Articles | Volume 10, issue 4
Solid Earth, 10, 1269–1282, 2019
https://doi.org/10.5194/se-10-1269-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Solid Earth, 10, 1269–1282, 2019
https://doi.org/10.5194/se-10-1269-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
02 Aug 2019
Research article
| 02 Aug 2019
Extrusion dynamics of deepwater volcanoes revealed by 3-D seismic data
Qiliang Sun et al.
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Cited
15 citations as recorded by crossref.
- Structural controls on the location, geometry and longevity of an intraplate volcanic system: the Tuatara Volcanic Field, Great South Basin, New Zealand T. Phillips & C. Magee 10.1144/jgs2020-050
- Linking oceanographic processes to contourite features: Numerical modelling of currents influencing a contourite depositional system on the northern South China Sea margin H. Chen et al. 10.1016/j.margeo.2021.106714
- How do deep-water volcanoes grow? Q. Sun et al. 10.1016/j.epsl.2020.116320
- Massive seafloor mounds depict potential for seafloor mineral deposits in the Great South Basin (GSB) offshore New Zealand O. Olakunle et al. 10.1038/s41598-021-88620-x
- Extensional tectonics and post-rift magmatism in the southern South China Sea: New constraints from multi-channel seismic data Y. Zhang et al. 10.1016/j.marpetgeo.2020.104396
- Nature, timing and magnitude of buried Late Cretaceous magmatism on the central West Iberian Margin R. Pereira et al. 10.1111/bre.12640
- Characteristics and implications of Albian volcanism in a magma-rich rift basin: Seismic volcano stratigraphic and geomorphological evidence from the Upper Suhongtu Member in the Chagan Sag, China-Mongolia border region M. Tan et al. 10.1016/j.marpetgeo.2021.105164
- Interplay of tectonics and magmatism during post‐rift inversion on the central West Iberian Margin (Estremadura Spur) R. Pereira et al. 10.1111/bre.12524
- A case study of mapping igneous sill distribution in coal measures using borehole and 3D seismic data F. Zhou et al. 10.1016/j.coal.2020.103531
- Volcanogenic mass flow deposits and seafloor diapirism following the largest insular Quaternary eruption of the eastern Mediterranean at Nisyros island, Aegean volcanic arc V. Anagnostopoulos & G. Anastasakis 10.1016/j.margeo.2020.106185
- Discovery of large-scale buried volcanoes within the Cenozoic succession of the Prawn Platform, offshore Otway Basin, southeastern Australia Y. Niyazi et al. 10.1016/j.marpetgeo.2020.104747
- Sediment deformation triggered by underlying magma intrusion C. Wang et al. 10.1016/j.jseaes.2021.105045
- Growth and geomorphic evolution of the Ustica volcanic complex at the Africa-Europe plate margin (Tyrrhenian Sea) A. Sulli et al. 10.1016/j.geomorph.2020.107526
- Seismic interpretation of the architecture, evolution and structural characteristics of paleo-diatremes and volcanoes in the Vigrid syncline, Norwegian North Sea K. Omosanya 10.1007/s11001-021-09446-w
- Post-rift magmatism on the northern South China Sea margin Q. Sun et al. 10.1130/B35471.1
15 citations as recorded by crossref.
- Structural controls on the location, geometry and longevity of an intraplate volcanic system: the Tuatara Volcanic Field, Great South Basin, New Zealand T. Phillips & C. Magee 10.1144/jgs2020-050
- Linking oceanographic processes to contourite features: Numerical modelling of currents influencing a contourite depositional system on the northern South China Sea margin H. Chen et al. 10.1016/j.margeo.2021.106714
- How do deep-water volcanoes grow? Q. Sun et al. 10.1016/j.epsl.2020.116320
- Massive seafloor mounds depict potential for seafloor mineral deposits in the Great South Basin (GSB) offshore New Zealand O. Olakunle et al. 10.1038/s41598-021-88620-x
- Extensional tectonics and post-rift magmatism in the southern South China Sea: New constraints from multi-channel seismic data Y. Zhang et al. 10.1016/j.marpetgeo.2020.104396
- Nature, timing and magnitude of buried Late Cretaceous magmatism on the central West Iberian Margin R. Pereira et al. 10.1111/bre.12640
- Characteristics and implications of Albian volcanism in a magma-rich rift basin: Seismic volcano stratigraphic and geomorphological evidence from the Upper Suhongtu Member in the Chagan Sag, China-Mongolia border region M. Tan et al. 10.1016/j.marpetgeo.2021.105164
- Interplay of tectonics and magmatism during post‐rift inversion on the central West Iberian Margin (Estremadura Spur) R. Pereira et al. 10.1111/bre.12524
- A case study of mapping igneous sill distribution in coal measures using borehole and 3D seismic data F. Zhou et al. 10.1016/j.coal.2020.103531
- Volcanogenic mass flow deposits and seafloor diapirism following the largest insular Quaternary eruption of the eastern Mediterranean at Nisyros island, Aegean volcanic arc V. Anagnostopoulos & G. Anastasakis 10.1016/j.margeo.2020.106185
- Discovery of large-scale buried volcanoes within the Cenozoic succession of the Prawn Platform, offshore Otway Basin, southeastern Australia Y. Niyazi et al. 10.1016/j.marpetgeo.2020.104747
- Sediment deformation triggered by underlying magma intrusion C. Wang et al. 10.1016/j.jseaes.2021.105045
- Growth and geomorphic evolution of the Ustica volcanic complex at the Africa-Europe plate margin (Tyrrhenian Sea) A. Sulli et al. 10.1016/j.geomorph.2020.107526
- Seismic interpretation of the architecture, evolution and structural characteristics of paleo-diatremes and volcanoes in the Vigrid syncline, Norwegian North Sea K. Omosanya 10.1007/s11001-021-09446-w
- Post-rift magmatism on the northern South China Sea margin Q. Sun et al. 10.1130/B35471.1
Latest update: 20 Sep 2022
Short summary
3-D seismic reflection data reveal that deepwater volcanoes have rugged basal contacts, which truncate underlying strata, and erupted lava flows that feed lobate lava fans. The lava flows (> 9 km long) account for 50–97 % of the total erupted volume. This indicates that deepwater volcanic edifices may thus form a minor component (~ 3–50 %) of the extrusive system and that accurate estimates of erupted volume require knowledge of the basal surface of genetically related lava flows.
3-D seismic reflection data reveal that deepwater volcanoes have rugged basal contacts, which...
