Articles | Volume 10, issue 4
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.
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.
Extrusion dynamics of deepwater volcanoes revealed by 3-D seismic data
Key Laboratory of Tectonics and Petroleum Resources, China University
of Geosciences (Wuhan), Ministry of Education, Wuhan 430074, China
Laboratory for Marine Mineral Resources, Qingdao National Laboratory
for Marine Science and Technology, Qingdao 266061, China
College of Marine Science and Technology, China University of
Geosciences (Wuhan), Wuhan, Hubei 430074, PR China
Christopher A.-L. Jackson
Basins Research Group (BRG), Department of Earth Science
&Engineering, Imperial College, London, SW7 2BP, UK
Craig Magee
Basins Research Group (BRG), Department of Earth Science
&Engineering, Imperial College, London, SW7 2BP, UK
School of Earth and Environment, University of Leeds, Leeds, LS2 9JT, UK
Samuel J. Mitchell
School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, UK
Xinong Xie
Key Laboratory of Tectonics and Petroleum Resources, China University
of Geosciences (Wuhan), Ministry of Education, Wuhan 430074, China
College of Marine Science and Technology, China University of
Geosciences (Wuhan), Wuhan, Hubei 430074, PR China
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- The High Arctic Large Igneous Province: first seismic-stratigraphic evidence for multiple Mesozoic volcanic pulses on the Lomonosov Ridge, central Arctic Ocean Y. Kristoffersen et al. 10.1144/jgs2022-153
- 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
- Understanding the petrophysical properties, seismic responses and impacts of the basalt-sediment transition in prospective sedimentary basins N. Famelli et al. 10.1016/j.jsames.2024.105113
- How do deep-water volcanoes grow? Q. Sun et al. 10.1016/j.epsl.2020.116320
- Postrift buried volcanoes and igneous plumbing systems along a continental ribbon: Insights from the Xisha massif, northwestern margin of the South China Sea L. Wang et al. 10.1190/INT-2023-0039.1
- 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
- In situ carbon storage potential in a buried volcano R. Pereira & D. Gamboa 10.1130/G50965.1
- 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
- Seismic investigations around an aseismic Comorin ridge, Indian Ocean D. Pandey et al. 10.1144/jgs2021-113
- 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
- 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
- Submarine volcanism in the southern margin of the South China Sea C. Zhang et al. 10.1007/s00343-022-2088-z
- Seismic Reflection Data Reveal the 3D Subsurface Structure of Pit Craters C. Magee et al. 10.1029/2021JE007155
- Post-rift magma plumbing system in the northern Great South Basin, New Zealand L. Cao et al. 10.1016/j.tecto.2023.230030
- 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
- 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
- Seismic acquisition parameters to improve imaging beneath mafic igneous units: case study from Australia’s Northwest Shelf C. Yule et al. 10.1080/08123985.2022.2072724
- 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
- 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
- Towards more consistent volcano morphometry datasets: Assessing boundary delineation and DEM impact on geometric and drainage parameters R. van Wees et al. 10.1016/j.geomorph.2024.109381
- Early Miocene magmatism in the Baiyun Sag (South China Sea): A view to the origin of intense post-rift magmatism Q. Sun et al. 10.1016/j.gr.2022.05.013
- Post-rift magmatism on the northern South China Sea margin Q. Sun et al. 10.1130/B35471.1
Latest update: 24 Dec 2024
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...