Seismic modeling of two depositional systems

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 sy...

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Bibliographic Details
Main Authors: G. Seriani, M. Rebesco, A. Polonia, A. Manzella, C. De Cillia, G. Casula, G. Brancolini
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 1994-06-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/4183
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spelling doaj-ddc87c35e04742668a2ee1804d05725b2020-11-25T00:51:34ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X1994-06-0137510.4401/ag-4183Seismic modeling of two depositional systemsG. SerianiM. RebescoA. PoloniaA. ManzellaC. De CilliaG. CasulaG. BrancoliniTwo 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.http://www.annalsofgeophysics.eu/index.php/annals/article/view/4183seismic modelingdepositional systemstidal barsfluvial complexwave equation
collection DOAJ
language English
format Article
sources DOAJ
author G. Seriani
M. Rebesco
A. Polonia
A. Manzella
C. De Cillia
G. Casula
G. Brancolini
spellingShingle G. Seriani
M. Rebesco
A. Polonia
A. Manzella
C. De Cillia
G. Casula
G. Brancolini
Seismic modeling of two depositional systems
Annals of Geophysics
seismic modeling
depositional systems
tidal bars
fluvial complex
wave equation
author_facet G. Seriani
M. Rebesco
A. Polonia
A. Manzella
C. De Cillia
G. Casula
G. Brancolini
author_sort G. Seriani
title Seismic modeling of two depositional systems
title_short Seismic modeling of two depositional systems
title_full Seismic modeling of two depositional systems
title_fullStr Seismic modeling of two depositional systems
title_full_unstemmed Seismic modeling of two depositional systems
title_sort seismic modeling of two depositional systems
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
series Annals of Geophysics
issn 1593-5213
2037-416X
publishDate 1994-06-01
description 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.
topic seismic modeling
depositional systems
tidal bars
fluvial complex
wave equation
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/4183
work_keys_str_mv AT gseriani seismicmodelingoftwodepositionalsystems
AT mrebesco seismicmodelingoftwodepositionalsystems
AT apolonia seismicmodelingoftwodepositionalsystems
AT amanzella seismicmodelingoftwodepositionalsystems
AT cdecillia seismicmodelingoftwodepositionalsystems
AT gcasula seismicmodelingoftwodepositionalsystems
AT gbrancolini seismicmodelingoftwodepositionalsystems
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