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1. Identity statement
Reference TypeJournal Article
Sitemtc-m16b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier6qtX3pFwXQZGivnK2Y/SkSgK
Repositorysid.inpe.br/mtc-m17@80/2007/12.03.13.03   (restricted access)
Last Update2018:04.13.17.35.02 (UTC) marciana
Metadata Repositorysid.inpe.br/mtc-m17@80/2007/12.03.13.03.05
Metadata Last Update2018:06.05.03.35.51 (UTC) administrator
Secondary KeyINPE--PRE/
ISSN0016-8033
Labelself-archiving-INPE-MCTIC-GOV-BR
Citation KeySilvaOlivBarbCamp:2007:GrInUs
TitleGravity inversion using entropic regularization
Year2007
Access Date2024, May 08
Secondary TypePRE PI
Number of Files1
Size819 KiB
2. Context
Author1 Silva, João B. C.
2 Oliveria, Francisco S.
3 Barbosa, Valérica C. F.
4 Campos Velho, Haroldo Fraga de
Group1
2
3
4 LAC-INPE-MCT-BR
Affiliation1 Universidade Federal do Pará (UFPA)
2 Universidade Federal do Pará (UFPA)
3 LNCC
4 Instituto Nacional de Pesquisas Espaciais (INPE)
JournalGeophysics
Volume74
Pages151-160
History (UTC)2007-12-19 23:09:47 :: simone -> administrator ::
2012-11-24 01:32:37 :: administrator -> simone :: 2007
2013-02-20 15:20:09 :: simone -> administrator :: 2007
2013-09-27 16:56:38 :: administrator -> marciana :: 2007
2018-04-13 17:35:02 :: marciana -> administrator :: 2007
2018-06-05 03:35:51 :: administrator -> marciana :: 2007
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
AbstractWe present a new gravity inversion method, which produces an apparent density contrast mapping on the horizontal plane by combining the minimization of the first-order entropy with the maximization of the zeroth-order entropy of the estimated density contrasts. The maximization of the zeroth-order entropy is similar to the global smoothness constraint whereas the minimization of the first-order entropy favors solutions presenting sharp borders, so a judicious combination of both constrains may lead to solutions characterized by regions where the estimated density contrasts are virtually constant (in the case of homogeneous bodies), separated by sharp discontinuities. The method is applied to synthetic data simulating the intrusive bodies in sediments. By comparing our results with those obtained with the smoothness inversion we show that both methods produce good and equivalent locations of the source positions, but the entropic regularization delineates the contour of the bodies with greater resolution, even in the case of 100 m wide bodies separated by a distance as small as 50 m. Both, the proposed and the global smoothness inversions, have been applied to real data produced by the Lands' End batholithic intrusion from England. The entropic regularization inversion delineates a batholith with horizontal and nearly flat top being consistent with the known geological information.
AreaCOMP
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > LABAC > Gravity inversion using...
doc Directory Contentaccess
source Directory Contentthere are no files
agreement Directory Contentthere are no files
4. Conditions of access and use
Languageen
Target Filegravity inversion.pdf
User Groupadministrator
simone
Visibilityshown
Archiving Policydenypublisher denyfinaldraft
Read Permissiondeny from all and allow from 150.163
Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/3ESGTTP
DisseminationWEBSCI; PORTALCAPES.
Host Collectioncptec.inpe.br/walmeida/2003/04.25.17.12
6. Notes
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7. Description control
e-Mail (login)marciana
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