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Laterite Soil Engineering

Laterite --- Soil mechanics --- Mécanique des sols --- Laterite. --- Soil mechanics. --- PEDOLOGIE --- PEDOGENESE --- SEDIMENTOLOGIE --- PETROLOGIE ROCHES SEDIMENTAIRES --- ROCHES TERRIGENES --- ALTERATION ATMOSPHERIQUE

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Basalt. --- Volcanism. --- Planets --- Planetary volcanism. --- Geology. --- 552.3 --- Basalt --- Planetary volcanism --- Volcanism --- Basaltic rocks --- Igneous rocks --- 552.3 Magmatic rocks. Igneous rocks --- Magmatic rocks. Igneous rocks --- Geology --- Planetary geology --- Volcanicity --- Vulcanism --- Astrogeology --- Geodynamics --- Volcanology --- DOMAINE EXTRA-TERRESTRE --- GEOLOGIE REGIONALE --- PETROLOGIE ROCHES IGNEES --- ROCHES IGNEES BASIQUES, ULTRA-BASIQUES --- PETROLOGIE ROCHES CRISTALLINES

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Continental Red Beds

Red beds. --- Issue --- Sedimentary rocks. --- Rocks, Sedimentary --- Rocks --- Beds, Red --- Red rock --- Redbeds --- Sedimentary rocks --- SEDIMENTOLOGIE --- DEPOTS MILIEUX MIXTES --- SEDIMENTOLOGIE DEPOTS CONTINENTAUX --- PETROLOGIE ROCHES SEDIMENTAIRES --- ROCHES FERRUGINEUSES ET MANGANESIFERES --- DIAGENESE ET METASOMATOSE --- GEOPHYSIQUE --- GEOMAGNETISME --- PALEOMAGNETISME

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Carbonate diagenesis is a subject of enormous complexity because of the basic chemical reactivity of carbonate minerals. These carbonate minerals react quickly with natural waters that either dissolve the carbonates, or precipitate new carbonates to bring the water into equilibrium with the host carbonate sediments and rocks. These rock-water interactions either create porosity by dissolution, or destroy porosity by the precipitation of carbonate cements into pore spaces. Carbonate Diagenesis and Porosity examines these important relationships in detail. This volume is published in co-ope

Carbonate rocks. --- Diagenesis. --- Porosity. --- Adsorption --- Osmosis --- Permeability --- Sedimentology --- Rocks, Carbonate --- Carbonates --- Sedimentary rocks --- GEOMORPHOLOGIE GENERALE --- KARST --- SEDIMENTOLOGIE --- PETROLOGIE ROCHES SEDIMENTAIRES --- ROCHES CARBONATEES --- ROCHES TERRIGENES --- MINERALOGIE DES MINERAUX, DES ROCHES --- EXTREME ORIENT --- ASIE --- GEOLOGIE REGIONALE --- DIAGENESE ET METASOMATOSE

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Petrochronology is a rapidly emerging branch of Earth science that links time (ages or rates) with specific rock-forming processes and their physical conditions. It is founded in petrology and geochemistry, which define a petrogenetic context or delimit a specific process, to which chronometric data are then linked. This combination informs Earth's petrogenetic processes better than petrology or geochronology alone. This volume and the accompanying short courses address three broad categories of inquiry.Conceptual approaches chaptersinclude petrologic modeling of multi-component chemical and mineralogic systems, and development of methods that include diffusive alteration of mineral chemistry.Methods chaptersaddress four main analytical techniques, specifically EPMA, LA-ICP-MS, SIMS and TIMS.Mineral-specific chaptersexplore applications to a wide range of minerals, including zircon (metamorphic, igneous, and detrital/Hadean), baddeleyite, REE minerals (monazite, allanite, xenotime and apatite), titanite, rutile, garnet, and major igneous minerals (olivine, plagioclase and pyroxenes). These applications mainly focus on metamorphic, igneous, or tectonic processes, but additionally elucidate fundamental transdisciplinary progress in addressing mechanisms of crystal growth, the chemical consequences of mineral growth kinetics, and how chemical transport and deformation affect chemically complex mineral composites. Most chapters further recommend areas of future research.

Petrology. --- Petroleum --- Geological time. --- Age of rocks --- Geochronology --- Geochrony --- Rocks --- Time, Geological --- Chronology --- Historical geology --- Sequence stratigraphy --- Petroleum geology --- Geology --- Lithology --- Petrography --- Physical geology --- Geology. --- Age --- Pétrologie. --- Géologie pétrolière. --- Géochronologie.