Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/1855
DC Field | Value | Language |
---|---|---|
dc.contributor.authorall | Brancolini, G.; Osservatorio Geofisico Sperimentale, Trieste, Italy | en |
dc.contributor.authorall | Casula, G.; Osservatorio Geofisico Sperimentale, Trieste, Italy | en |
dc.contributor.authorall | De Cillia, C.; Osservatorio Geofisico Sperimentale, Trieste, Italy | en |
dc.contributor.authorall | Manzella, A.; C.N.R., Istituto Intemazionale Ricerche Geotermiche, Pisa, Italy | en |
dc.contributor.authorall | Polonia, A.; Osservatorio Geofisico Sperimentale, Trieste, Italy | en |
dc.contributor.authorall | Rebesco, M.; Osservatorio Geofisico Sperimentale, Trieste, Italy | en |
dc.contributor.authorall | Seriani, G.; Osservatorio Geofisico Sperimentale, Trieste, Italy | en |
dc.date.accessioned | 2006-12-06T11:16:43Z | en |
dc.date.available | 2006-12-06T11:16:43Z | en |
dc.date.issued | 1994-09 | en |
dc.identifier.uri | http://hdl.handle.net/2122/1855 | en |
dc.description.abstract | Two ideal lithologic sections representing a tidal bar system and a fluvial complex were drawn in order to run seismic modeling programs developed by OGS on behalf of the European Community. The simulations allowed an accurate analysis of the seismic expressions of the two sections. The tidal bar system is formed by a number of sandstone lenses interlayered with siltstone and mudstone deposits. These lenses meet together on an erosion surface, while they thin and vanish in the other direction. The fluvial complex is fonned by a limestone basement overlain by coarse alluvial plain sediments which in turn are transgressed by finer flood plain sediments, including sandstone lenses stacking towards the top in a meandering belt. These lithofacies associations represent potential multi-pool reservoirs in which the mudstone layers constitute the plugs. As a function of the granulometric and depositional features of each lithological unit, together with fluid content, wave velocities and densities were evaluated. A 2D modeling for elastic plane wave propagation in these hypothesized geologic sections was run on a Cray supercomputer. The numerical scheme is based on solving the full wave equation by pseudospectral methods. | en |
dc.format.extent | 5195786 bytes | en |
dc.format.mimetype | application/pdf | en |
dc.language.iso | English | en |
dc.relation.ispartofseries | 5/37 (1994) | en |
dc.subject | seismic modeling | en |
dc.subject | depositional systems | en |
dc.subject | tidal bars | en |
dc.subject | fluvial complex | en |
dc.subject | wave equation | en |
dc.title | Seismic modeling of two depositional systems | en |
dc.type | article | en |
dc.type.QualityControl | Peer-reviewed | en |
dc.subject.INGV | 04. Solid Earth::04.02. Exploration geophysics::04.02.06. Seismic methods | en |
dc.subject.INGV | 04. Solid Earth::04.04. Geology::04.04.10. Stratigraphy | en |
dc.description.journalType | JCR Journal | en |
dc.description.fulltext | open | en |
dc.contributor.author | Brancolini, G. | en |
dc.contributor.author | Casula, G. | en |
dc.contributor.author | De Cillia, C. | en |
dc.contributor.author | Manzella, A. | en |
dc.contributor.author | Polonia, A. | en |
dc.contributor.author | Rebesco, M. | en |
dc.contributor.author | Seriani, G. | en |
dc.contributor.department | Osservatorio Geofisico Sperimentale, Trieste, Italy | en |
dc.contributor.department | Osservatorio Geofisico Sperimentale, Trieste, Italy | en |
dc.contributor.department | Osservatorio Geofisico Sperimentale, Trieste, Italy | en |
dc.contributor.department | C.N.R., Istituto Intemazionale Ricerche Geotermiche, Pisa, Italy | en |
dc.contributor.department | Osservatorio Geofisico Sperimentale, Trieste, Italy | en |
dc.contributor.department | Osservatorio Geofisico Sperimentale, Trieste, Italy | en |
dc.contributor.department | Osservatorio Geofisico Sperimentale, Trieste, Italy | en |
item.openairetype | article | - |
item.cerifentitytype | Publications | - |
item.languageiso639-1 | en | - |
item.grantfulltext | open | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
crisitem.author.dept | Osservatorio Geofisico Sperimentale, Trieste, Italy | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia | - |
crisitem.author.dept | Osservatorio Geofisico Sperimentale, Trieste, Italy | - |
crisitem.author.dept | CNR, Istituto Internazionale per le Ricerche Geotermiche, Pisa, Italy | - |
crisitem.author.dept | CNR - ISMAR | - |
crisitem.author.dept | Istituto Nazionale di Oceanografia e di Geofisica Sperimentale | - |
crisitem.author.dept | Osservatorio Geofisico Sperimentale, Trieste, Italy | - |
crisitem.author.orcid | 0000-0001-7934-2019 | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
Appears in Collections: | Annals of Geophysics |
Files in This Item:
File | Description | Size | Format | |
---|---|---|---|---|
03 brancolini.pdf | 5.07 MB | Adobe PDF | View/Open |
Page view(s)
146
checked on Apr 24, 2024
Download(s) 20
483
checked on Apr 24, 2024