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1. Identity statement
Reference TypeConference Paper (Conference Proceedings)
Sitesibgrapi.sid.inpe.br
Holder Codeibi 8JMKD3MGPEW34M/46T9EHH
Identifier83LX3pFwXQZeBBx/fLgGL
Repositorydpi.inpe.br/banon/1999/01.13.19.10
Last Update1999:01.18.02.00.00 (UTC) administrator
Metadata Repositorysid.inpe.br/banon/2001/03.30.15.53.57
Metadata Last Update2022:06.14.00.16.32 (UTC) administrator
Citation KeySantaRosa:1998:ImPrTe
TitleAn image processing technique to derive geological discontinuities in South America
Year1998
Access Date2024, May 03
Number of Files1
Size105 KiB
2. Context
AuthorSanta Rosa, Antônio Nuno de Castro
EditorCosta, L. da F
Camara, G.
Conference NameInternational Symposium on Computer Graphics, Image Processing and Vision, 11 (SIBGRAPI)
Conference LocationRio de Janeiro, RJ, Brazil
Date20-23 Oct. 1998
PublisherSociedade Brasileira de Computação
Publisher CityPorto Alegre
Book TitleProceedings
Tertiary TypeFull Paper
OrganizationSBC - Sociedade Brasileira de Computação
History (UTC)2008-07-17 14:17:53 :: administrator -> banon ::
2008-08-26 15:25:26 :: banon -> administrator ::
2009-08-13 20:35:55 :: administrator -> banon ::
2010-10-01 04:19:36 :: banon -> administrator ::
2022-06-14 00:16:32 :: administrator -> :: 1998
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Keywordsimage processing
image modeling
moho discontinuity
geology
processamento de imagem
modelagem de imagem
reconhecimento de padrão
AbstractThe aim of this paper is to construc an image from Moho discontinuity in South America. This result can be obtained through global modeling of Rayleigh waves phase and group velocity (ROSA (1986) and SANTA ROSA (1996)). The initial 2-D inversion model was defined according to the geographic position of each block, sized 10 x 10 degrees by ROSA (1986), in the continent and in the ocean. As a result of the inversion, we obtained global group velocity, i.e. the images for the following periods: 50, 55, 60, 65, 70 e 75 seconds. In the next step, 48 blocks were selected; that is, the number of blocks that cover the whole extension of South America. Global phase and group velocity inversions were made for each block, thus determining shear wave versus depth images. Finally, to determine the image of the Mohorocivic discontinuity for South America, we fixed the minimum value for shear wave velocity in 4.6 km/s and interpolated it for all blocks. The final result is the first image of the Moho discontinuity in South America. This work was supported by the Brazilian National Council for Scientific and Technological Development (CNPq).
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4. Conditions of access and use
data URLhttp://urlib.net/ibi/83LX3pFwXQZeBBx/fLgGL
zipped data URLhttp://urlib.net/zip/83LX3pFwXQZeBBx/fLgGL
Target Filesse079.pdf
User Groupadministrator
Visibilityshown
5. Allied materials
Next Higher Units8JMKD3MGPEW34M/46RGNB8
8JMKD3MGPEW34M/4742MCS
Citing Item Listsid.inpe.br/sibgrapi/2022/05.08.04.49 3
Host Collectionsid.inpe.br/banon/2001/03.30.15.38
6. Notes
NotesThe conference was held in Rio de Janeiro, RJ, Brazil, from October 20 to 23.
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