Hyperspectral analysis (VNIR-SWIR) applied to the characterization of a dolomitization context: a case study in Rio Bonito Quarry, Brazil

[1]  C. Lamarão,et al.  Characteristics and mechanisms of multistage dolomitization in Proterozoic dolomitic breccia from Água Clara Formation, Ribeira Belt, Brazil , 2022, Carbonates and Evaporites.

[2]  A. Falcão,et al.  Hyperspectral data as a proxy for porosity estimation of carbonate rocks , 2022, Australian Journal of Earth Sciences.

[3]  S. Buckley,et al.  Quantitative mapping of dolomitization using close-range hyperspectral imaging: Kimmeridgian carbonate ramp, Alacón, NE Spain , 2022, Geosphere.

[4]  B. Rivard,et al.  Shortwave infrared hyperspectral imaging as a novel method to elucidate multi-phase dolomitization, recrystallization, and cementation in carbonate sedimentary rocks , 2021, Scientific Reports.

[5]  M. Barton,et al.  Extending geometallurgy to the mine scale with hyperspectral imaging: a pilot study using drone- and ground-based scanning , 2021, Mining, Metallurgy & Exploration.

[6]  Shuhab D. Khan,et al.  Close-range, ground-based hyperspectral imaging for mining applications at various scales: Review and case studies , 2019, Earth-Science Reviews.

[7]  A. P. Lopes,et al.  Hydrothermal dolomitization and porosity development: An example from Precambrian dolomitic rocks of Água Clara Formation, Ribeira Belt, southern Brazil , 2019, Journal of South American Earth Sciences.

[8]  C. John,et al.  Ground-based hyperspectral imaging as a tool to identify different carbonate phases in natural cliffs , 2018 .

[9]  B. P. Thornton,et al.  The effect of temperature on stoichiometry, cation ordering, and reaction rate in high-temperature dolomitization experiments , 2017 .

[10]  C. Scherer,et al.  Lithostratigraphy and volcanology of the Serra Geral Group, Paraná-Etendeka Igneous Province in Southern Brazil: Towards a formal stratigraphical framework , 2017 .

[11]  F. Nader Multi-scale Quantitative Diagenesis and Impacts on Heterogeneity of Carbonate Reservoir Rocks , 2016 .

[12]  Claudia Biermann,et al.  Mineralogical Applications Of Crystal Field Theory , 2016 .

[13]  D. Bish,et al.  Mineralogy, nucleation and growth of dolomite in the laboratory and sedimentary environment: A review , 2015 .

[14]  C. Tassinari,et al.  Diachronic collision, slab break-off and long-term high thermal flux in the Brasiliano–Pan-African orogeny: Implications for the geodynamic evolution of the Mantiqueira Province , 2015 .

[15]  Harald van der Werff,et al.  Determination of Carbonate Rock Chemistry Using Laboratory-Based Hyperspectral Imagery , 2014, Remote. Sens..

[16]  M. Boni,et al.  Hydrothermal dolomitization in a complex geodynamic setting (Lower Palaeozoic, northern Spain) , 2014 .

[17]  B. D. B. Neves,et al.  Neoproterozoic evolution of the basement of the South-American platform , 2013 .

[18]  R. P. Almeida,et al.  Recurring extensional and strike-slip tectonics after the Neoproterozoic collisional events in the southern Mantiqueira province , 2012 .

[19]  Harald van der Werff,et al.  Effect of Grain Size and Mineral Mixing on Carbonate Absorption Features in the SWIR and TIR Wavelength Regions , 2012, Remote. Sens..

[20]  B. D. B. Neves The Paleoproterozoic in the South-American continent: Diversity in the geologic time , 2011 .

[21]  D. Sibley,et al.  On the evolution of dolomite stoichiometry and cation order during high-temperature synthesis experiments: An alternative model for the geochemical evolution of natural dolomites , 2011 .

[22]  M. Basei,et al.  Major shear zones of southern Brazil and Uruguay: escape tectonics in the eastern border of Rio de La plata and Paranapanema cratons during the Western Gondwana amalgamation , 2011 .

[23]  Kei Sato,et al.  Geology and geochronology of the Betara region in south-southeastern Brazil: Evidence for possible Statherian (1.80–1.75 Ga) and Calymmian (1.50–1.45 Ga) extension events , 2011 .

[24]  N. Machado,et al.  Evolution of reworked Paleoproterozoic basement rocks within the Ribeira belt (Neoproterozoic), SE-Brazil, based on U–Pb geochronology: Implications for paleogeographic reconstructions of the São Francisco-Congo paleocontinent , 2010 .

[25]  M. Gomes,et al.  REVISÃO DA EXTENSÃO AREAL E DO VOLUME DA FORMAÇÃO SERRA GERAL, BACIA DO PARANÁ, AMÉRICA DO SUL , 2009 .

[26]  Kei Sato,et al.  Lower and Upper Neoproterozoic magmatic records in Itaiacoca Belt (Paraná-Brazil): Zircon ages and lithostratigraphy studies , 2009 .

[27]  A. Nutman,et al.  Constraining the age of the Iporanga Formation with SHRIMP U-Pb zircon: Implications for possible Ediacaran glaciation in the Ribeira Belt, SE Brazil , 2008 .

[28]  G. Davies,et al.  Structurally controlled hydrothermal dolomite reservoir facies: An overview , 2006 .

[29]  John F. Mustard,et al.  Detection and discrimination of sulfate minerals using reflectance spectroscopy , 2006 .

[30]  A. P. Nutman,et al.  A Formação Água Clara na Região de Araçaíba - SP: registro U-Pb de uma bacia mesoproterozóica , 2004 .

[31]  F. Meer Analysis of spectral absorption features in hyperspectral imagery , 2004 .

[32]  Celso Dal Ré Carneiro,et al.  Geologia do continente Sul-Americano: evolução da obra de Fernando Flávio Marques de Almeida , 2004 .

[33]  C. R. Passarelli,et al.  Litoquímica, geocronologia U-Pb e Geologia isotópica (Sr-Nd-Pb) das rochas graníticas dos batólitos Cunhaporanga e Três Córregos na porção sul do Cinturão Ribeira, Estado do Paraná , 2003 .

[34]  Roger,et al.  Spectroscopy of Rocks and Minerals , and Principles of Spectroscopy , 2002 .

[35]  B. Vivo,et al.  Hydrothermal dolomites in SW Sardinia (Italy): evidence for a widespread late-Variscan fluid flow event , 2000 .

[36]  F. D. van der Meer,et al.  Spectral reflectance of carbonate mineral mixtures and bidirectional reflectance theory: Quantitative analysis techniques for application in remote sensing , 1995 .

[37]  R. Reeder,et al.  Energetics of calcium-rich dolomite , 1995 .

[38]  Reis Neto,et al.  Faixa Itaiacoca: registro de uma colisão entre dois blocos continentais no Neoproterozóico , 1994 .

[39]  Gil Francisco Piekarz,et al.  O Granito Passa Tres, PR e as minerações auriferas associadas , 1992 .

[40]  R. Clark,et al.  High spectral resolution reflectance spectroscopy of minerals , 1990 .

[41]  James K. Crowley,et al.  Visible and near‐infrared spectra of carbonate rocks: Reflectance variations related to petrographic texture and impurities , 1986 .

[42]  SuseN J. Ger Spectral reflectance of-carbonate minerals in the visible and near infrared (0.35-2.55 microns): calcite, aragonite, and dolomite , 1986 .

[43]  S. Gaffey,et al.  Reflectance spectroscopy in the visible and near-infrared (0.35–2.55 µm): Applications in carbonate petrology , 1985 .

[44]  R. Mathis,et al.  On the Formation and Occurrence of Saddle Dolomite , 1980 .

[45]  D. Lumsden Discrepancy between thin-section and X-ray estimates of dolomite in limestone , 1979 .

[46]  Y. Hasui Evolução polifasica do precambriano a oeste de São Paulo , 1975 .

[47]  G. Hunt Visible and near-infrared spectra of minerals and rocks : I silicate minerals , 1970 .