Gas Type of the Paperhydrate Estimate in an Area of Deformation and High Heat Flow at the Chile Triple Junction

Large amounts of gas hydrate are present in marine sediments offshore Taitao Peninsula, near the Chile Triple Junction. Here, marine sediments on the forearc contain carbon that is converted to methane in a regime of very high heat flow and intense rock deformation above the downgoing oceanic spread...

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Published in:Geosciences
Main Authors: Lucía Villar-Muñoz, Iván Vargas-Cordero, Joaquim P. Bento, Umberta Tinivella, Francisco Fernandoy, Michela Giustiniani, Jan H. Behrmann, Sergio Calderón-Díaz
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2019
Subjects:
BSR
Online Access:https://doi.org/10.3390/geosciences9010028
https://doaj.org/article/1891d0498d6f488a81d3b5ad437c457b
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spelling ftdoajarticles:oai:doaj.org/article:1891d0498d6f488a81d3b5ad437c457b 2023-05-15T13:45:53+02:00 Gas Type of the Paperhydrate Estimate in an Area of Deformation and High Heat Flow at the Chile Triple Junction Lucía Villar-Muñoz Iván Vargas-Cordero Joaquim P. Bento Umberta Tinivella Francisco Fernandoy Michela Giustiniani Jan H. Behrmann Sergio Calderón-Díaz 2019-01-01T00:00:00Z https://doi.org/10.3390/geosciences9010028 https://doaj.org/article/1891d0498d6f488a81d3b5ad437c457b EN eng MDPI AG http://www.mdpi.com/2076-3263/9/1/28 https://doaj.org/toc/2076-3263 2076-3263 doi:10.3390/geosciences9010028 https://doaj.org/article/1891d0498d6f488a81d3b5ad437c457b Geosciences, Vol 9, Iss 1, p 28 (2019) BSR gas hydrate methane seepage active margin Chile Triple Junction Geology QE1-996.5 article 2019 ftdoajarticles https://doi.org/10.3390/geosciences9010028 2022-12-30T20:46:45Z Large amounts of gas hydrate are present in marine sediments offshore Taitao Peninsula, near the Chile Triple Junction. Here, marine sediments on the forearc contain carbon that is converted to methane in a regime of very high heat flow and intense rock deformation above the downgoing oceanic spreading ridge separating the Nazca and Antarctic plates. This regime enables vigorous fluid migration. Here, we present an analysis of the spatial distribution, concentration, estimate of gas-phases (gas hydrate and free gas) and geothermal gradients in the accretionary prism, and forearc sediments offshore Taitao (45.5°–47° S). Velocity analysis of Seismic Profile RC2901-751 indicates gas hydrate concentration values <10% of the total rock volume and extremely high geothermal gradients (<190 °C·km−1). Gas hydrates are located in shallow sediments (90–280 m below the seafloor). The large amount of hydrate and free gas estimated (7.21 × 1011 m3 and 4.1 × 1010 m3; respectively), the high seismicity, the mechanically unstable nature of the sediments, and the anomalous conditions of the geothermal gradient set the stage for potentially massive releases of methane to the ocean, mainly through hydrate dissociation and/or migration directly to the seabed through faults. We conclude that the Chile Triple Junction is an important methane seepage area and should be the focus of novel geological, oceanographic, and ecological research. Article in Journal/Newspaper Antarc* Antarctic Directory of Open Access Journals: DOAJ Articles Antarctic Geosciences 9 1 28
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic BSR
gas hydrate
methane
seepage
active margin
Chile Triple Junction
Geology
QE1-996.5
spellingShingle BSR
gas hydrate
methane
seepage
active margin
Chile Triple Junction
Geology
QE1-996.5
Lucía Villar-Muñoz
Iván Vargas-Cordero
Joaquim P. Bento
Umberta Tinivella
Francisco Fernandoy
Michela Giustiniani
Jan H. Behrmann
Sergio Calderón-Díaz
Gas Type of the Paperhydrate Estimate in an Area of Deformation and High Heat Flow at the Chile Triple Junction
topic_facet BSR
gas hydrate
methane
seepage
active margin
Chile Triple Junction
Geology
QE1-996.5
description Large amounts of gas hydrate are present in marine sediments offshore Taitao Peninsula, near the Chile Triple Junction. Here, marine sediments on the forearc contain carbon that is converted to methane in a regime of very high heat flow and intense rock deformation above the downgoing oceanic spreading ridge separating the Nazca and Antarctic plates. This regime enables vigorous fluid migration. Here, we present an analysis of the spatial distribution, concentration, estimate of gas-phases (gas hydrate and free gas) and geothermal gradients in the accretionary prism, and forearc sediments offshore Taitao (45.5°–47° S). Velocity analysis of Seismic Profile RC2901-751 indicates gas hydrate concentration values <10% of the total rock volume and extremely high geothermal gradients (<190 °C·km−1). Gas hydrates are located in shallow sediments (90–280 m below the seafloor). The large amount of hydrate and free gas estimated (7.21 × 1011 m3 and 4.1 × 1010 m3; respectively), the high seismicity, the mechanically unstable nature of the sediments, and the anomalous conditions of the geothermal gradient set the stage for potentially massive releases of methane to the ocean, mainly through hydrate dissociation and/or migration directly to the seabed through faults. We conclude that the Chile Triple Junction is an important methane seepage area and should be the focus of novel geological, oceanographic, and ecological research.
format Article in Journal/Newspaper
author Lucía Villar-Muñoz
Iván Vargas-Cordero
Joaquim P. Bento
Umberta Tinivella
Francisco Fernandoy
Michela Giustiniani
Jan H. Behrmann
Sergio Calderón-Díaz
author_facet Lucía Villar-Muñoz
Iván Vargas-Cordero
Joaquim P. Bento
Umberta Tinivella
Francisco Fernandoy
Michela Giustiniani
Jan H. Behrmann
Sergio Calderón-Díaz
author_sort Lucía Villar-Muñoz
title Gas Type of the Paperhydrate Estimate in an Area of Deformation and High Heat Flow at the Chile Triple Junction
title_short Gas Type of the Paperhydrate Estimate in an Area of Deformation and High Heat Flow at the Chile Triple Junction
title_full Gas Type of the Paperhydrate Estimate in an Area of Deformation and High Heat Flow at the Chile Triple Junction
title_fullStr Gas Type of the Paperhydrate Estimate in an Area of Deformation and High Heat Flow at the Chile Triple Junction
title_full_unstemmed Gas Type of the Paperhydrate Estimate in an Area of Deformation and High Heat Flow at the Chile Triple Junction
title_sort gas type of the paperhydrate estimate in an area of deformation and high heat flow at the chile triple junction
publisher MDPI AG
publishDate 2019
url https://doi.org/10.3390/geosciences9010028
https://doaj.org/article/1891d0498d6f488a81d3b5ad437c457b
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_source Geosciences, Vol 9, Iss 1, p 28 (2019)
op_relation http://www.mdpi.com/2076-3263/9/1/28
https://doaj.org/toc/2076-3263
2076-3263
doi:10.3390/geosciences9010028
https://doaj.org/article/1891d0498d6f488a81d3b5ad437c457b
op_doi https://doi.org/10.3390/geosciences9010028
container_title Geosciences
container_volume 9
container_issue 1
container_start_page 28
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