Porphyry
Mostrando 1-12 de 12 artigos, teses e dissertações.
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1. CaracterizaÃÃo tecnolÃgica e radiomÃtrica de um diabÃsio da regiÃo de ApuiarÃs - CE / Technological characterization and radiometric a region of diabase ApuiarÃs - CE
This paper presents the technological and mineralogical characteristics of a diabase, which outcrop in the form of dike is located in the district CanafÃstula in ApuiarÃs - CE. In order to assess their qualities for application as ornamental, were carried out technological tests of fitness levels and physical-mechanical, based on standards from ABNT, as we
IBICT - Instituto Brasileiro de Informação em Ciência e Tecnologia. Publicado em: 31/01/2011
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2. Os Depósitos de Cu-Au-Mo do tipo pórfiro de Bajo de La Alumbrera e Água Rica, Argentina : considerações genéticas sobre formação e fonte de minério
The world-class deposits of Bajo de la Alumbrera and Agua Rica in NW Argentina, are of the Cu-Au-Mo porphyry type (although Agua Rica has some epithermal characteristics). Both deposits are closely related to the activities and formation processes of the Miocene Farallón Negro Volcanic Complex. They are also controlled by the Tucuman Transfer Zone, which is
IBICT - Instituto Brasileiro de Informação em Ciência e Tecnologia. Publicado em: 2011
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3. Evolução magmática, alteração hidrotermal e gênese da mineralização de ouro e cobre do Palito, Província Aurífera do Tapajós (PA) / Magmatic evolution, hydrothermal alteration and geneseis of gold-copper mineralization at Palito, Tapajós Gold Province (PA)
The Palito porphyry type copper-gold deposit is located in the central region of the Amazonian craton, in the Tapajós Gold Province (TGP), in an area that is dominated by intermediate to felsic granitic and volcanic rocks of late Paleoproterozoic age. Three lithotypes make up this deposit. The Palito Granite, with porphyritic features, is the host rock for
Publicado em: 2010
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4. Características epigenéticas do depósito de cu-au chapada, arco magmático de goiás
The Cu-Au Chapada deposit is located from 8km of Alto Horizonte-GO. The geologic picture is dominated by metavulcanic sedimentary sequences that integrate the Neoproterozoic Magmatic Arc of Mara Rosa, located in the central portion of the Tocantins Province. The framework of the deposit is represented by an antiform whose core is composed by association of t
Publicado em: 2009
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5. Hydrothermal and superegene alteration of the El Salvador porphyry copper deposit, Chile : a study using multispectral and hyperspectral remote sensing data / Estudo da alteração hidrotermal e supergenica do deposito de cobre porfiro El Salvador - Cile : usando sensoriamento remoto multiespectral e hiperespectral
Foram avaliadas neste estudo técnicas exploratórias para a caracterização da alteração hidrotermal da região do depósito de cobre pórfiro de El Salvador, Chile. O trabalho abrangeu análises por espectroscopia de reflectância de 238 amostras de rochas com alteração hidrotermal, cobrindo parte do distrito de El Salvador. Estas análises foram util
Publicado em: 2009
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6. Caracterização e correlação de inclusões sólidas em pirita com alteração hidrotermais no pórfiro de cobre de Cuajone - Perú / Characterization and correlation of inclusions in pyrite with strong hydrothermal alterations in the porphyry copper Cuajone-Peru
A mina Cuajone é uma jazida de tipo pórfiro de cobre (porphyry copper), localizada na Província Cuprífera do Pacífico, nos flancos ocidentais da Cadeia Andina, no estado de Moquegua, sul do Perú, em coordenadas 17° 02(S) e 70° 42(W) e altitudes entre 3100 e 3830 m. A região é caracterizada pela ocorrência, na base, de derrames vulcânicos (andesit
Publicado em: 2008
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7. Processos metalogenéticos em ambientes de arco magmático tipo andino, caso de estudo: mineralizações da região dos Andes Patagônicos setentrionais do Chile / Metallogenic processes in andean volcanic arc setting, study case: mineralizations in the Chilean North-Patagonion Andes
In the Patagonian Andes region between 41 and 44° S extensive and continuous plutonic rocks of the North-Patagonian Batholith north segment are exposed. During their evolution most of the granitic rocks were emplaced in metamorphic rocks and other parts were emplaced in Late Jurassic-Berriasan volcanic rocks, Early Cretaceous sedimentary and volcanic rocks,
Publicado em: 2008
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8. Condutividade térmica de rochas: uma aplicação para granitos ornamentais
This dissertation focuses on rock thermal conductivity and its correlations with petrographic, textural, and geochemical aspects, especially in granite rocks. It aims at demonstrating the relations of these variables in an attempt to enlighten the behavior of thermal effect on rocks. Results can be useful for several applications, such as understanding and c
Publicado em: 2006
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9. Estudo de mineralizações de tipo Cu-porfiro do sul do Peru por meio de sensoriamento remoto e aeromagnetometria
A large number of mineral deposits are known in the Andes, including Cu-porphyry deposits. Among these, Cuajone, Quellaveco and Toquepala are some of the most important in the southern portion of Peru. They are located in the domain ofthe Bolivian Orocline, within the Incapuquio shear zone, a structure that controls the mineralization, ofabout 60 Ma. Airborn
Publicado em: 2002
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10. Natureza e evolução dos fluidos hidrotermais no deposito cupro-aurifero Golden Hill, Camaguey, Cuba
The Cu-Au mineralization at the Golden Hill deposit in the Las Tunas Province, Eastem Cuba, is characterized by breccia-hosted massive and semi-massive sulfide bodies confined to the Contramaestre Fonnation in the Cretaceous Volcanic Arc. The deposit is enveloped by a silicic, argillic and advanced argillic alteration assemblage, typical of high sulfidation
Publicado em: 2000
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11. Arizona porphyry copper/hydrothermal deposits II: Crystal structure of ajoite, (K + Na)3Cu20Al3Si29O76(OH)16⋅∼8H2O
A crystal from the type locality Ajo, AZ, yielded just enough intensity from streaked diffractions using synchrotron x-rays at the Advanced Photon Source to solve the crystal structure with composition (K + Na)3Cu20Al3Si29O76(OH)16⋅∼8H2O; triclinic, P1̄, a = 13.634(5) Å, b = 13.687(7), c = 14.522(7), α = 110.83(1)°, β = 107.21(1), γ = 105.68(1); r
National Academy of Sciences.
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12. Attached and Unattached Bacterial Communities in a 120-Meter Corehole in an Acidic, Crystalline Rock Aquifer
The bacteria colonizing geologic core sections (attached) were contrasted with those found suspended in the groundwater (unattached) by examining the microbiology of 16 depth-paired core and groundwater samples using a suite of culture-independent and culture-dependent analyses. One hundred twenty-two meters was continuously cored from a buried chalcopyrite
American Society for Microbiology.