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Role of Fluids in Crustal Processes.

Detalles Bibliográficos
Clasificación:Libro Electrónico
Autor principal: Committee, Geophysics Study
Formato: Electrónico eBook
Idioma:Inglés
Publicado: Washington : National Academies Press, 1989.
Colección:Studies in geophysics The Role of fluids in crustal processes
Temas:
Acceso en línea:Texto completo

MARC

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245 1 0 |a Role of Fluids in Crustal Processes. 
260 |a Washington :  |b National Academies Press,  |c 1989. 
300 |a 1 online resource (183 pages) 
336 |a text  |b txt  |2 rdacontent 
337 |a computer  |b c  |2 rdamedia 
338 |a online resource  |b cr  |2 rdacarrier 
490 0 |a Studies in geophysics The Role of fluids in crustal processes 
588 0 |a Print version record. 
505 0 |a The Role of Fluids in Crustal Processes; Copyright; Studies in Geophysics; PREFACE; Contents; OVERVIEW AND RECOMMENDATIONS; SUMMARY; INTRODUCTION; CONSERVATION EQUATIONS; Physical Parameters; Mineral-Fluid Reactions; COUPLING; DISCUSSION: GEOLOGIC PHENOMENA; DRIVING FORCES; Topographic Relief; Tectonic Dilation and Compression; Diagenesis; Heat; Source of Fluids; RECOMMENDED RESEARCH; 1. Field Studies; 2. Fractured Rocks; 3. Permeability; 4. Low-Permeability Rocks; 5. Chemical Reactions; 6. Pore Fluids in Active Tectonic Areas; 7. Crustal Deformation; 8. Mathematical Analysis; References. 
505 8 |a BACKGROUND1 Mass and Energy Transport in an Deforming Earth's Crust ; INTRODUCTION; CONSERVATION EQUATIONS; Darcy's Law; Flow Equation; Dispersion-Diffusion-Advection; Heat Transport; Stress and Strain; Mineral-Fluid Reactions; COUPLING; DISCUSSION: GEOLOGIC PHENOMENA; HOW PERMEABLE IS THE CRUST?; MECHANISMS THAT CREATE HIGH PORE PRESSURE; Topographic Relief; Tectonic Dilation and Compression; Diagenesis; Geothermal Systems; Source of Fluids; SUMMARY; References; 2 Pore Fluid Pressure Near Magma Chambers ; INTRODUCTION; PRESSURE AT DEPTH; CHANGE IN FLUID PRESSURE; FLUIDS IN ROCKS. 
505 8 |a FAILURE CRITERIAVOLUME CHANGE CAUSED BY FAILURE; ENERGY REQUIRED FOR FRACTURE; ADVECTION AND PORE PRESSURE; SUMMARY; References; 3 Evolution and Style of Fracture Permeability in Intrusion-Centered Hydrothermal Systems ; ABSTRACT; INTRODUCTION; Geological Setting and Environments; NATURE OF SECONDARY POROSITY IN INTRUSION-CENTERED SYSTEMS; ROLE OF MAGMATIC PROCESSES IN FORMATION OF JOINTS; NATURE OF JOINTS AND FRACTURE SYSTEMS; Joint and Fracture Orientations; Alteration, Succession, and Distribution of Altered Fractures; SOURCE OF WATER; Fluid Inclusion Data; Data from Isotopes. 
505 8 |a NATURE AND EVOLUTION OF FRACTURE-RELATED PERMEABILITYSYNTHESIS; ACKNOWLEDGMENTS; References; 4 Fluid Dynamics During Progressive Regional Metamorphism ; INTRODUCTION; FLUID-ROCK RATIOS AND FLUID FLUX; FLUID FLOW AT MID-TO LOWER-CRUSTAL LEVELS; FLOW MECHANISM WHERE FLUID PRESSURE EQUALS LITHOSTATIC; CHANNELIZATION OF FLUID FLOW; ACKNOWLEDGMENTS; References; 5 Oxygen and Hydrogen Isotope Constraints On the Deep Circulation of Surface Waters Into Zones of Hydrothermal Metamorphism ... ; INTRODUCTION; OXYGEN ISOTOPE KINETICS IN THE QUARTZ-FELDSPAR SYSTEM. 
505 8 |a MAJOR FOSSIL METEORIC HYDROTHERMAL SYSTEMS OF WESTERN NORTH AMERICACordilleran Batholiths of Southern British Columbia; Meteoric Hydrothermal Effects of Eocene Magmatism, Southern Idaho Batholith; Miocene Meteoric Hydrothermal Systems, Western Cascade Range, Oregon; Other Localities; HYDROTHERMAL SYSTEMS ASSOCIATED WITH LAYERED GABBRO BODIES; Mineralogical Alteration Effects in 18O-Depleted Layered Gabbros; Contrasting Effects in Gabbros and Granites; LOW-18O BASALTIC AND RHYOLITIC MAGMAS; Low-18O Magmas Produced During Caldera Collapse, Yellowstone Volcanic Field. 
500 |a Low-18O Basaltic and Rhyolitic Magmas in Iceland. 
546 |a English. 
590 |a ProQuest Ebook Central  |b Ebook Central Academic Complete 
650 0 |a Fluid dynamics. 
650 2 |a Hydrodynamics 
650 6 |a Dynamique des fluides. 
650 7 |a Fluid dynamics  |2 fast 
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776 0 8 |i Print version:  |a Committee, Geophysics Study.  |t Role of Fluids in Crustal Processes.  |d Washington : National Academies Press, ©1989  |z 9780309040372 
856 4 0 |u https://ebookcentral.uam.elogim.com/lib/uam-ebooks/detail.action?docID=3377778  |z Texto completo 
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994 |a 92  |b IZTAP