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|a 9781107696297
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|a WAA
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|a spa
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|a Frost, B. Ronald
|9 16265
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|a Essentials of igneous and metamorphic petrology /
|c B. Ronald Frost and Carol D. Frost
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|a 1st. ed.
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260 |
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|a Cambridge :
|b Cambridge University Press,
|c 2014
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300 |
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|a [xiv], 303 p. :
|b 28 cm.
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|a Incluye Indice analLtico
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|a 1. Introduction to igneous Petrology -- 1.1 Introduction -- 1.2 The scope of igneous Petrology -- 1.3 Clasification of Igneous Rocks -- 1.3.1 Preliminary Classification -- 1.3.2 IUGS Clasification of Plutonic Rocks -- 1.3.2 IUGS Clasification of volcanic and Hypabyssal Rocks -- 1.4 Igneous Textures -- 1.4.1 Crystal Size -- 1.4.2 Crystal Shape -- 1.5 Igneous Structures -- 1.5.1 Structures in Volcanic Flows -- 1.5.2 Structures in Pyroclastic Deposits -- 1.5.3 Structures in Hypabyssal Rocks -- 1.5.4 Structures in Plutonic Rocks.
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|a 2. An introduction o igneous Phase Diagrams -- 2.1 Introductión -- 2.2 The Phase Rule -- 2.3 The Lever Rule -- 2.4 Two-Component Systems Involving Melt -- 1.4.1 Binary Systems with a Eutectic -- 1.4.2 Binary systems with a Peritectic -- 2.4.3 Binary systems with a Thermal Barrier -- 2.4.4 Binary systems with Solid Solution -- 2.4.5 Binary systems with Partial Solid Solution -- 2.5 Phase Diagrams of Ternary Systems -- 2.5.1 The Ternary Sstem Mg2SiO4- CaAl2S2O8 - CagSi2O6 -- 2.6 Implications for Petrology Summary.
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|a 3. Introduction to silicate Melts and Magmas .3.1 Introduction -- 3.2 The role of volatiles -- 3.2.1 Rle of H2O -- 3.2.2 Role of CO2 -- 3.3 Physical Properties of Magma -- 3.3.1 Temperature -- 3.3.2 Heat Capacity and Heat of Fusión -- 3.3.3 Viscosity -- 3.3.4 Density -- 3.4 The Ascent of Magmas -- 3.5.2 Crystallization Processes -- 3.5.3 Liquid-liquid Fractionation -- 3.5.4 Assimilation -- 3.5.5 Magma Mixing.
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|a 4. The chemistry of igneous Rocks -- 4.1 Introduction -- 4.2 Modal Mineralogy versus Normative Mineralgy -- 4.3 Variation Diagrams Based on Major Elements -- 4.4 Major Element Indicees of Differntiation -- 4.4.1 Modified Alkali- Lime Index -- 4.4.2 Iron Enrichment Index -- 4. 4.3 Aluminum Saturation Index -- 4.4.4 Alkalinity Index --4.4.5 Feldspathoid Silica Saturation Index -- 4.5 Identification of Differentiation Processes Using Trace Elements -- 4.5.1 Use of trace elements to model melting anda Crystallization Processes -- 4.5.2 Graphical Representations of trace element compositions -- 4.6 Application of Stable and radioactive isotopes in igneouus petrology -- 4.6.1 Geochrology -- 4.6.2 Isotopic Tracing of magma sources.
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|a 5. Basalts and mantle structure -- 5.1 Introduction -- 5.2 Basalt petrology -- 5.2.1 Classification -- 5.2.2 Chemistry and petrography -- 5.3 Melt generation from the mantle -- 5.3.1 Mntle composition -- 5.3.2 Crust and mantle structure -- 5.3.3 Mechanisms for partial melting of the mantle -- 5.3.4 The process of manle Melting -- 5.3.5 Origin of tholeiitic versus Alkali Basalts -- 5.4 Environments where magmas are generated.
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|a 6. Ocean magmatism. 6.1 Introduction -- 6.2 The petrology and structure of the crust -- 6.2.1 Ophiolites as a model of the ocean crust -- 6.2.2 Refinements of the Ophiolite model -- 6.3 Petrography and geochemistry of oceanic magmatism --
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|a 7. Convergent margin magmatism -- 7.1 Introduction -- 7.2 Oceanic and Continental Arcs -- 7.2.1 Island Arc Magmatism -- 7.2.2 Continental Arc Magmatism -- 7.2.3 Structure of Island and continental Arcs -- 7.2.4 Examples of Island and Continental Arcs --7.3 Petrographic characteristics of island and continental Arc Rocks -- 7.3.1 Petrograph of island Arc Rocks -- 7.3.2 Petrography of continental Arc Rocks -- 7.4 Geochemical characteristiccs of convergent margin magma series -- 7.4.1 Comparison of oceanic and Arcs differentiation trends -- 7.4.2 Comparisson of Island and continental Arc Magma series -- 7.4.3 Comparison of oceanic and continental (cordilleram) plutonic complexes -- 7.4.4 Geochemical Identification of contrasting processes forming Seguam and Mount saint Helens -- 7.5 Magma generation at convergent Margins.
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|a 8. Intracontinetal volcanism. 8.1 Continental floodBasalt Providences -- 8.2.1 The columbia Plateau-Sbake River Plain Province -- 8.2.2 Petroraphy and chemistry of continental Flood Basalts -- 8.2.3 Models for the generation os continental Flood Basalts -- 8.3 Bimodal volcanism --8.3.1 Bimodal volcanism in the Yellowstone-Sanke River plain providence -- 8.3.2 Geochemistry of the Yellowston-Snake river Plain Bimodal Suite -- 8.3.3 Models for the generation of Bimodal volcanism -- 8.4 Alkaline volcanism -- 8.4.1 Sodic alkaline magmatism of the East African Rift -- 8.4.2 Potassic Alkaline Volcanism -- 8.5 Origin of the chemical diversity of Intracontiental Basaltic Magmas.
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|a 9. Intracontinental Plutonism. 9.1 Introduction -- 9.2 Layered mafic intrusions-- 9.2.1 The bushveld intrusion -- 9.2.2 Mineralogical Variation in LMIs -- 9.2.3 Granitic Rocks associated with LMIs -- 9.2.4 Tectonic Environments of LMIs -- 9.3 Anorthosites and related rocks -- 9.3.1 Archean anorthosites -- 9.3.2 Massif anorthosites -- 9.4 Ferroan granites -- 9.4.1 The pikes peak Batholith -- 9.4.2 The composition of ferroan franites -- 9.5 Alkaline complexes -- 9.5.1 Geology of the ilimaussaq Intrusion.
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|a 10. Interpretaction of granitic rocks. 10.1 Introduction -- 10.2 Classification of granites rocks -- 10.2.1 Mineralogical classification -- 10.2.2 Clasaification based on Opaque Oxides -- 10.2.3 Alphabetic classification -- 10.2.4 Geochemical classification -- 10.3 Peraluminous Leucogranites -- 10.3.1 Himalayan leucogranites -- 10.3.2 Geochemical of peraluminous leucogranites -- 10.4 Caledonian granites - 10.4.1 The etive granite -- 10.4.2 Geochemistry and origin of caledonian granites -- 10.5 Review of the four Main granite Types Summary.
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|a 11. Introduction to metamorphic petrology -- 11.1 Introduction -- 11.2 The scope of metamophism -- 11.3 Types of metamorphism -- 11.3.1 Regional metamorphism -- 11.3.2 Contact metamorphism --11.3.3 Burial metamorphism -- 11.3.4 Dynamic metamorphism -- 11.3.5 Hydrothermal metamorphism -- 11.4 Basic goals of metamorphic petrology -- 11.5 Identification of protolith -- 11.5.1 Rocks of clearly sedimentary parentage -- 11.5.2 Rocks of clearly igneous parentage -- 11.5.3 Rocks of uncertain parentage -- 11.6 Determination of metamorphic conditions -- 11.6.1 Stability range of single minerals -- 11.6.2 Stability of mineral Assemblages -- 11.6.3 Metamorphic facies -- 11.6.4 Thermobarometry -- 11.7 Metamorphic textures -- 11.7.1 Primary textures -- 11.7.2 Metamorphic txtures -- 11.8 Naming a metamorphic rocks.
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|a 12. Interpretacition of metamorphic phase diagrams -- 12.1 Introduction -- 12.2 A little history -- 12.3 Use of chemographic projections -- 12.3.1 Chemographic projections in a two-component system --12.3.2 Chemographic projections in a three-component system -- 12.3.3 Chemographic projections in systems with four and more components.
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|a 13. Metamorphic facies and the metamorphism of mafic rocks -- 13.1 Introduction -- 13.2 Definition of metamorphic facies -- 13.3 Facies of regional metamorphism -- 13.3.1 Greenschist facies -- 13.3.2 Blueschist facies -- 13.3 Amphibolite facies -- 13.3.4 Very low-temperature metamorphism --13.3.5 Granulite facies -- 13.3.6 Eclogite facies -- 13.4 Facies of contact metamorphism -- 13.5 Textural changes during metamorphism -- 13.6 Mafic mineral assemblages at increasing temperature and pressure -- 13.6.1 Relations at very low temperatures -- 13.6.2 Relations at Low Pressre with increasing temperature -- 13.6.3 Relation at Low Temperature with increasing pressure.
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|a 14. Thermobarometry and the conditions of metamorphism -- 14.1 Introduction -- 14.2 Review of thermodynamics -- 14.2 .1 Free energy -- 14.2.2 Effect of changes in pressuere and temperature on AG -- 14.2.3 The equilibrium constant -- 14.2.4 Activity-composition relations -- 14.3 Thermobarometers -- 14.3.1 Geothermomentry -- 14.3.2 Geobarometry --14.3.3 Thermobarometry -- 14.4 Conditions of metamorphism -- 14.4.1 The pressure and temperature conditionns for the metamorphic facies -- 14.4.2 The upper temperature limts to metamorphsim and migmatites.
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|a 15.Metamorphism of peridotitic rocks -- 15.1 Introduction -- 15.2 The process of serpentinization -- 15.3 Prograde metamorphsim of serpentinite : reactions in the system CaO- MgO-SiO-2H2O -- 15.4 Role of minor components -- 15.4.1 Iron -- 15.4.2 Aluminum -- 15.5 Metaperidotites and metamorphic facies --15.6 Role of CO2 in metamorphic of peridotites -- 15.7 Metasomatism of peridotites -- 15.8 Examples of metaperidotites in the field -- 15.8.1 Malenco serpentinite -- 15.8.2 Ingalls peridotite.
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|a 16. Metamorphism of pelitic rocks -- 16.1 Introduction -- 16.2 Chemographic projestions for pelitic systems -- 16.2.1 Chemographic projections for continuous reactions -- 16.2.2 AMF projections for pelitic rocks -- 16.3 Progressive metamorphsim of pelitic rocks: barrovian metamorphsim -- 16.3.1 The protolith: the mineralogy of shale -- 16.3.2 Low-Grade metamorphsim of pelitic rocks -- 16.3.3 Barrovian metamophsim of pelitic schists -- 16.4 P-T Conditions for metamorphic assemblages in metapelitic rocks -- 16.4.1 Metapelitic assemblages and metamorphic facies -- 16.4.2 Pressure information from metapelitic rocks.
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|a 17.Metamorphism of calcareous roks and the role of fluids in metamorphsim -- 17.1 Introduction -- 17.2 Metamorphsim of impure dolomitic marble -- 17.2.1Stability of metamorphic assemblages in T-XSpace -- 17.2.2 Examples of how mineral assemblages can monitor fluid flow in aureoles -- 17.3 Buffering of Other Flid Components -- 17.4 Buffering of pH.
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|a 18. Regional occurrence and tectonic significance of metamorphic rocks -- 18. Introduction -- 18.2 Metamorphsim along convergent plate margins -- 18.2.1 Characteristics of Low-Temperature, highs pressure belts -- 18.2.3 Tectonic interpretation -- 18.3 Metamorphsim in continental collisions -- 18.3.1 Examples of continental collision -- 18.4 Metamorphsim in rifting terrains -- 18.5 Sea floor metamorphsim -- 18.6 Granulite terrains -- 18.7 Metamorphsim in archean terrains -- 18.7.1 Greenstone belts -- 18.7.2 Gneiss terrains -- 18.7.3 Tectonic interpretation of archean metamorphic belts.
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|a Rocas ígneas
|9 11634
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650 |
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|a Geología
|9 1052
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650 |
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|a Rocas metamórficas
|9 15465
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|a Petrología
|9 13605
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|a Frost, Carol D.
|9 16266
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