Monitoring the Spanish gas fields in the Ría de Vigo (1991–2001)
Abstract The Ría de Vigo is located on the NW coast of Spain, and includes gassy areas studied in several high-resolution seismic surveys between 1991 and 2001. The position of the acoustic blankings and gas seepages has been monitored vertically and spatially in the surveyed area. Also, a 253-cm-lo...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
García-García, A. [verfasserIn] García-Gil, S. [verfasserIn] Vilas, F. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2003 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Geo-marine letters - Berlin : Springer, 1984, 23(2003), 3-4 vom: 17. Okt., Seite 200-206 |
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| Übergeordnetes Werk: |
volume:23 ; year:2003 ; number:3-4 ; day:17 ; month:10 ; pages:200-206 |
| Links: |
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| DOI / URN: |
10.1007/s00367-003-0147-9 |
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| Katalog-ID: |
SPR004570952 |
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| 520 | |a Abstract The Ría de Vigo is located on the NW coast of Spain, and includes gassy areas studied in several high-resolution seismic surveys between 1991 and 2001. The position of the acoustic blankings and gas seepages has been monitored vertically and spatially in the surveyed area. Also, a 253-cm-long vibrocore was recovered in a gas field in the inner part of the ría. The predominant facies of the core is dark mud with small bioclastic fragments and a very strong $ H_{2} $S smell. The repeated surveys of this ría show that these shallow gas fields have been active in the last decade and were active in the past (buried collapse structures). Available direct gas analyses show that methane is one of the components of the gas in the ría. Thus, bacterial degradation of organic matter in shallow sediments is considered the most likely source for the gas in the Ría de Vigo. | ||
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| 650 | 4 | |a Seismic Stratigraphy |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Acoustic Blankings |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a García-Gil, S. |e verfasserin |4 aut | |
| 700 | 1 | |a Vilas, F. |e verfasserin |4 aut | |
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10.1007/s00367-003-0147-9 doi (DE-627)SPR004570952 (SPR)s00367-003-0147-9-e DE-627 ger DE-627 rakwb eng 550 ASE 38.48 bkl García-García, A. verfasserin aut Monitoring the Spanish gas fields in the Ría de Vigo (1991–2001) 2003 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The Ría de Vigo is located on the NW coast of Spain, and includes gassy areas studied in several high-resolution seismic surveys between 1991 and 2001. The position of the acoustic blankings and gas seepages has been monitored vertically and spatially in the surveyed area. Also, a 253-cm-long vibrocore was recovered in a gas field in the inner part of the ría. The predominant facies of the core is dark mud with small bioclastic fragments and a very strong $ H_{2} $S smell. The repeated surveys of this ría show that these shallow gas fields have been active in the last decade and were active in the past (buried collapse structures). Available direct gas analyses show that methane is one of the components of the gas in the ría. Thus, bacterial degradation of organic matter in shallow sediments is considered the most likely source for the gas in the Ría de Vigo. Seismic Line (dpeaa)DE-He213 Collapse Structure (dpeaa)DE-He213 Seismic Unit (dpeaa)DE-He213 Seismic Stratigraphy (dpeaa)DE-He213 Acoustic Blankings (dpeaa)DE-He213 García-Gil, S. verfasserin aut Vilas, F. verfasserin aut Enthalten in Geo-marine letters Berlin : Springer, 1984 23(2003), 3-4 vom: 17. Okt., Seite 200-206 (DE-627)300183690 (DE-600)1481423-7 1432-1157 nnns volume:23 year:2003 number:3-4 day:17 month:10 pages:200-206 https://dx.doi.org/10.1007/s00367-003-0147-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_612 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.48 ASE AR 23 2003 3-4 17 10 200-206 |
| spelling |
10.1007/s00367-003-0147-9 doi (DE-627)SPR004570952 (SPR)s00367-003-0147-9-e DE-627 ger DE-627 rakwb eng 550 ASE 38.48 bkl García-García, A. verfasserin aut Monitoring the Spanish gas fields in the Ría de Vigo (1991–2001) 2003 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The Ría de Vigo is located on the NW coast of Spain, and includes gassy areas studied in several high-resolution seismic surveys between 1991 and 2001. The position of the acoustic blankings and gas seepages has been monitored vertically and spatially in the surveyed area. Also, a 253-cm-long vibrocore was recovered in a gas field in the inner part of the ría. The predominant facies of the core is dark mud with small bioclastic fragments and a very strong $ H_{2} $S smell. The repeated surveys of this ría show that these shallow gas fields have been active in the last decade and were active in the past (buried collapse structures). Available direct gas analyses show that methane is one of the components of the gas in the ría. Thus, bacterial degradation of organic matter in shallow sediments is considered the most likely source for the gas in the Ría de Vigo. Seismic Line (dpeaa)DE-He213 Collapse Structure (dpeaa)DE-He213 Seismic Unit (dpeaa)DE-He213 Seismic Stratigraphy (dpeaa)DE-He213 Acoustic Blankings (dpeaa)DE-He213 García-Gil, S. verfasserin aut Vilas, F. verfasserin aut Enthalten in Geo-marine letters Berlin : Springer, 1984 23(2003), 3-4 vom: 17. Okt., Seite 200-206 (DE-627)300183690 (DE-600)1481423-7 1432-1157 nnns volume:23 year:2003 number:3-4 day:17 month:10 pages:200-206 https://dx.doi.org/10.1007/s00367-003-0147-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_612 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.48 ASE AR 23 2003 3-4 17 10 200-206 |
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10.1007/s00367-003-0147-9 doi (DE-627)SPR004570952 (SPR)s00367-003-0147-9-e DE-627 ger DE-627 rakwb eng 550 ASE 38.48 bkl García-García, A. verfasserin aut Monitoring the Spanish gas fields in the Ría de Vigo (1991–2001) 2003 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The Ría de Vigo is located on the NW coast of Spain, and includes gassy areas studied in several high-resolution seismic surveys between 1991 and 2001. The position of the acoustic blankings and gas seepages has been monitored vertically and spatially in the surveyed area. Also, a 253-cm-long vibrocore was recovered in a gas field in the inner part of the ría. The predominant facies of the core is dark mud with small bioclastic fragments and a very strong $ H_{2} $S smell. The repeated surveys of this ría show that these shallow gas fields have been active in the last decade and were active in the past (buried collapse structures). Available direct gas analyses show that methane is one of the components of the gas in the ría. Thus, bacterial degradation of organic matter in shallow sediments is considered the most likely source for the gas in the Ría de Vigo. Seismic Line (dpeaa)DE-He213 Collapse Structure (dpeaa)DE-He213 Seismic Unit (dpeaa)DE-He213 Seismic Stratigraphy (dpeaa)DE-He213 Acoustic Blankings (dpeaa)DE-He213 García-Gil, S. verfasserin aut Vilas, F. verfasserin aut Enthalten in Geo-marine letters Berlin : Springer, 1984 23(2003), 3-4 vom: 17. Okt., Seite 200-206 (DE-627)300183690 (DE-600)1481423-7 1432-1157 nnns volume:23 year:2003 number:3-4 day:17 month:10 pages:200-206 https://dx.doi.org/10.1007/s00367-003-0147-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_612 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.48 ASE AR 23 2003 3-4 17 10 200-206 |
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10.1007/s00367-003-0147-9 doi (DE-627)SPR004570952 (SPR)s00367-003-0147-9-e DE-627 ger DE-627 rakwb eng 550 ASE 38.48 bkl García-García, A. verfasserin aut Monitoring the Spanish gas fields in the Ría de Vigo (1991–2001) 2003 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The Ría de Vigo is located on the NW coast of Spain, and includes gassy areas studied in several high-resolution seismic surveys between 1991 and 2001. The position of the acoustic blankings and gas seepages has been monitored vertically and spatially in the surveyed area. Also, a 253-cm-long vibrocore was recovered in a gas field in the inner part of the ría. The predominant facies of the core is dark mud with small bioclastic fragments and a very strong $ H_{2} $S smell. The repeated surveys of this ría show that these shallow gas fields have been active in the last decade and were active in the past (buried collapse structures). Available direct gas analyses show that methane is one of the components of the gas in the ría. Thus, bacterial degradation of organic matter in shallow sediments is considered the most likely source for the gas in the Ría de Vigo. Seismic Line (dpeaa)DE-He213 Collapse Structure (dpeaa)DE-He213 Seismic Unit (dpeaa)DE-He213 Seismic Stratigraphy (dpeaa)DE-He213 Acoustic Blankings (dpeaa)DE-He213 García-Gil, S. verfasserin aut Vilas, F. verfasserin aut Enthalten in Geo-marine letters Berlin : Springer, 1984 23(2003), 3-4 vom: 17. Okt., Seite 200-206 (DE-627)300183690 (DE-600)1481423-7 1432-1157 nnns volume:23 year:2003 number:3-4 day:17 month:10 pages:200-206 https://dx.doi.org/10.1007/s00367-003-0147-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_612 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.48 ASE AR 23 2003 3-4 17 10 200-206 |
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10.1007/s00367-003-0147-9 doi (DE-627)SPR004570952 (SPR)s00367-003-0147-9-e DE-627 ger DE-627 rakwb eng 550 ASE 38.48 bkl García-García, A. verfasserin aut Monitoring the Spanish gas fields in the Ría de Vigo (1991–2001) 2003 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The Ría de Vigo is located on the NW coast of Spain, and includes gassy areas studied in several high-resolution seismic surveys between 1991 and 2001. The position of the acoustic blankings and gas seepages has been monitored vertically and spatially in the surveyed area. Also, a 253-cm-long vibrocore was recovered in a gas field in the inner part of the ría. The predominant facies of the core is dark mud with small bioclastic fragments and a very strong $ H_{2} $S smell. The repeated surveys of this ría show that these shallow gas fields have been active in the last decade and were active in the past (buried collapse structures). Available direct gas analyses show that methane is one of the components of the gas in the ría. Thus, bacterial degradation of organic matter in shallow sediments is considered the most likely source for the gas in the Ría de Vigo. Seismic Line (dpeaa)DE-He213 Collapse Structure (dpeaa)DE-He213 Seismic Unit (dpeaa)DE-He213 Seismic Stratigraphy (dpeaa)DE-He213 Acoustic Blankings (dpeaa)DE-He213 García-Gil, S. verfasserin aut Vilas, F. verfasserin aut Enthalten in Geo-marine letters Berlin : Springer, 1984 23(2003), 3-4 vom: 17. Okt., Seite 200-206 (DE-627)300183690 (DE-600)1481423-7 1432-1157 nnns volume:23 year:2003 number:3-4 day:17 month:10 pages:200-206 https://dx.doi.org/10.1007/s00367-003-0147-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_612 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.48 ASE AR 23 2003 3-4 17 10 200-206 |
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Enthalten in Geo-marine letters 23(2003), 3-4 vom: 17. Okt., Seite 200-206 volume:23 year:2003 number:3-4 day:17 month:10 pages:200-206 |
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Seismic Line Collapse Structure Seismic Unit Seismic Stratigraphy Acoustic Blankings |
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García-García, A. @@aut@@ García-Gil, S. @@aut@@ Vilas, F. @@aut@@ |
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2003-10-17T00:00:00Z |
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García-García, A. |
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García-García, A. ddc 550 bkl 38.48 misc Seismic Line misc Collapse Structure misc Seismic Unit misc Seismic Stratigraphy misc Acoustic Blankings Monitoring the Spanish gas fields in the Ría de Vigo (1991–2001) |
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550 ASE 38.48 bkl Monitoring the Spanish gas fields in the Ría de Vigo (1991–2001) Seismic Line (dpeaa)DE-He213 Collapse Structure (dpeaa)DE-He213 Seismic Unit (dpeaa)DE-He213 Seismic Stratigraphy (dpeaa)DE-He213 Acoustic Blankings (dpeaa)DE-He213 |
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Monitoring the Spanish gas fields in the Ría de Vigo (1991–2001) |
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Monitoring the Spanish gas fields in the Ría de Vigo (1991–2001) |
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García-García, A. García-Gil, S. Vilas, F. |
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monitoring the spanish gas fields in the ría de vigo (1991–2001) |
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Monitoring the Spanish gas fields in the Ría de Vigo (1991–2001) |
| abstract |
Abstract The Ría de Vigo is located on the NW coast of Spain, and includes gassy areas studied in several high-resolution seismic surveys between 1991 and 2001. The position of the acoustic blankings and gas seepages has been monitored vertically and spatially in the surveyed area. Also, a 253-cm-long vibrocore was recovered in a gas field in the inner part of the ría. The predominant facies of the core is dark mud with small bioclastic fragments and a very strong $ H_{2} $S smell. The repeated surveys of this ría show that these shallow gas fields have been active in the last decade and were active in the past (buried collapse structures). Available direct gas analyses show that methane is one of the components of the gas in the ría. Thus, bacterial degradation of organic matter in shallow sediments is considered the most likely source for the gas in the Ría de Vigo. |
| abstractGer |
Abstract The Ría de Vigo is located on the NW coast of Spain, and includes gassy areas studied in several high-resolution seismic surveys between 1991 and 2001. The position of the acoustic blankings and gas seepages has been monitored vertically and spatially in the surveyed area. Also, a 253-cm-long vibrocore was recovered in a gas field in the inner part of the ría. The predominant facies of the core is dark mud with small bioclastic fragments and a very strong $ H_{2} $S smell. The repeated surveys of this ría show that these shallow gas fields have been active in the last decade and were active in the past (buried collapse structures). Available direct gas analyses show that methane is one of the components of the gas in the ría. Thus, bacterial degradation of organic matter in shallow sediments is considered the most likely source for the gas in the Ría de Vigo. |
| abstract_unstemmed |
Abstract The Ría de Vigo is located on the NW coast of Spain, and includes gassy areas studied in several high-resolution seismic surveys between 1991 and 2001. The position of the acoustic blankings and gas seepages has been monitored vertically and spatially in the surveyed area. Also, a 253-cm-long vibrocore was recovered in a gas field in the inner part of the ría. The predominant facies of the core is dark mud with small bioclastic fragments and a very strong $ H_{2} $S smell. The repeated surveys of this ría show that these shallow gas fields have been active in the last decade and were active in the past (buried collapse structures). Available direct gas analyses show that methane is one of the components of the gas in the ría. Thus, bacterial degradation of organic matter in shallow sediments is considered the most likely source for the gas in the Ría de Vigo. |
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| title_short |
Monitoring the Spanish gas fields in the Ría de Vigo (1991–2001) |
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https://dx.doi.org/10.1007/s00367-003-0147-9 |
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García-Gil, S. Vilas, F. |
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García-Gil, S. Vilas, F. |
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| doi_str |
10.1007/s00367-003-0147-9 |
| up_date |
2024-07-04T01:40:39.260Z |
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| score |
7.401639 |