RRS "Charles Darwin" Cruise 178, 14 Mar - 11 Apr 2006. 3D seismic acquisition over mud volcanoes in the Gulf of Cadiz and submarine landslides in the Eivissa Channel, western Mediterranean Sea [PDF]
, 2006 The major aims of Charles Darwin Cruise 178 were to obtain (i) 3D seismic imagery, video transects and swath bathymetry maps of mud volcanoes in the southern Gulf of Cadiz, (ii) video transects across suspected cold water coral reefs in the Alboran Sea ...
Berndt, C., Masson, D.G.
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MUD VOLCANO SHUGO, DEPTH STRUCTURE AND MECHANISMS OF ACTIVITY [PDF]
Геологія і корисні копалини Світового океану, 2020 Most mud volcanoes are located along large tectonic zones within the Alpine and Central Asian folded regions, the Pacific mobile belt and rift regions of the Atlantic and Indian oceans.
L.E. Sobisevich, A.L. Sobisevich
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RRS James Cook Cruise 10, 13 May-07 Jul 2007. Hotspot ecosystems in the NE Atlantic, UK contribution to the HERMES Project. Mud volcanoes in the Gulf of Cadiz; submarine canyons west of Portugal; submarine canyons in the northern Bay of Biscay [PDF]
, 2007 The major objective of RRS James Cook Cruise 10 was to increase our understanding of how seafloor environmental variables affect the biodiversity, structure, function and dynamics of faunal communities in two specific ‘biological hotspot’ environments ...
Masson, D.G., Weaver, P.P.E.
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Journal of Marine Science and Engineering, 2022 Mud volcanoes and other fluid seepage pathways usually transport sufficient gas for the formation of gas reservoirs and are beneficial to the accumulation of gas hydrate.
Zhifeng Wan +6 more
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Gravity Data Allow to Image the Shallow‐Medium Subsurface Below Mud Volcanoes
Geophysical Research Letters, 2023 The debate about the conceptual model of mud volcanoes functioning is still alive in the literature. A large part of the literature focuses on the characterization of the deep reservoir where expelled fluids are expected to originate.
Massimo Nespoli +5 more
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, 2010 Mud volcanoes are frequently encountered geo-structures at active and passive continental margins. In contrast to magmatic volcanoes, mud volcanoes are marine or terrestrial, topographic elevation built from vertically rising fluidized mud or mud breccia.
Boetius, A. +3 more
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Seabed gas emissions and submarine landslides off SW Taiwan
Terrestrial, Atmospheric and Oceanic Sciences, 2018 Methane emissions out of the seabed could seriously affect Earthâs climate and are usually associated with the dissociation of gas hydrates stored in marine sediments on the continental margins.
Shu-Kun Hsu +9 more
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Scientia Marina, 2006 This research focuses on the mud volcanoes Amsterdam, Kazan and Kula located in the Anaximander Mountains (SW Turkey continental margin), which are characterized by the presence of sediments containing gas and gas hydrate.
David Casas +4 more
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Mud volcano dynamics in Azerbaijan: the overlooked role of creeping mud flows in landscape evolution [PDF]
Earth Surface DynamicsAzerbaijan hosts the world's highest concentration of mud volcanoes (MVs) on Earth, including some of the largest edifices that produce kilometre-scale mud breccia flows.
C. Fenske +4 more
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Frontiers in Earth Science, 2023 Mud volcanoes are topographic features through which over-pressurized sediments are intruded upward and erupted, transporting fluids and sediments from the deep subsurface to the surface/seafloor. To understand material and biogeochemical cycling through
Akira Ijiri +18 more
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