.proc.66.120.1982
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.81773310.2973/dsdp.proc.66.120.1982
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