{"id":17,"date":"2023-01-31T10:25:25","date_gmt":"2023-01-31T13:25:25","guid":{"rendered":"https:\/\/www.ige.unicamp.br\/geofisica\/?page_id=17"},"modified":"2025-03-24T20:07:11","modified_gmt":"2025-03-24T23:07:11","slug":"projetos","status":"publish","type":"page","link":"https:\/\/www.ige.unicamp.br\/geofisica\/projetos\/","title":{"rendered":"Projetos"},"content":{"rendered":"
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Estudo Geof\u00edsico das Estruturas de Impacto de Vista Alegre\/SC e Varge\u00e3o\/SC\u00a001-Jan-2011<\/small><\/p>\n\t\t\t

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\u00c9 proposto um estudo geof\u00edsico de duas crateras de impacto bas\u00e1lticas da Bacia do Paran\u00e1: Vista Alegre (di\u00e2metro \u2248 9,5 km) e Varge\u00e3o (di\u00e2metro \u2248 12 km). O estudo ser\u00e1 concentrado na coleta, processamento e interpreta\u00e7\u00e3o de dados gravim\u00e9tricos e magnetom\u00e9tricos terrestres. A coleta dos dados terrestres tem por objetivo a caracteriza\u00e7\u00e3o geof\u00edsica de detalhe das duas estruturas e as modelagens 2D e 3D das rochas em subsuperf\u00edcie. Embora comuns em outros planetas terrestres e suas respectivas luas, crateras de impacto formadas em basaltos s\u00e3o raras na Terra, sendo que apenas alguns poucos exemplos s\u00e3o conhecidos at\u00e9 hoje. Essas raras crateras bas\u00e1lticas terrestres podem fornecer importantes informa\u00e7\u00f5es para o estudo dos efeitos dos impactos em alvos bas\u00e1lticos. Em um contexto mais geral, os resultados deste projeto poder\u00e3o contribuir para o entendimento da g\u00eanese, forma\u00e7\u00e3o, estrutura\u00e7\u00e3o e deforma\u00e7\u00e3o destas duas estruturas de impacto e para a compreens\u00e3o da evolu\u00e7\u00e3o crustal da Bacia do Paran\u00e1.<\/p>\n\n\n

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Situa\u00e7\u00e3o<\/p>\n\t\t\t

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Conclu\u00eddo<\/p>\n\n<\/div>\n\t\t<\/div>\n\n

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Natureza<\/p>\n\t\t\t

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Pesquisa<\/p>\n\n<\/div>\n\t\t<\/div>\n\n

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Alunos envolvidos<\/p>\n\t\t\t

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    \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tGradua\u00e7\u00e3o: 2<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
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    \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tMestrado acad\u00eamico: 1<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n<\/div><\/ul>\n<\/div>\n\t\t<\/div>\n\n
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    Integrantes<\/p>\n\t\t\t

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      \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tEmilson Pereira Leite \u2013 Coordenador<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
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      \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\t\u00c1lvaro Penteado Cr\u00f3sta \u2013 Integrante<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n<\/div><\/ul>\n<\/div>\n\t\t<\/div>\n\n
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      Financiador(es)<\/p>\n\t\t\t

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      Funda\u00e7\u00e3o de Amparo \u00e0 Pesquisa do Estado de S\u00e3o Paulo \u2013 Aux\u00edlio financeiro<\/p>\n\n<\/div>\n\t\t<\/div>\n<\/div>\n<\/div>\n\t\t<\/div>\n<\/div>\n\n

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      Aplica\u00e7\u00e3o da gamaespectrometria na correla\u00e7\u00e3o de afloramentos com perfis geof\u00edsicos de po\u00e7os\u00a001-Jan-2011<\/small><\/p>\n\t\t\t

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      A perfilagem gamaespectrom\u00e9trica em afloramentos permite registrar pequenas varia\u00e7\u00f5es litol\u00f3gicas atrav\u00e9s das medidas das concentra\u00e7\u00f5es dos elementos K, Th e U, constituindo uma t\u00e9cnica ideal para caracteriza\u00e7\u00e3o objetiva e quantitativa de litof\u00e1cies e limites estratigr\u00e1ficos. Atrav\u00e9s da calibra\u00e7\u00e3o em afloramentos an\u00e1logos, \u00e9 poss\u00edvel melhorar os modelos de litof\u00e1cies em subsuperf\u00edcie, elaborados a partir de perfis geof\u00edsicos de po\u00e7os e testemunhos de rochas. Particularmente, isto torna a gamaespectrometria de superf\u00edcie potencialmente \u00fatil na caracteriza\u00e7\u00e3o de rochas reservat\u00f3rios, tendo sido recentemente utilizada na elabora\u00e7\u00e3o de modelos geol\u00f3gicos 3D de reservat\u00f3rios em ambientes similares. O principal problema a ser abordado \u00e9 a presente dificuldade em estabelecer a correla\u00e7\u00e3o estratigr\u00e1fica em subsuperf\u00edcie. Al\u00e9m disso, o car\u00e1ter similar de f\u00e1cies sedimentares existentes entre diferentes unidades e a fraca correla\u00e7\u00e3o lateral entre os limites das seq\u00fc\u00eancias estratigr\u00e1ficas aflorantes fazem com que exista uma grande ambig\u00fcidade ao se tentar estabelecer correla\u00e7\u00f5es individuais sem o uso da gamaespectrometria. Neste contexto, este projeto prop\u00f5e a coleta e interpreta\u00e7\u00e3o de dados gamaespectrom\u00e9tricos em afloramentos sedimentares do Grupo Tubar\u00e3o (Bacia do Paran\u00e1) e na Bacia de Taubat\u00e9. Estas duas \u00e1reas de estudo apresentam significativas heterogeneidades litol\u00f3gicas, o que implica em grande varia\u00e7\u00e3o na capacidade de fluxo de \u00e1gua. Desta forma, a caracteriza\u00e7\u00e3o dos reservat\u00f3rios utilizando todas as informa\u00e7\u00f5es geof\u00edsicas e geol\u00f3gicas, dispon\u00edveis em superf\u00edcie e em subsuperf\u00edcie, \u00e9 de fundamental import\u00e2ncia para o melhor entendimento dessas heterogeneidades. Os perfis gamaespectrom\u00e9tricos elaborados ser\u00e3o analisados e correlacionados com os perfis geof\u00edsicos de po\u00e7os e informa\u00e7\u00f5es geol\u00f3gicas dispon\u00edveis nas regi\u00f5es vizinhas aos afloramentos. Desta forma, este trabalho pretende fornecer novos dados para a caracteriza\u00e7\u00e3o geol\u00f3gica das rochas reservat\u00f3rios das duas.<\/p>\n\n\n

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      Situa\u00e7\u00e3o<\/p>\n\t\t\t

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      Conclu\u00eddo<\/p>\n\n<\/div>\n\t\t<\/div>\n\n

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      Natureza<\/p>\n\t\t\t

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      Pesquisa<\/p>\n\n<\/div>\n\t\t<\/div>\n\n

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      Integrantes<\/p>\n\t\t\t

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        \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tEmilson Pereira Leite \u2013 Coordenador<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
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        \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tAlexandre Campane Vidal \u2013 Integrante<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n<\/div><\/ul>\n<\/div>\n\t\t<\/div>\n<\/div>\n<\/div>\n\t\t<\/div>\n<\/div>\n\n
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        Caracteriza\u00e7\u00e3o geol\u00f3gica e geof\u00edsica da potencial estrutura de impacto de Santa Marta (PI)\u00a001-Jan-2012<\/small><\/p>\n\t\t\t

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        Atualmente 182 estruturas de impacto meteor\u00edtico s\u00e3o conhecidas na superf\u00edcie da Terra. No Brasil, apenas seis estruturas desse tipo foram diagnosticadas at\u00e9 o presente, tratando-se de tema de pesquisa que apenas recentemente vem ganhando express\u00e3o. O grupo de estudos de crateras de impacto do Instituto de Geoci\u00eancias da UNICAMP, coordenado pelo proponente deste projeto, tem pesquisado essas estruturas, o que tem permitido a identifica\u00e7\u00e3o de evid\u00eancias desse tipo raro de processo e sua caracteriza\u00e7\u00e3o geol\u00f3gica e geof\u00edsica. Isso vem permitindo nos \u00faltimos anos o desenvolvimento de projetos de colabora\u00e7\u00e3o com outros grupos nacionais e internacionais, propiciando o avan\u00e7o do conhecimento cient\u00edfico das crateras meteor\u00edticas brasileiras e a sua divulga\u00e7\u00e3o por meio de artigos cient\u00edficos em peri\u00f3dicos internacionais e em importantes f\u00f3runs cient\u00edficos internacionais dedicados aos temas da geologia planet\u00e1ria. A Bacia do Parna\u00edba cont\u00e9m diversas estruturas circulares com potencial de terem sido formadas por impacto meteor\u00edtico. A estrutura circular de Santa Marta (PI), em especial, mostrou-se como forte candidata ao apresentar, em estudo anterior do grupo de pesquisa, caracter\u00edsticas geof\u00edsicas compat\u00edveis com aquelas esperadas para estruturas de impacto. O presente projeto visa, portanto, dar continuidade \u00e0 investiga\u00e7\u00e3o da natureza da estrutura de Santa Marta, a partir de um trabalho detalhado de mapeamento geol\u00f3gico e de caracteriza\u00e7\u00e3o geof\u00edsica, com o objetivo de identificar fei\u00e7\u00f5es macro e microsc\u00f3picas de choque que comprovem sua origem por impacto, juntamente com uma an\u00e1lise da assinatura geof\u00edsica de detalhe e da modelagem num\u00e9rica da sua forma\u00e7\u00e3o.<\/p>\n\n\n

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        Situa\u00e7\u00e3o<\/p>\n\t\t\t

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        Conclu\u00eddo<\/p>\n\n<\/div>\n\t\t<\/div>\n\n

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        Natureza<\/p>\n\t\t\t

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        Pesquisa<\/p>\n\n<\/div>\n\t\t<\/div>\n\n

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        Alunos envolvidos<\/p>\n\t\t\t

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          \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tMestrado acad\u00eamico: 1<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
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          \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tDoutorado: 1<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n<\/div><\/ul>\n<\/div>\n\t\t<\/div>\n\n
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          Integrantes<\/p>\n\t\t\t

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            \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\t\u00c1lvaro Penteado Cr\u00f3sta \u2013 Coordenador<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
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            \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tEmilson Pereira Leite \u2013 Integrante<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
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            \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tAna Maria G\u00f3es \u2013 Integrante<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
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            \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tMarcos Alberto Rodrigues Vasconcelos \u2013 Integrante<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
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            \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tRaiumundo Mariano Gomes Castelo Branco \u2013 Integrante<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
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            \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tWolf Uwe Reimold \u2013 Integrante.<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n<\/div><\/ul>\n<\/div>\n\t\t<\/div>\n\n
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            Financiador(es)<\/p>\n\t\t\t

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            Funda\u00e7\u00e3o de Amparo \u00e0 Pesquisa do Estado de S\u00e3o Paulo \u2013 Aux\u00edlio financeiro<\/p>\n\n<\/div>\n\t\t<\/div>\n<\/div>\n<\/div>\n\t\t<\/div>\n<\/div>\n\n

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            M\u00e9todos de invers\u00e3o s\u00edsmica pr\u00e9-empilhamento aplicados a caracteriza\u00e7\u00e3o e modelagem de reservat\u00f3rios\u00a001-Jan-2013<\/small><\/p>\n\t\t\t

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            O objetivo principal do projeto \u00e9 estudar as possibilidades e limita\u00e7\u00f5es na recupera\u00e7\u00e3o de par\u00e2metros petrof\u00edsicos de reservat\u00f3rios de hidrocarbonetos a partir da invers\u00e3o simult\u00e2nea de dados s\u00edsmicos pr\u00e9-empilhamento. Os tipos de reservat\u00f3rio que constituir\u00e3o o foco dos estudos decorrentes desse projeto ser\u00e3o os carbon\u00e1ticos.<\/p>\n\n\n

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            Situa\u00e7\u00e3o<\/p>\n\t\t\t

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            Conclu\u00eddo<\/p>\n\n<\/div>\n\t\t<\/div>\n\n

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            Natureza<\/p>\n\t\t\t

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            Pesquisa<\/p>\n\n<\/div>\n\t\t<\/div>\n\n

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            Alunos envolvidos<\/p>\n\t\t\t

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              \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tMestrado acad\u00eamico: 2<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n<\/div><\/ul>\n<\/div>\n\t\t<\/div>\n\n
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              Integrantes<\/p>\n\t\t\t

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                \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tEmilson Pereira Leite \u2013 Coordenador<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n<\/div><\/ul>\n<\/div>\n\t\t<\/div>\n\n
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                Financiador(es)<\/p>\n\t\t\t

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                Funda\u00e7\u00e3o de Amparo \u00e0 Pesquisa do Estado de S\u00e3o Paulo \u2013 Aux\u00edlio financeiro<\/p>\n\n<\/div>\n\t\t<\/div>\n<\/div>\n<\/div>\n\t\t<\/div>\n<\/div>\n\n

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                Estudo Geof\u00edsico da Estrutura de Cerro do Jara\u00fa\u00a001-Jan-2014<\/small><\/p>\n\t\t\t

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                O projeto tem como objetivo principal avaliar a hip\u00f3tese de impacto meteor\u00edtico para explicar a forma\u00e7\u00e3o da estrutura de Cerro do Jarau, localizada no munic\u00edpio de Quara\u00ed\/RS, com base em modelos geol\u00f3gicos elaborados por meio de invers\u00f5es de dados de gravimetria e magnetometria, al\u00e9m de interpreta\u00e7\u00f5es de dados gamaespectrom\u00e9tricos. Apesar de n\u00e3o estar comprovada, essa hip\u00f3tese para forma\u00e7\u00e3o da estrutura \u00e9 sustentada pelas evid\u00eancias geol\u00f3gicas encontradas at\u00e9 o momento. Todos os dados geof\u00edsicos ser\u00e3o coletados, processados e interpretados no sentido de caracterizar os principais padr\u00f5es de anomalias geof\u00edsicas. Posteriormente, ser\u00e3o elaborados modelos 3D de distribui\u00e7\u00e3o de densidades e magnetiza\u00e7\u00f5es em subsuperf\u00edcie levando em conta as informa\u00e7\u00f5es geol\u00f3gicas dispon\u00edveis. Espera-se que esses modelos ampliem o conhecimento geol\u00f3gico de subsuperf\u00edcie desta e de outras estruturas similares, formadas sobre rochas bas\u00e1lticas.<\/p>\n\n\n

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                Situa\u00e7\u00e3o<\/p>\n\t\t\t

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                Conclu\u00eddo<\/p>\n\n<\/div>\n\t\t<\/div>\n\n

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                Natureza<\/p>\n\t\t\t

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                Pesquisa<\/p>\n\n<\/div>\n\t\t<\/div>\n\n

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                Alunos envolvidos<\/p>\n\t\t\t

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                  \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tGradua\u00e7\u00e3o: 2<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
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                  \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tMestrado acad\u00eamico: 1<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n<\/div><\/ul>\n<\/div>\n\t\t<\/div>\n\n
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                  Integrantes<\/p>\n\t\t\t

                  <\/span><\/div>\n\t\t<\/div>\n\t\t\t
                  \n
                    \n
                  • \n\t\t\t
                    \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tEmilson Pereira Leite \u2013 Coordenador<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
                  • \n\t\t\t
                    \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\t\u00c1lvaro Penteado Cr\u00f3sta \u2013 Integrante<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
                  • \n\t\t\t
                    \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tMarcos Alberto Rodrigues Vasconcelos \u2013 Integrante<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n<\/div><\/ul>\n<\/div>\n\t\t<\/div>\n\n
                    \n\t\t\t
                    \n\t\t\t

                    Financiador(es)<\/p>\n\t\t\t

                    <\/span><\/div>\n\t\t<\/div>\n\t\t\t
                    \n\n

                    Funda\u00e7\u00e3o de Amparo \u00e0 Pesquisa do Estado de S\u00e3o Paulo \u2013 Aux\u00edlio financeiro<\/p>\n\n<\/div>\n\t\t<\/div>\n<\/div>\n<\/div>\n\t\t<\/div>\n<\/div>\n\n

                    \n
                    \n\t\t\t
                    \n\t\t\t

                    Predi\u00e7\u00e3o de litof\u00e1cies utlizando atributos s\u00edsmicos e dados de po\u00e7os\u00a001-Jan-2016<\/small><\/p>\n\t\t\t

                    <\/span><\/div>\n\t\t<\/div>\n\t\t\t
                    \n\n

                    O problema b\u00e1sico a ser abordado neste projeto \u00e9 como relacionar os volumes de atributos s\u00edsmicos (p. e.x. imped\u00e2ncia P, imped\u00e2ncia S, Vp\/Vs, densidade) obtidos com invers\u00f5es s\u00edsmicas aos perfis geof\u00edsicos de po\u00e7os. Uma maneira rotineira de se fazer isso \u00e9 atrav\u00e9s de diagramas de correla\u00e7\u00e3o cruzada entre esses par\u00e2metros e ent\u00e3o destacar certas zonas selecionadas nos diagramas, as quais correspondem a determinadas litof\u00e1cies. Essas zonas s\u00e3o ent\u00e3o identificadas e marcadas no volume s\u00edsmico. O problema \u00e9 que a \u00e1rea interpretada no volume depende criticamente do tamanho da zona selecionada no diagrama. Portanto, em vez de definir um limiar de corte arbitr\u00e1rio para delimitar a zona de interesse, a ideia da abordagem a ser seguida neste projeto \u00e9 trabalhar com distribui\u00e7\u00f5es de probabilidade, sendo que essas distribui\u00e7\u00f5es devem ser mapeadas no volume s\u00edsmico usando uma classifica\u00e7\u00e3o bayesiana.<\/p>\n\n\n

                    \n
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                    Situa\u00e7\u00e3o<\/p>\n\t\t\t

                    <\/span><\/div>\n\t\t<\/div>\n\t\t\t
                    \n\n

                    Conclu\u00eddo<\/p>\n\n<\/div>\n\t\t<\/div>\n\n

                    \n\t\t\t
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                    Natureza<\/p>\n\t\t\t

                    <\/span><\/div>\n\t\t<\/div>\n\t\t\t
                    \n\n

                    Pesquisa<\/p>\n\n<\/div>\n\t\t<\/div>\n\n

                    \n\t\t\t
                    \n\t\t\t

                    Alunos envolvidos<\/p>\n\t\t\t

                    <\/span><\/div>\n\t\t<\/div>\n\t\t\t
                    \n
                      \n
                    • \n\t\t\t
                      \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tGradua\u00e7\u00e3o: 1<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
                    • \n\t\t\t
                      \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tMestrado acad\u00eamico: 1<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
                    • \n\t\t\t
                      \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tDoutorado: 1<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n<\/div><\/ul>\n<\/div>\n\t\t<\/div>\n\n
                      \n\t\t\t
                      \n\t\t\t

                      Integrantes<\/p>\n\t\t\t

                      <\/span><\/div>\n\t\t<\/div>\n\t\t\t
                      \n
                        \n
                      • \n\t\t\t
                        \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tEmilson Pereira Leite \u2013 Coordenador<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n<\/div><\/ul>\n<\/div>\n\t\t<\/div>\n<\/div>\n<\/div>\n\t\t<\/div>\n<\/div>\n\n
                        \n
                        \n\t\t\t
                        \n\t\t\t

                        Gravimetria e gamaespectrometria da cratera de impacto de Araguainha\u00a001-Jan-2017<\/small><\/p>\n\t\t\t

                        <\/span><\/div>\n\t\t<\/div>\n\t\t\t
                        \n\n

                        \u00c9 proposto um estudo gravim\u00e9trico e gamaespectrom\u00e9trico da cratera de impacto de Araguainha. O estudo consistir\u00e1 no processamento e interpreta\u00e7\u00e3o geol\u00f3gica de dados gravim\u00e9tricos e gamaespectrom\u00e9tricos terrestres a serem coletados durante o projeto. Pretende-se caracterizar as anomalias gravim\u00e9tricas da \u00e1rea e elaborar modelos tridimensionais da distribui\u00e7\u00e3o de densidades de massa em subsuperf\u00edcie. Esses modelos dever\u00e3o refletir os contatos litol\u00f3gicos e as estruturas em profundidade, contribuindo para o entendimento da evolu\u00e7\u00e3o geol\u00f3gica dessa estrutura de impacto. Os dados gamaespectrom\u00e9tricos fornecer\u00e3o mapas das concentra\u00e7\u00f5es dos elementos radioativos U238, Th232 e K40, al\u00e9m de produtos derivados, tais como mapas de raz\u00f5es entre os elementos e do pot\u00e1ssio an\u00f4malo que, quando associados \u00e0s informa\u00e7\u00f5es publicadas de petrografia, poder\u00e3o revelar a presen\u00e7a de zonas de altera\u00e7\u00e3o hidrotermal associadas \u00e0 cratera. Os resultados de ambos os m\u00e9todos ser\u00e3o interpretados em conjunto, \u00e0 luz do conhecimento geol\u00f3gico da cratera.<\/p>\n\n\n

                        \n
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                        Situa\u00e7\u00e3o<\/p>\n\t\t\t

                        <\/span><\/div>\n\t\t<\/div>\n\t\t\t
                        \n\n

                        Conclu\u00eddo<\/p>\n\n<\/div>\n\t\t<\/div>\n\n

                        \n\t\t\t
                        \n\t\t\t

                        Natureza<\/p>\n\t\t\t

                        <\/span><\/div>\n\t\t<\/div>\n\t\t\t
                        \n\n

                        Pesquisa<\/p>\n\n<\/div>\n\t\t<\/div>\n\n

                        \n\t\t\t
                        \n\t\t\t

                        Alunos envolvidos<\/p>\n\t\t\t

                        <\/span><\/div>\n\t\t<\/div>\n\t\t\t
                        \n
                          \n
                        • \n\t\t\t
                          \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tGradua\u00e7\u00e3o: 1<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
                        • \n\t\t\t
                          \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tEspecializa\u00e7\u00e3o: 1<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
                        • \n\t\t\t
                          \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tMestrado acad\u00eamico: 1<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n<\/div><\/ul>\n<\/div>\n\t\t<\/div>\n\n
                          \n\t\t\t
                          \n\t\t\t

                          Integrantes<\/p>\n\t\t\t

                          <\/span><\/div>\n\t\t<\/div>\n\t\t\t
                          \n
                            \n
                          • \n\t\t\t
                            \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tEmilson Pereira Leite \u2013 Coordenador<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
                          • \n\t\t\t
                            \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\t\u00c1lvaro Penteado Cr\u00f3sta \u2013 Integrante<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
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                            \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tMarcos Alberto Rodrigues Vasconcelos \u2013 Integrante<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n<\/div><\/ul>\n<\/div>\n\t\t<\/div>\n<\/div>\n<\/div>\n\t\t<\/div>\n<\/div>\n\n
                            \n
                            \n\t\t\t
                            \n\t\t\t

                            An\u00e1lise integrada multi-escala de rochas carbon\u00e1ticas do pr\u00e9-sal para caracteriza\u00e7\u00e3o e previs\u00e3o de propriedades de reservat\u00f3rios\u00a001-Jan-2019<\/small><\/p>\n\t\t\t

                            <\/span><\/div>\n\t\t<\/div>\n\t\t\t
                            \n\n

                            O objetivo geral do projeto \u00e9 desenvolver e aplicar metodologias para caracteriza\u00e7\u00e3o e predi\u00e7\u00e3o multi-escala de propriedades de reservat\u00f3rios carbon\u00e1ticos do pr\u00e9-sal, integrando dados petrof\u00edsicos, informa\u00e7\u00f5es geol\u00f3gicas, dados de perfis de po\u00e7os e dados s\u00edsmicos. Ser\u00e3o obtidas uma s\u00e9rie de medi\u00e7\u00f5es petrof\u00edsicas cl\u00e1ssicas e modernas, para vincular previs\u00f5es de propriedades petrof\u00edsicas a partir de par\u00e2metros el\u00e1sticos baseados em t\u00e9cnicas de Aprendizado de M\u00e1quina (ML \u2013 Machine Learning) desenvolvidos recentemente e em algoritmos de invers\u00e3o s\u00edsmica-petrof\u00edsica probabil\u00edstica. As invers\u00f5es ser\u00e3o aplicadas para previs\u00e3o de propriedades petrof\u00edsicas em regi\u00f5es onde somente dados s\u00edsmicos est\u00e3o dispon\u00edveis. A metodologias propostas dever\u00e3o levar em conta as incertezas de forma robusta, a fim de mitigar o risco de perfura\u00e7\u00e3o de po\u00e7os secos, juntamente com t\u00e9cnicas apropriadas de transfer\u00eancia de escala para transformar os dados de escala fina (escala de poros; micr\u00f4metros) para escala m\u00e9dia (escala de perfis de po\u00e7os; cent\u00edmetros) at\u00e9 escala grossa (escala s\u00edsmica; metros) minimizando a perda de informa\u00e7\u00e3o.<\/p>\n\n\n

                            \n
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                            \n\t\t\t

                            Situa\u00e7\u00e3o<\/p>\n\t\t\t

                            <\/span><\/div>\n\t\t<\/div>\n\t\t\t
                            \n\n

                            Em andamento<\/p>\n\n<\/div>\n\t\t<\/div>\n\n

                            \n\t\t\t
                            \n\t\t\t

                            Natureza<\/p>\n\t\t\t

                            <\/span><\/div>\n\t\t<\/div>\n\t\t\t
                            \n\n

                            Pesquisa<\/p>\n\n<\/div>\n\t\t<\/div>\n\n

                            \n\t\t\t
                            \n\t\t\t

                            Alunos envolvidos<\/p>\n\t\t\t

                            <\/span><\/div>\n\t\t<\/div>\n\t\t\t
                            \n
                              \n
                            • \n\t\t\t
                              \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tMestrado acad\u00eamico: 3<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
                            • \n\t\t\t
                              \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tDoutorado: 2<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n<\/div><\/ul>\n<\/div>\n\t\t<\/div>\n\n
                              \n\t\t\t
                              \n\t\t\t

                              Integrantes<\/p>\n\t\t\t

                              <\/span><\/div>\n\t\t<\/div>\n\t\t\t
                              \n
                                \n
                              • \n\t\t\t
                                \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tEmilson Pereira Leite \u2013 Coordenador<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
                              • \n\t\t\t
                                \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tAlexandre Cruz Sanchetta \u2013 Integrante<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
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                                \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tHenrique Bueno dos Santos \u2013 Integrante<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
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                                \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tAlessandro Batezelli \u2013 Integrante<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
                              • \n\t\t\t
                                \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tGelvam Andr\u00e9 Hartmann \u2013 Integrante<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
                              • \n\t\t\t
                                \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tNath\u00e1lia Helena Secol Mattos \u2013 Integrante<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
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                                \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tRafael Medeiros de Souza \u2013 Integrante<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
                              • \n\t\t\t
                                \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tMarta Henriques J\u00e1como \u2013 Integrante<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n<\/div><\/ul>\n<\/div>\n\t\t<\/div>\n<\/div>\n<\/div>\n\t\t<\/div>\n<\/div>\n\n
                                \n
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                                \n\t\t\t

                                O campo paleomagn\u00e9tico m\u00e9dio na \u00c1merica do Sul entre 0-5 Ma\u00a001-Jan-2019<\/small><\/p>\n\t\t\t

                                <\/span><\/div>\n\t\t<\/div>\n\t\t\t
                                \n\n

                                <\/p>\n\n\n

                                \n
                                \n\t\t\t
                                \n\t\t\t

                                Situa\u00e7\u00e3o<\/p>\n\t\t\t

                                <\/span><\/div>\n\t\t<\/div>\n\t\t\t
                                \n\n

                                Em andamento<\/p>\n\n<\/div>\n\t\t<\/div>\n\n

                                \n\t\t\t
                                \n\t\t\t

                                Natureza<\/p>\n\t\t\t

                                <\/span><\/div>\n\t\t<\/div>\n\t\t\t
                                \n\n

                                Pesquisa<\/p>\n\n<\/div>\n\t\t<\/div>\n\n

                                \n\t\t\t
                                \n\t\t\t

                                Alunos envolvidos<\/p>\n\t\t\t

                                <\/span><\/div>\n\t\t<\/div>\n\t\t\t
                                \n
                                  \n
                                • \n\t\t\t
                                  \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tMestrado acad\u00eamico: 1<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
                                • \n\t\t\t
                                  \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tDoutorado: 1<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n<\/div><\/ul>\n<\/div>\n\t\t<\/div>\n\n
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                                  \n\t\t\t

                                  Integrantes<\/p>\n\t\t\t

                                  <\/span><\/div>\n\t\t<\/div>\n\t\t\t
                                  \n
                                    \n
                                  • \n\t\t\t
                                    \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tGelvam Andr\u00e9 Hartmann \u2013 Coordenador<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
                                  • \n\t\t\t
                                    \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tRicardo Ivan Ferreira da Trindade \u2013 Integrante<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
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                                    \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tJairo Francisco Savian \u2013 Integrante<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
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                                    \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tThiago Ribas Moncinhatto \u2013 Integrante<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
                                  • \n\t\t\t
                                    \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tCarlos Augusto Sommer \u2013 Integrante<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n\n
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                                    \n\t\t\t\t\n\t\t\t\t\t<\/path><\/svg>\n\t\t\t\t<\/span>\n\t\t\t\tWellington Paulo de Oliveira \u2013 Integrante<\/span>\n\t\t\t<\/div>\n\t\t\t\n\t\t<\/li>\n<\/div><\/ul>\n<\/div>\n\t\t<\/div>\n\n
                                    \n\t\t\t
                                    \n\t\t\t

                                    Financiador(es)<\/p>\n\t\t\t

                                    <\/span><\/div>\n\t\t<\/div>\n\t\t\t
                                    \n\n

                                    Conselho Nacional de Desenvolvimento Cient\u00edfico e Tecnol\u00f3gico \u2013 Aux\u00edlio financeiro.<\/p>\n\n<\/div>\n\t\t<\/div>\n<\/div>\n<\/div>\n\t\t<\/div>\n\n

                                    \n\t\t\t
                                    \n\t\t\t

                                    O Atl\u00e2ntico Sul em um planeta 2\u00b0C mais quente 01-Mar-2023<\/small><\/p>\n\t\t\t

                                    <\/span><\/div>\n\t\t<\/div>\n\t\t\t
                                    <\/div>\n\t\t<\/div>\n<\/div>\n\n\n

                                    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