Joint gravity and isostatic analysis for basement studies - A novel tool
We have created a working tool – named Lithoflex- that is useful for the interpretation of gravity data in oceanic and continental areas. The tool combines gravity forward and inverse calculation with an investigation of the isostatic state. Density models derived from the gravity field are ambiguou...
Main Authors: | , , , , |
---|---|
Other Authors: | , , , , , |
Format: | Conference Object |
Language: | English |
Published: |
EAGE-SEG
2007
|
Subjects: | |
Online Access: | http://hdl.handle.net/11368/2304910 http://www2.ogs.trieste.it/egm2007/egm2007/Sessione%20B/Poster%20papers/B_PP_05.pdf |
_version_ | 1821864662198648832 |
---|---|
author | BRAITENBERG, CARLA Wienecke S. Ebbing J. Born W. Redfield T. |
author2 | Fedi M. Braitenberg, Carla Wienecke, S. Ebbing, J. Born, W. Redfield, T. |
author_facet | BRAITENBERG, CARLA Wienecke S. Ebbing J. Born W. Redfield T. |
author_sort | BRAITENBERG, CARLA |
collection | Università degli studi di Trieste: ArTS (Archivio della ricerca di Trieste) |
description | We have created a working tool – named Lithoflex- that is useful for the interpretation of gravity data in oceanic and continental areas. The tool combines gravity forward and inverse calculation with an investigation of the isostatic state. Density models derived from the gravity field are ambiguous if external geological or geophysical constraints are scarce or unavailable. However, because isostasy is a physical condition , some of the native ambiguity can be reduced by checking the compatibility of the density model with the isostatic state. We demonstrate the usefulness of our tool in the analysis of the basement in the Barents Sea and in the South China Sea, where the basement characterization is accomplished by the high-resolution analysis of the equivalent elastic thickness. Other situations for which our tool could be useful include the recovery of depth-to-basement by the inversion of the gravity field, the identification of distinctive terrains by their variation in elastic thickness, or, given a comprehensive gravity field, the interpolation of crustal thickness between seismic lines. |
format | Conference Object |
genre | Barents Sea |
genre_facet | Barents Sea |
geographic | Barents Sea |
geographic_facet | Barents Sea |
id | ftunitriestiris:oai:arts.units.it:11368/2304910 |
institution | Open Polar |
language | English |
op_collection_id | ftunitriestiris |
op_relation | info:eu-repo/semantics/altIdentifier/isbn/9780000000002 ispartofbook:Innovation in EM, Grav and Mag Methods: a new Perspective for Exploration EGM 2007 International Workshop, Innovation in EM, Grav and Mag Methods: a new Perspective for Exploration, firstpage:- lastpage:- http://hdl.handle.net/11368/2304910 http://www2.ogs.trieste.it/egm2007/egm2007/Sessione%20B/Poster%20papers/B_PP_05.pdf |
publishDate | 2007 |
publisher | EAGE-SEG |
record_format | openpolar |
spelling | ftunitriestiris:oai:arts.units.it:11368/2304910 2025-01-16T21:11:54+00:00 Joint gravity and isostatic analysis for basement studies - A novel tool BRAITENBERG, CARLA Wienecke S. Ebbing J. Born W. Redfield T. Fedi M. Braitenberg, Carla Wienecke, S. Ebbing, J. Born, W. Redfield, T. 2007 ELETTRONICO http://hdl.handle.net/11368/2304910 http://www2.ogs.trieste.it/egm2007/egm2007/Sessione%20B/Poster%20papers/B_PP_05.pdf eng eng EAGE-SEG place:Trieste info:eu-repo/semantics/altIdentifier/isbn/9780000000002 ispartofbook:Innovation in EM, Grav and Mag Methods: a new Perspective for Exploration EGM 2007 International Workshop, Innovation in EM, Grav and Mag Methods: a new Perspective for Exploration, firstpage:- lastpage:- http://hdl.handle.net/11368/2304910 http://www2.ogs.trieste.it/egm2007/egm2007/Sessione%20B/Poster%20papers/B_PP_05.pdf Lithoflex basement studie gravity isostasy info:eu-repo/semantics/conferenceObject 2007 ftunitriestiris 2023-04-09T06:06:54Z We have created a working tool – named Lithoflex- that is useful for the interpretation of gravity data in oceanic and continental areas. The tool combines gravity forward and inverse calculation with an investigation of the isostatic state. Density models derived from the gravity field are ambiguous if external geological or geophysical constraints are scarce or unavailable. However, because isostasy is a physical condition , some of the native ambiguity can be reduced by checking the compatibility of the density model with the isostatic state. We demonstrate the usefulness of our tool in the analysis of the basement in the Barents Sea and in the South China Sea, where the basement characterization is accomplished by the high-resolution analysis of the equivalent elastic thickness. Other situations for which our tool could be useful include the recovery of depth-to-basement by the inversion of the gravity field, the identification of distinctive terrains by their variation in elastic thickness, or, given a comprehensive gravity field, the interpolation of crustal thickness between seismic lines. Conference Object Barents Sea Università degli studi di Trieste: ArTS (Archivio della ricerca di Trieste) Barents Sea |
spellingShingle | Lithoflex basement studie gravity isostasy BRAITENBERG, CARLA Wienecke S. Ebbing J. Born W. Redfield T. Joint gravity and isostatic analysis for basement studies - A novel tool |
title | Joint gravity and isostatic analysis for basement studies - A novel tool |
title_full | Joint gravity and isostatic analysis for basement studies - A novel tool |
title_fullStr | Joint gravity and isostatic analysis for basement studies - A novel tool |
title_full_unstemmed | Joint gravity and isostatic analysis for basement studies - A novel tool |
title_short | Joint gravity and isostatic analysis for basement studies - A novel tool |
title_sort | joint gravity and isostatic analysis for basement studies - a novel tool |
topic | Lithoflex basement studie gravity isostasy |
topic_facet | Lithoflex basement studie gravity isostasy |
url | http://hdl.handle.net/11368/2304910 http://www2.ogs.trieste.it/egm2007/egm2007/Sessione%20B/Poster%20papers/B_PP_05.pdf |