Three‐Dimensional Seismic Imaging of Ancient Submarine Lava Flows: An Example From the Southern Australian Margin
Submarine lava flows are the most common surficial igneous rock on the Earth. However, they are inherently more difficult to study than their subaerial counterparts due to their inaccessibility. In this study, we use newly acquired 3‐D (three‐dimensional) seismic reflection data to document the dist...
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Published in: | Geochemistry, geophysics, geosystems : G3 geophysics, geosystems : G3, 2017-11, Vol.18 (11), p.3840-3853 |
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Main Authors: | , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Request full text |
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Summary: | Submarine lava flows are the most common surficial igneous rock on the Earth. However, they are inherently more difficult to study than their subaerial counterparts due to their inaccessibility. In this study, we use newly acquired 3‐D (three‐dimensional) seismic reflection data to document the distribution and morphology of 26 ancient, buried lava flows within the middle Eocene‐aged Bight Basin Igneous Complex, offshore southern Australia. Many of these lava flows are associated with volcanoes that vary from 60 to 625 m in height and 0.3 to 10 km in diameter. Well data and seismic‐stratigraphic relationships suggest that the lava flows and volcanoes were emplaced offshore in water depths of |
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ISSN: | 1525-2027 1525-2027 |
DOI: | 10.1002/2017GC007178 |