Summary Deception Island is a volcanic island with a flooded caldera that has a complex geological setting in Brans-field Strait, Antarctica. We use P-wave arrivals recorded on land and seafloor seismometers from airgun shots within the caldera and around the island to invert for the P-wave velocity...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.505.8144 2023-05-15T13:51:04+02:00 The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.505.8144 http://pubs.usgs.gov/of/2007/1047/ea/of2007-1047ea078.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.505.8144 http://pubs.usgs.gov/of/2007/1047/ea/of2007-1047ea078.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://pubs.usgs.gov/of/2007/1047/ea/of2007-1047ea078.pdf text ftciteseerx 2016-01-08T09:22:10Z Summary Deception Island is a volcanic island with a flooded caldera that has a complex geological setting in Brans-field Strait, Antarctica. We use P-wave arrivals recorded on land and seafloor seismometers from airgun shots within the caldera and around the island to invert for the P-wave velocity structure along two orthogonal profiles. The results reveal a low-velocity anomaly beneath the caldera with a maximum anomaly of ~-1 km/s extending from the seafloor to ~5 km depth. Refracted arrivals suggest a>1-km-thick layer of sediments and unconsolidated lavas infilling the calde-ra. Synthetic inversions show that this layer accounts for only a small portion of the velocity anomaly, implying that there is a significant region of low velocities at greater depths. Further synthetic inversions and melt fraction calcula-tions suggest that the caldera is underlain by an extensive region of magma that extends downwards from <2 km be-neath the seafloor. Text Antarc* Antarctica Deception Island Unknown Deception Island ENVELOPE(-60.633,-60.633,-62.950,-62.950) |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
description |
Summary Deception Island is a volcanic island with a flooded caldera that has a complex geological setting in Brans-field Strait, Antarctica. We use P-wave arrivals recorded on land and seafloor seismometers from airgun shots within the caldera and around the island to invert for the P-wave velocity structure along two orthogonal profiles. The results reveal a low-velocity anomaly beneath the caldera with a maximum anomaly of ~-1 km/s extending from the seafloor to ~5 km depth. Refracted arrivals suggest a>1-km-thick layer of sediments and unconsolidated lavas infilling the calde-ra. Synthetic inversions show that this layer accounts for only a small portion of the velocity anomaly, implying that there is a significant region of low velocities at greater depths. Further synthetic inversions and melt fraction calcula-tions suggest that the caldera is underlain by an extensive region of magma that extends downwards from <2 km be-neath the seafloor. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.505.8144 http://pubs.usgs.gov/of/2007/1047/ea/of2007-1047ea078.pdf |
long_lat |
ENVELOPE(-60.633,-60.633,-62.950,-62.950) |
geographic |
Deception Island |
geographic_facet |
Deception Island |
genre |
Antarc* Antarctica Deception Island |
genre_facet |
Antarc* Antarctica Deception Island |
op_source |
http://pubs.usgs.gov/of/2007/1047/ea/of2007-1047ea078.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.505.8144 http://pubs.usgs.gov/of/2007/1047/ea/of2007-1047ea078.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766254662364692480 |