Volcaniclastic Sedimentation in Deep-Water Basins
A special issue of Minerals (ISSN 2075-163X).
Deadline for manuscript submissions: closed (15 February 2025) | Viewed by 1483
Special Issue Editors
Interests: field geology; stratigraphy sedimentary; geological processes; sedimentology; stratigraphy; regional geology; sedimentary basins; geology-volcanology; petrographic thin section; surficial geology; paleomagnetism; grain size analysis; earth sciences; sediments; geodynamics; cartography; geology; sediment transport; carbonates; climate change; tectonics; petrography; geochronology; structural geology; plate tectonics; sequence stratigraphy; basin analysis; granulometry; crustal deformation
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Special Issue Information
Dear Colleagues,
Origin and way of transport of volcaniclastic particles through the environments are more than those concerning sedimentary particles, considering that volcaniclastic particles might be produced and transported by primary volcanic mechanisms (sensu White and Houghton, 2006) during explosive eruptions. In most cases, when the transport agent is volcanic (e.g., pyroclastic density currents), particles would travel wrapped into a hot gas medium that, once in contact with water, would react giving rise to a multiple spectrum of depositional features that could potentially result in the obliteration of the primary volcaniclastic origin of particles. Consequent to an eruptive event, large dispersal deposits could potentially enter the sediments’ routing system, giving rise to a series of volcaniclastic and non-volcaniclastic beds during the long-term reapproach of a sedimentary system to pre-eruptive conditions. In other cases, volcaniclastic beds are the simple results of passive erosion, transportation and accumulation of particles from volcanic terranes to depocenters. Deep-water basins, the most distal depocenters of a sedimentary system, can host all the aforementioned bed types organized in a wide range of depositional architectures. Eventually, such architectures also potentially interact with non-volcanic sedimentary systems.
This Special Issue aims to bring together works on deep-water volcaniclastic sedimentation in both modern and ancient sedimentary basins, focusing on (but not limited to) impact of volcanic eruptions on sea-floor sedimentary architectures, reconstruction of eruptive series from deep-water sediments, reconstruction of volcaniclastic architectures from seismic data, provenance analyses on tephra fallout deposits recovered in deep-marine realms, impact of volcaniclastic sedimentation on other sedimentary processes (e.g., carbonate accumulation). Papers on the study of volcaniclastic sequences as potential reservoirs for geoenergy and carbon capture and storage will be also welcome.
Dr. Andrea Di Capua
Dr. Federica Barilaro
Guest Editors
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Keywords
- deep-water sedimentation
- volcaniclastic
- volcanogenic
- volcanoes
- volcanism
- pyroclastic density currents
- numerical models
- geochemistry
- sands/sandstones petrography
- provenance
- paleogeography
- geodynamics
- carbon capture and storage
- geoenergies
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