Geological Setting & Seismic Interpretation

Detalhes bibliográficos
Autor(a) principal: Cramez, Carlos
Data de Publicação: 2007
Tipo de documento: Artigo de conferência
Idioma: eng
Título da fonte: Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Texto Completo: http://hdl.handle.net/10284/270
Resumo: Assuming that the understanding of tectonics and structural evolution allows geologists, and particularly seismic interpreters, to propose a priori interpretations in compressional areas, where the quality of seismic data is poor, the main geological concepts of Southern Rocky Mountains are review. Indeed, in this particular area, a priori knowledge, which contrasts with empiric knowledge (derived from sensorial experience), is absolutely necessary to interpret the seismic lines and so predict the more likely location of the exploration wells.
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spelling Geological Setting & Seismic InterpretationRocky MountainsCompressional StructuresMigration of ForedeepRegional CrosssectionsSeismic examples.Assuming that the understanding of tectonics and structural evolution allows geologists, and particularly seismic interpreters, to propose a priori interpretations in compressional areas, where the quality of seismic data is poor, the main geological concepts of Southern Rocky Mountains are review. Indeed, in this particular area, a priori knowledge, which contrasts with empiric knowledge (derived from sensorial experience), is absolutely necessary to interpret the seismic lines and so predict the more likely location of the exploration wells.Repositório Institucional da Universidade Fernando PessoaCramez, Carlos2007-04-12T07:47:04Z2007-01-01T00:00:00Z2007-01-01T00:00:00Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/conferenceObjectapplication/pdfhttp://hdl.handle.net/10284/270enginfo:eu-repo/semantics/openAccessreponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãoinstacron:RCAAP2022-09-06T02:00:21Zoai:bdigital.ufp.pt:10284/270Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-19T15:38:11.155878Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãofalse
dc.title.none.fl_str_mv Geological Setting & Seismic Interpretation
title Geological Setting & Seismic Interpretation
spellingShingle Geological Setting & Seismic Interpretation
Cramez, Carlos
Rocky Mountains
Compressional Structures
Migration of Foredeep
Regional Crosssections
Seismic examples.
title_short Geological Setting & Seismic Interpretation
title_full Geological Setting & Seismic Interpretation
title_fullStr Geological Setting & Seismic Interpretation
title_full_unstemmed Geological Setting & Seismic Interpretation
title_sort Geological Setting & Seismic Interpretation
author Cramez, Carlos
author_facet Cramez, Carlos
author_role author
dc.contributor.none.fl_str_mv Repositório Institucional da Universidade Fernando Pessoa
dc.contributor.author.fl_str_mv Cramez, Carlos
dc.subject.por.fl_str_mv Rocky Mountains
Compressional Structures
Migration of Foredeep
Regional Crosssections
Seismic examples.
topic Rocky Mountains
Compressional Structures
Migration of Foredeep
Regional Crosssections
Seismic examples.
description Assuming that the understanding of tectonics and structural evolution allows geologists, and particularly seismic interpreters, to propose a priori interpretations in compressional areas, where the quality of seismic data is poor, the main geological concepts of Southern Rocky Mountains are review. Indeed, in this particular area, a priori knowledge, which contrasts with empiric knowledge (derived from sensorial experience), is absolutely necessary to interpret the seismic lines and so predict the more likely location of the exploration wells.
publishDate 2007
dc.date.none.fl_str_mv 2007-04-12T07:47:04Z
2007-01-01T00:00:00Z
2007-01-01T00:00:00Z
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url http://hdl.handle.net/10284/270
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