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Research > Chapter 20043
Solifluction boulder streams Babi lom ridge Brno
Solifluction covers Swiss National Park relationships post glacial landform evolution
Solifluction deposits late Wisconsinan Peoria Loess middle Missouri Valley, Iowa Nebraska
Solifluction deposits upper Holocene age summit Mont Saint-Pierre,ern Gaspesie
Solifluction forms theern slope Kohoutovska Highland city Brno
Solifluction forms, distribution climatic relationships; overview present-day conditions specific reference Swiss Alps tropical Andes
Solifluction Scotland
Solifluction dolomitic limestones, Sierra Nevada, Betic Cordillera
Solifluction inern Eurasia; review
Solifluction inern Finland; present
Solifluction Swedish mountains; distribution relationship vegetation snow cover
Solifluction mountains of Asia; distribution, morphology, processes
Solifluction layers indicators environmental history
Solifluction equator
Solifluction low-angled slopes inamptonshire
Solifluction phenomena periglacial denudation soil
Solifluction properties theeast part Tetenyi plateau
Solifluction rates Ruby Range, Yukon Territory; report
Solifluction resulting one-sided two-sided freezing; field data Svalbard
Solifluction shears Carsington, Derbyshire
Solifluction terraces in Wales
Solifluction Enschede
Solifluction constituent subaerial denudation
Solifluction-sliding phenomena Baikal area
Solifluction; constituent subaerial denudation
Solifluction; model trial
Solifluidized patterned ground distribution subnival altitudinal steps Braldo Biafo valleys, Karakoram
Solifluxao industrias paleoliticas
Solifluxion periglacially modified landforms Wellington, Novel Zealand
Solifluxion phenomena Hutt region
Solifluxion, congelifluxion similar slope processes
Soligorsk glaciodislocations (Byelorussia)
Solikamskaya svita, vazhnyi markiruyushchii gorizont Priuralya
Solimoes Basin
Solimoes Basin; oil potential exploration perspectives,ern Brazil
Solimoes megashear; intraplate tectonics inwestern Brazil
Solitario uplift, Presidio-Brewster counties, Texas
Solitary phaceloid rugose corals upper Givetian Cantabrian Mountains,western Spain
Solitary coral growth forms distribution patterns index sediment-accumulation rates
Solitary corals (Zoantharia, Microsolenina) Cretaceous Bohemia, upper Cenomanian, Czech Republic
Solitary geological structures
Solitary rugose corals algae Upper Carboniferous Oklahoma, U.S.A
Solitary rugose corals algae upper Carboniferous Oklahoma, U.S.A
Solitary rugose corals Upper Permian theern Russian Platform
Solitary streptelasmatid corals, Ordovician ofern Hudson Bay Lowland, Manitoba, Canada
Solitary wave Burridge-Knopoff model slip-dependent friction clue understanding mechanism self-healing slip pulse earthquake rupture process
Solitary wave model magma ascent viscous, deformable cylindrical conduit
Solitary wave propagation fluid conduit viscous matrix
Solitary waves instabilities laboratory conduits
Solitary waves agents primary hydrocarbon transport Gulf Mexico Basin
Solitary waves crustal fault
Solitary waves viscosity buoyant upwellings
Solitary waves magmatic systems
Solitary waves mantle plumes
Solitary waves Earth
Solitary waves crustal fault
Solitary waves Bingham-plastic seabed
Solitary waves, sediment transport, large-scale mudbanks theeastern coast of America
Soliton properties seismic waves single single-row explosions
Soliton properties teleseismic waves
Soliton resonances improved Boussinesq equation
Solitons, mantle shear, segmentation plume tails; plume dynamics Snake River plain, Idaho
Solitudinella hollardi n. gen., n. sp. (Brachiopoda, Lissatrypidae) Pragian pre-Saharan Morocco
Sollenella? sp.; isochilinid ostracode specimens freshwater back-swamp fluvial facies (upper Middle Devonian), Catskill Mountains, Novel York
Solling-Platten
Sollingen excursion; stock seasonal soil mechanisms beech fir ecosystems Podsols Bunter assessment organic waste
Solnhofen 5 Villafranchian fissure filling Bavaria
Solnhofen Bavaria
Solnhofen; Plattenkalk preservation Archaeopteryx
Solnhofen; glance earth history; book review
Solnhofen; page
Solnhofen; book review
Solo Valley science 1975 Java, Indonesia
Soloing Mauna Loa
Solomons alluvial gold
Solomons, SW Pacific
Solomons, Santa Cruz, Rennell, Solomon, Malaita-Uki, Choiseul Solomons basins
Solomons; mineral occurrences guide additional exploration
Solomon Markovich Tilman (1919-1994)
Solomon Markovich Tilman; 70th birthday
Solomon Microplate rotation transpressional convergent zone, SW Pacific
Solomon R. Dresser (1842-1911)
Solomon Sea formation seismic reflection data
Solomon's volcanoes; life verge
Solonets formations
Solongo Deposit exotic boron ores Buryatia
Solonskaya Series Eocene ofernern Caucasus
Soloviejo manganese deposit; mineralogy geochemistry, development report
Sols de touyas alluvial deposits Pyrenean gaves; Veracrisols, integration Referentiel Pedologique
Sols des regions mediterraneennes de lAfrique (du Tell)
Sols argiles noirs tropicaux subtropicaux dAfrique; tropical subtropical black soils clays Africa
Sols terroirs du pays de Cognac (Charente)
Sols geometriques actuels en Velay
Sols polygonaux dans la Puna bolivienne
Sols polygonaux terrasses marines du Spitzberg
Sols polygonaux sur le Causse Mejean
Sols stries eboulis ordonnes; stone stripes bedded screes
Sols stries polygonaux periglaciaires
Solubilidad de los compuestos ionicos en relacion con su cristaloquimica; I, Relacion entre los radios ionicos los coeficientes de solubilidad de los halogenuros alcalinos en agua acetona
Solubilisation influence spent wash oxide-ores manganese iron
Solubilisation par les eaux naturelles de larsenic lie au fer dans les roches sedimentaires
Solubilite du quartz, dans des solutions de sels alcalins, sous pression au-dessus de la temperature critique
Solubilite du radon dans leau desequilibre
Solubilities partitioning noble gases mineral-melt systems; I, Synthesis reversal experiments Ar anorthite coexisting melt
Solubilities partitioning noble gases mineral-melt systems; II, Synthesis experiments Ne, Ar, Kr, Xe anorthite, diopside, forsterite, coexisting melts
Solubilities partitioning noble gases mineral/ melt systems; results Ne, Ar, Kr, Xe anorthite, diopside, forsterite coexisting melt implications terrestrial planet atmospheric evolution
Solubilities thermodynamic properties MnCl (sub 2) degrees scheme MnSiO (sub 3) -SiO (sub 2) -HCl-H (sub 2) O
Solubilities transport ore minerals, 8
Solubilities calcite-dolomite-gypsum scheme implications karst hydrology
Solubilities scheme Al<2) O<3) -SiO<2) -H<2) O
Solubilities Fe-S-O minerals NaCl-bearing aqueous solutions 250 degrees 350 degrees C
Solubilities O Si liquid iron balance (Mg,Fe)SiO (sub 3) perovskite light elements core
Solubilities Pt, Ir, Pd silicate melts high pressures
Solubilities PtS, PdS Au aqueous sulfide solutions temperatures 200 degrees -350 degrees C
Solubilities actinide solids oxic conditions
Solubilities aluminum hydroxides oxyhydroxides alkaline solutions; correlation thermodynamic properties Al(OH) (sub 4) (super -)
Solubilities calcite dolomite hydrothermal solutions
Solubilities calcium magnesium sulfates carbonates high temperature water systems
Solubilities calcium silicates high pressures temperatures
Solubilities carbon dioxide water rhyolitic melts
Solubilities carbon dioxide natural andesite, tholeiite olivine nepheline melilitite melts 30 kbar pressure
Solubilities danburite datolite aqueous solutions 25 degrees 250 degrees C
Solubilities heavy-metal sulfides deposition hydrothermal solutions
Solubilities highly siderophile elements silicate melts; experimental results geochemical implications
Solubilities metallic sulfides quartz hydrothermal sulfide solutions
Solubilities natural synthetic ferrimolybdite
Solubilities nickel cobalt silicate melts presence graphite (CO,CO (sub 2) ) fluid 1350-1400 degrees C 7-15 kbar
Solubilities nitrogen noble gases basalt melt
Solubilities noble gases magnetite; implications planetary gases meteorites
Solubilities ore minerals.; 2
Solubilities pyrite marcasite NaCl-S degrees -H (sub 2) O scheme
Solubilities quartz, corundum, gold aqueous chloride hydroxide solutions
Solubilities calcium minerals prepared calcium compounds EDTA (ethylene diamine tetraacetic acid) solutions
Solubilities oxides ions dilute aqueous solutions calculated thermodynamic basis significance ore deposits
Solubilities stibnite, orpiment realgar borate, carbonate hydroxide solutions functions temperature pressure implications applied borax deposit Boron, California
Solubilities sulfur, noble gases, nitrogen, chlorine, fluorine magmas
Solubilities sylvite three-phase curve binary scheme KCl-H (sub 2úO
Solubilities synthetic schwertmannite ferrihydrite
Solubilities tungsten cobalt silicate melts role melt composition
Solubilities water carbon dioxide basaltic magmas
Solubilities water basaltic melt influence degree oxygen fugacity crystallization water-saturated basaltic melt
Solubility Constants System MgO-SiO (sub 2) -H (sub 2) O-HCl
Solubility Raman spectroscopic investigations speciation tungsten molybdenum hydrothermal solutions
Solubility Solubility Product Gypsum Soil Solutions Other Aqueous Solutions
Solubility and accumulation of metals in Chinese brake fern, vetiver and rostrate sesbania using chelating agents
Solubility availability sorbed sulfate hawaiian soils
Solubility behavior lead green orthoclase (amazonite) Broken Hill, New Wales, Australia
Solubility behaviour sulphur hexafluoride water 250 degrees C; implications geothermal tracer
Solubility capacity form aggregates humic substances humates
Solubility cation exchange properties zeolite-apatite mix balance water
Solubility complexing scheme zirconium hydroxide-fulvic acids-water relationship zirconium migration natural waters
Solubility complexing nickel supercritical aqueous chloride solutions
Solubility composition magnesium hydroxy sulfate
Solubility crystal growth ZnAl (sub 2) O (sub 4) Al (sub 2) O (sub 3) molten PbF (sub 2) solutions
Solubility crystallization silica chloride solutions
Solubility crystallization yttrium-iron garnet melts
Solubility deposit conditions lead zinc sulphides hydrothermal solutions alkalies carbonates halides
Solubility diffusion helium amorphous diopside anorthite; measurements glass transition
Solubility diffusion rare gases silicate melts
Solubility diffusion water silicate minerals
Solubility diffusional absorption hydrogen quartz high water pressures; implications hydrolytic weakening
Solubility diffusivity noble gases synthetic phlogopite; UVLAMP investigation
Solubility dissolution behavior monazite LREE diffusion hydrous granitic melt
Solubility dissolution kinetics albite pH-bufffered solutions acetate, oxalate, citrate, BTCA; experimental study 100 degrees C, 13.8 MPa
Solubility dissolution kinetics dolomite Ca-Mg-HCO (sub 3) / CO (sub 3) solutions 25 degrees C 0.1 MPa carbon dioxide
Solubility electrokinetic properties bassetite
Solubility forms incidence copper aluminosilicate melts
Solubility forms incidence silica normal dilute solutions
Solubility geochemistry phosphorus magmas
Solubility growth quartz crystals phosphate solution
Solubility interphase fractionation hydrolysis products density fluids
Solubility mobility petroleum hydrodynamic conditions, Surat Basin, Queensland
Solubility monocrystalline growth phlogopite mica sodic hydrothermal solutions
Solubility numerical simulation dynamics heavy metals polluted soil; case study
Solubility incidence lead surface water
Solubility partitioning uranium uranium oxide-haplogranite-H (sub 2) O-NaCl(NaF) scheme 780 degrees C, 2 kbar, controlled fO (sub 2)
Solubility partitioning water synthetic forsterite enstatite scheme MgO-SiO (sub 2) -H (sub 2) O+ -Al (sub 2) O (sub 3)
Solubility polymerization silica salt solutions
Solubility potentiometric investigations REE complexation simple carboxylate (acetate, oxalate) ligands 25 degrees 80 degrees C
Solubility rate solution calcium carbonate
Solubility response kinetics solution-solid reactions determined situ notes
Solubility response rates aluminum solid phases hydrothermal conditions
Solubility soil mobility polychlorinated biphenyls
Solubility solution capacity compressed gases oil gas condensate systems
Solubility sorption protactinium near-field far-field environments radioactive waste repository
Solubility speciation C-O-H fluids andesitic melt T = 1100-1300 degrees C P = 200 500 MPa
Solubility speciation ZrO (sub 2) acid hydrothermal solution; experimental advance
Solubility speciation sulphur role fO (sub 2) fS (sub 2) silicic melts; thermodynamic model
Solubility speciation water clinopyroxene; (super 1) H MAS NMR data
Solubility speciation zinc Calcareous soils
Solubility spectrochemical characteristics synthetic chernikovite meta-ankoleite
Solubility stability hydrogen diopside single crystals
Solubility stability magnesium phosphates sea water
Solubility stability scorodite, FeAsO (sub 4) .2H (sub 2) O; data additional discussion
Solubility stability scorodite, FeAsO (sub 4ú.2H (sub 2úO; discussions replies
Solubility surface adsorption characteristics metal oxides high temperature
Solubility thermodynamic constants dissolution zeolites 4A 13X basic aqueous solutions
Solubility thermodynamic properties NaCl water vapor T = 300-500 degrees C P< =300 bar
Solubility transport saline geothermal system; natural analog study
Solubility transport arsenic coal ash
Solubility transport plantinum-group elements Au saline hydrothermal fluids; constraints geothermal brine data
Solubility transport platinum-group elements hydrothermal solutions; thermodynamic physical chemical constraints
Solubility valency uranium model granitic melts
Solubility calculations concentrated brine model; sea water scheme
Solubility characteristics Ag base-metals sulphide assemblages Ingaldhal, Karnataka, India; experimental study
Solubility constants rock-forming minerals
Solubility constraint; important consideration safety evaluation nuclear waste disposal
Solubility controlled mineral zonation efflorescences crusts building walls
Solubility controls transformation mechanisms silica diagenesis
Solubility controls carbonate fluorapatite seawater
Solubility controls fluorine, barium chromium ground water alluvial basins Arizona
Solubility controls determine dissolved organic matter composition surface- ground-waters
Solubility curves calcite water presence carbon dioxide
Solubility diagrams explaining zone sequences bauxite, kaolin pyrophyllite-diaspore deposits
Solubility increased pressure density phases stability SiO (sub 2) modifications
Solubility equation characteristic petroleum stratified pools
Solubility equilibria multicomponent oceanic salt systems = 0 200 degrees C; model parameterization databases
Solubility balance constant strengite
Solubility experiments diamond anvil cell; NaCl-H (sub 2) O 2 GPa 300 degrees C
Solubility implications apatite sea water
Solubility aqua regia selected chemical elements occurring fine fraction
Solubility Quaternary scheme (Rb (super +) , Mg (super +2) ) SO (sub 4) (super 2?) -Cl (super?) -H (sub 2) O 35 degrees C
Solubility isotherms scheme CaO--B (sub 2) O (sub 3) --MgCl (sub 2) -H (sub 2) O 70 degrees C
Solubility limit gold arsenian pyrite carlin-type epithermal deposits; EMPA, SIMS, HRTEM quantum-mechanical constraints
Solubility measurements scheme CaSO (sub 4) -NaCl-H (sub 2) O 35 degrees , 50 degrees , 70 degrees C atmosphere pressure
Solubility measurements neptunium-incorporated soddyite
Solubility measurements phases illites
Solubility measurements sphalerite
Solubility mechanism water hydrogen albite melt (1200 degrees C, 2 kbar)
Solubility mechanisms H (sub 2) O Ca-aluminosilicate melts high pressure
Solubility mechanisms H (sub 2) O silicate melts high pressures temperatures; Raman spectroscopic study
Solubility mechanisms H (sub 2) O silicate melts high pressures temperatures; Raman spectroscopic study; discussion reply
Solubility mechanisms carbon dioxide silicate melts; Raman spectroscopic study
Solubility mechanisms fluorine NaAlO (sub 2ú-SiO (sub 2ú-F, SiO (sub 2ú-AlF (sub 3ú SiO (sub 2ú-NaF melts 1 atm
Solubility mechanisms fluorine silicate liquids; scheme CaO-CaF (sub 2) -SiO (sub 2)
Solubility mechanisms volatiles silicate melts
Solubility mechanisms water hydrogen magmatic model aluminosilicate melts acidic ultrabasic compositions
Solubility mechanisms water basalt melt high pressures temperatures; NaCaAlSi (sub 2) O (sub 7) -H (sub 2) O model
Solubility mechanisms water silicate melts high pressure temperature
Solubility modeling lead, copper, zinc potable water systems
Solubility (OH) quartz
Solubility 4A 13X zeolites basic aqueous solutions; I, Kinetic study
Solubility 4A 13X zeolites basic aqueous solutions; thermodynamic constants dissolution
Solubility A1 (sub 2) O (sub 3) Enstatite Spinel Garnet Peridotite Compositions
Solubility Added Phosphates Phosphate Saturated Soil
Solubility AgCl NaCl-bearing solutions 250 degrees C 400 degrees C diverse pressure
Solubility Al (sub 2) O (sub 3) Orthopyroxene Coexisting Garnet Clinopyroxene Compositions Diopside-Pyrope Join System CaSiO (sub 3) -MgSiO (sub 3) -Al (sub 2) O (sub 3)
Solubility Al (sub 2) O (sub 3) enstatite coexisting forsterite spinel
Solubility Al (sub 2) O (sub 3) orthopyroxene equilibrated almandine scheme FeO-Al (sub 2) O (sub 3) -SiO (sub 2)
Solubility Au-Ag alloys hydrothermal brines
Solubility C-O-H mixtures natural melts; experimental data function range models
Solubility CO (sub 2) Di-CO (sub 2) AB-CO (sub 2) -H (sub 2) O-Xe liquids high P T
Solubility CO (sub 2) Ca-rich leutite; effects pressure, temperature, oxygen fugacity
Solubility CO (sub 2) aqueous NaCl solutions
Solubility CO (sub 2) aqueous solutions electrolytes (problems salting out)
Solubility CO (sub 2) chloride solutions elevated temperatures CO (sub 2) pressures
Solubility CO (sub 2) haplokimberlite liquids high pressures join Ca (sub 2) SiO (sub 4) -Mg (sub 2) SiO (sub 4) -CO (sub 2)
Solubility CO (sub 2) kimberlitic carbonatitic melts
Solubility CO (sub 2) magmatic melts high temperatures pressures
Solubility CO (sub 2) melts acid composition case albite-silica scheme (65-35)
Solubility CO (sub 2) olivine melilitite high pressures function CO (sub 2) Earth's upper mantle
Solubility CO (sub 2) scheme Na (sub 2) O-Al (sub 2) O (sub 3) -SiO (sub 2) -H (sub 2) O-CO (sub 2) 30 kbar
Solubility Ca Al orthopyroxene spinel peridotite; good version empirical geothermometer
Solubility CaAl (sub 2) SiO (sub 6) CaScAlSiO (sub 6) -pyroxene
Solubility CaMgSi (sub 3) O (sub 8) ?Si (sub 4) O (sub 8) endmembers anorthite
Solubility Cr, Ti, Al co-existing olivine, spinel, liquid 1 atm
Solubility H (sub 2) O CO (sub 2) granite basalt melts high pressures
Solubility H (sub 2) O forsterite melt 20 kbar
Solubility H (sub 2) O nominally anhydrous mantle minerals (super 1) H MAS NMR
Solubility H (sub 2) O rhyolitic melts pressures
Solubility H (sub 2) O silicate melts; theoretical discussion
Solubility Hydrous Ferric Oxide Sea Water
Solubility K Fe-S liquid, planetary implications
Solubility K metal; results effects C, pressure, temperature
Solubility K metal; results effects pressure composition
Solubility Minerals High Water Pressures
Solubility MnO (sub 2) forms manganese incidence aqueous solutions
Solubility NdPO (sub 4) H (sub 2) O-NaCl-HCl fluids
Solubility Ni degrees silicate melts implications metal/ melt crystal/ melt partitioning
Solubility PbS concentrated NaCl solutions elevated temperatures
Solubility Petroleum Water Its Significance Petroleum Migration
Solubility Pt Pd Dio-An melts; methodology effects fO (sub 2) addition iron
Solubility Pt Pd sulfides Au metal aqueous bisulfide solutions; II, Results 200 degrees C 350 degrees C saturated vapor pressure
Solubility Pt, Pd sulfides Au aqueous bisulfide solutions 350 degrees C
Solubility Quartz H (sub 2) O-CO (sub 2) Fluids 5 kb. 500 degrees -900 degrees C
Solubility REE phosphate minerals stability constants REE chloride complexes hydrothermal solutions
Solubility Ra radioactive repository environment
Solubility Ru Pd silicate melts; influence melt composition
Solubility Silica Soils
Solubility SnO (sub 2) water aqueous solutions HCl, HCl+KCl, HNO (sub 3) 200-400 degrees C 101.3 MPa
Solubility SnO (sub 2) water, water solutions HCl, HCl+KCl, HNO (sub 3) 200 400 degrees C 101.3 MPa
Solubility Sodalite Aqueous Solutions NaOH Hydrothermal Conditions
Solubility Sulfur Mafic Magmas
Solubility Ta (sub 2) O (sub 5) silicate liquids
Solubility Ti andradite upper mantle conditions; results
Solubility TiO (sub 2) garnet orthopyroxene; Ti thermometer ultrahigh-temperature granulites
Solubility UO (sub 2) aqueous solution high temperature high pressure
Solubility Y-zeolite analcime aqueous basic solutions; thermodynamic dissolution values
Solubility multiphase sulfide scheme hydrothermal chlorine solutions
Solubility accessory minerals aqueous fluids 1.0-2.8 GPa 1000-1200 degrees C
Solubility acid alkaline gases electrolyte solution mixtures
Solubility albite hydrothermal solutions
Solubility albite+microcline+andalusite+quartz supercritical, chloride-rich aqueous solutions
Solubility alumina orthopyroxene spinel geobarometer complex systems; functions spinel-bearing alpine-type peridotites
Solubility aluminum iron ground water Globe, Arizona
Solubility aluminum hydroxide sea water
Solubility aluminum orthopyroxene; global inversion experimental data scheme MgO-Al (sub 2) O (sub 3) -SiO (sub 2)
Solubility uranium amorphous phase geochemical conditions representative direct disposal spent nuclear fuel Boom Clay
Solubility andalusite kyanite 420-500 degrees C 1300 bars thermodynamic constants minerals
Solubility anhydrite aqueous NaCl solutions elevated temperatures pressures
Solubility anhydrite water 100 degrees C. 275 degrees C. 1 bar 1000 bars
Solubility anhydrite, CaSO (sub 4) NaCl-H (sub 2) O solutions high pressures temperatures; functions fluid-rock interaction
Solubility apatite clay bearing systems; function agriculture
Solubility apatite iron-silicate liquids
Solubility apatite, monazite, zircon, rutile supercritical aqueous fluids implications subduction zone geochemistry
Solubility argon H (sub 2) O silicate melts high pressure temperature
Solubility argon silicate liquids high pressures
Solubility atrazine calcic montmorillonite gels
Solubility bayerite low-temperature acid environment thermodynamic properties Al (super 3+) ion 25 degrees C
Solubility beryl kaolinite 300 degrees C
Solubility beryl haplogranite melts
Solubility boehmite speciation aluminium hydrothermal solutions; complexation OH, CH (sub 3) , COO (super -) Na (super +) ligands
Solubility cadmium cobalt post-oxic sub-oxic sediment suspension
Solubility cadmium mercury oxides NaCl solutions comparatively high carbon dioxide partial pressures
Solubility cadmium polluted soil
Solubility calcite CO (sub 2) ; (sub 2) O 200 degrees 300 degrees C 500 1000 bars, role CO (sub 2) concentration
Solubility calcite NaCl solutions 50 degrees 200 degrees C
Solubility calcite diverse electrolytes temperatures 10 60 degrees C CO (sub 2) partial pressures 10 (super 3) Pascals
Solubility calcite high temperature aqueous solutions alkali carbonates problem structure carbonatites
Solubility calcite homogeneous H (sub 2) O-NaCl-CO (sub 2) systems temperatures 200-600 degrees
Solubility calcite mixed aqueous solutions NaCl KCl 25 degrees C CO (sub 2) partial pressures 1 kPa
Solubility calcite water 100 degrees C. 200 degrees C. Geol. Soc. America Bull., v. 70, no. 12, pt. 2
Solubility calcium carbonate precipitated montmorillonite suspensions
Solubility calcium phosphates sea water
Solubility calcium sulfate (gypsum)
Solubility calcium sulfate relationship temperature, carbon dioxide pressure presence calcium carbonate
Solubility carbon hydrogen simplified basaltic melts 2.8 GPa fO (sub 2) implications
Solubility carbon dioxide albitic melt
Solubility carbon dioxide aluminosilicate melts enhanced alkalinity, origin carbonatite magmas
Solubility carbon dioxide concentrated chloride solutions high temperatures pressures
Solubility carbon dioxide high alkaline aluminosilicate melts problems carbonatite magma genesis
Solubility carbon dioxide melts andesite, tholeiite, olivine nephelinite composition 30 kbar pressure
Solubility carbon dioxide molten albite
Solubility carbon dioxide water geothermal conditions
Solubility carbonate rocks exploration indicators ore-bearing karst
Solubility carbonates sea water; control carbonate complexes
Solubility cassiterite tin deposition theeast Asian tin belt
Solubility cassiterite silic chloride solutions 300 degrees 400 degrees
Solubility cassiterite silica-hydrochloric acid solutions 300 400 degrees C
Solubility cassiterite solvent HF methods transport tin ores subcritical fluids
Solubility cassiterite water NaOH solutions increased temperatures
Solubility cassiterite water aqueous NaOH solutions elevated temperatures
Solubility celestite (SrSO (sub 4) ) H (sub 2) O 50 degrees 250 degrees C 100 1500 bars
Solubility chlorargyrite AgCl (sub cr.) density aqueous fluid 400-425 degrees C 50-1000 bar
Solubility chlorine aluminosilicate melts
Solubility chromium oxygen metallic liquids co-crystallization chromite metal iron meteorite parent bodies
Solubility cinnabar (alpha -HgS) hydrosulfide solutions high temperatures
Solubility cinnabar Na (sub 2) S solutions 50-250 degrees C 1-1,800 bars, geologic functions
Solubility cinnabar synthetic ore solutions
Solubility co-existing pyrite pyrrhotite scheme NaHS-H (sub 2) S-NaCl-H (sub 2) O elevated temperature pressure
Solubility coal macerals
Solubility colemanite mineral CO (sub 2) -containing water geological structure mineral
Solubility colloidal ferric hydroxide
Solubility copper gold magmatic-epithermal systems
Solubility copper natural waters function geochemical prospecting
Solubility copper sulfur-free mafic melts
Solubility copper sulfides sulfide solutions
Solubility of core materials in aqueous polymeric solution effect on microencapsulation of curcumin
Solubility corundum + kyanite H (sub 2) O 700 degrees C 10 kbar; proof Al-Si complexing high pressure temperature
Solubility corundum H (super 2) 0 350 600 degrees C 0.5 2.2 kbar
Solubility corundum supercritical 0.1 molal CaCl (sub 2)
Solubility corundum water elevated temperatures pressures
Solubility corundum water temperatures 500-800 degrees C pressure 6 kbar
Solubility corundum+kyanite H2O 700C, 1 1.5 GPa; proof high Al mobility deep metasomatic environments
Solubility covellite synthetic ore solutions
Solubility crude oil methane role temperature pressure
Solubility cryolite 25 degrees C 1 atmosphere pressure
Solubility crystalline neodymium hydroxide hydrolysis trivalent Nd ion 30 degrees 290 degrees C
Solubility dimagnesium phosphate trihydrate trimagnesium phosphate
Solubility dolomite estimated basis chemical composition Florida ground waters
Solubility of ettringite (Ca (sub 6) (sub 2) (SO (sub 4) ) (sub 3) .26H (sub 2) O) at 5-75 degrees C
Solubility excess alumina hydrous granitic melts balance peraluminous minerals 700-800 degrees C 200 MPa, functions aluminum saturation index
Solubility fine-dispersed gold hydrothermal solutions high temperatures pressures, experimental investigations
Solubility fluoride semi-arid environments
Solubility fluorite complexing scheme CaF (sub 2) -NaCl-HCl-H (sub 2) O
Solubility fluorite aqueous sodium chloride solutions 150-500 degrees C
Solubility fluorite aqueous solutions NH (sub 4) Cl hydrothermal conditions
Solubility fluorite haplogranitic melt variable alkalis alumina content 800 degrees -1000 degrees C 100 MPa
Solubility fluorite supercritical aqueous fluid
Solubility fluorite supercritical water solutions NaCl CaCl (sub 2)
Solubility fluorspar CaF (sub 2) NaCl HCl solutions hydrothermal conditions
Solubility foraminifera seawater high pressures
Solubility fullerenes C (sub 60) C (sub 70) water
Solubility galena aqueous solution NH (sub 4) Cl hydrothermal conditions
Solubility galena chloride solutions high concentrations CO (sub 2) H (sub 2) S
Solubility galena sulfur-rich NaCl solutions
Solubility gallium sphalerite wurtzite 800 degrees C 900 degrees C
Solubility gases formation solutions
Solubility gases fluids geothermal conditions; estimation methods calculations
Solubility gelatinous silica 25 degrees C
Solubility gibbsite speciation aluminum H-Na-K-Cl-OH-acetate brines 6-125 degrees C 0-5 molal ionic strength
Solubility gibbsite speciation aluminum H-Na-K-Cl-OH-acetate brines range 6-125 degrees C 0-5 molal ionic strength
Solubility gibbsite NaCl-NaOH NaCl-HCl brines 6.4 80.0 degrees C ionic strengths 0.001 5.0m
Solubility gold silver fluids greenstone belt deposits
Solubility gold silver oxygen-saturated fluids structure high fineness gold grains lateritic profile
Solubility gold H (sub 2) S NaCl bearing aqueous solutions 250 degrees 350 degrees C
Solubility gold KCl (0.5m) solution hydrothermal conditions (350-500 degrees C, 500 bar)
Solubility gold aqueous chloride fluids 350-500 degrees C, 500-1500 atm pressure thermodynamic properties AuCl (super -) (sub 2(sol)) 750 degrees C 5000 atm
Solubility gold arseno-sulfidic solutions 200 300 degrees C
Solubility gold hydrothermal alkaline sulfide solutions
Solubility gold hydrothermal chloride solutions
Solubility gold pore water auriferous laterites Misseni, Mali
Solubility gold sulfide-arsenide solutions 200-300 degrees C
Solubility gold sulfur-containing solutions
Solubility gold sulfuric solutions
Solubility gold SiO (sub 2) -NaCl-H (sub 2) O scheme 300 degrees C 50 MPa
Solubility gold granitic melts; influences temperature, pressure, time
Solubility gold water high temperature genesis gold deposits
Solubility gold inorganic supergene conditions
Solubility graphite Fe-Ni melt
Solubility gypsum anhydrite water solutions CaCl (sub 2) temperature 25 50 degrees C
Solubility gypsum aqueous electrolytes affected ion association ionic strengths 0.15m 25degc
Solubility heavy metals contaminated soil; effects redox potential pH
Solubility heavy metals relationship geological context; theoretical advance
Solubility hematite chloride-bearing hydrothermal fluids
Solubility high soluble salts aqueous media; Part 1, NaCl, KCl, CaCl<2) , Na<2) SO<4) , K<2) SO<4) solubilities 100 degrees C
Solubility higher molecular volume n-paraffins distilled water sea water
Solubility hydrocarbons conditions bitumen deposition hydrothermal processes
Solubility hydrocarbons water stratified media
Solubility hydrocarbons water stratal conditions
Solubility hydrogen aluminum CaSiO (sub 3) -perovskite partitioning water silicates mantle
Solubility hydrogen ferric iron rutile TiO (sub 2) ; (II), Implications phase assemblages ultrahigh-pressure metamorphism stability silica polymorphs mantle
Solubility hydrogen diopside pressures 2.0 GPa
Solubility hydrogen olivine; dependence temperature iron content
Solubility hydrothermal kaolinite range 60-200 degrees C pH 6-9
Solubility hydroxostannate complexes cassiterite crystallization hydrothermal conditions
Solubility hydroxyl natural quartz annealed water 900 degrees C 1.5 GPa
Solubility hydroxyl pyrope garnet; infrared spectroscopic study
Solubility inverse problem gravity exploration trial-and-error technique
Solubility iron carbonate temperatures 25 degrees 70 degrees 1 atm total pressure
Solubility iron plagioclase, clinopyroxene silicate liquid scheme CaO-MgO-Al (sub 2úO (sub 3ú-SiO (sub 2ú-Fe-O
Solubility iron Fe-O-H-S fluids
Solubility iron TiO (sub 2) (rutile)
Solubility iron concretions extracts
Solubility iron oxides forest soils Tamm reagent
Solubility iron sulfides
Solubility ironand aluminum phosphates aqueous solutions
Solubility jadeite water 20 30 kbars
Solubility jadeite+quartzite H (sub 2) O 12-20 kbar, 400-600 degrees C
Solubility jarosite solid solutions precipitated acid waters, Iron Mountain, California, USA
Solubility kaolinite alkaline solutions hydrothermal conditions
Solubility kyanite, corundum, quartz amorphous silica aqueous hydrochloric acid solutions 285 degrees C 450 bars
Solubility kyanite, corundum, quartz, amorphous silica chloride water solutions 285 degrees C 450 bars
Solubility lignitic macerals anthracene oil presence hydrogen carbon monoxide
Solubility limestone
Solubility lithium, nickel, magnesium ferrites PbO-B (sub 2) O (sub 3)
Solubility albite NaCl solutions 250 degrees ) C
Solubility magnesite CO (sub 2) -H (sub 2) O 150 degrees , 200 degrees , 250 degrees C 100, 500, 1000 bars
Solubility magnetite supercritical HCl NaCl solutions
Solubility magnetite supercritical chloride solutions
Solubility major trace elements mantle metasomatic fluids; experimental constraints
Solubility major structures carbonate reservoir rocks foothills Caucasus mountains
Solubility malachite scheme Na(K)HCO (sub 3) -H (sub 2) O-CO (sub 2) NaCl-H (sub 2) O-CO (sub 2) hydrothermal conditions
Solubility mangocolumbite mangotantalite peraluminous peralkaline granitic melts 800 degrees C 2kbar
Solubility metakaolinite kaolinite acid environment
Solubility metal compounds generally concentrated hydrothermal processes
Solubility metal oxides carbon-dioxide chloride solutions comparatively high carbon-dioxide pressures
Solubility metal oxides 250 degrees C situ pH monitoring
Solubility metal sulphides dilute vein forming solutions
Solubility metals nutrients brines; implications ore deposits, bioproductivity, anoxia sedimentary basins
Solubility methane water elevated temperatures pressures
Solubility microcline, muscovite quartz speciation Al supercritical H (sub 2) O
Solubility minerals forms lead existence seawater
Solubility minerals pure water Grime's Grave mines, England
Solubility mixed H-O-Cl-S fluids silicate melts; influence fluid composition
Solubility molybdenite (MoS (sub 2) ) hydrothermal solutions
Solubility molybdenum oxide granite melts
Solubility natural fluorite 25 degrees C
Solubility natural gases aqueous salt solutions, Part 2, Nitrogen aqueous NaCl, CaCl (sub 2) , Na (sub 2) SO (sub 4) MgSO (sub 4) room temperatures pressures 1000 psia
Solubility natural gases aqueous salt solutions; 3, Nitrogen aqueous NaCl high temperatures
Solubility natural gases aqueous salt solutions; Part 1, Liquidus surfaces scheme CH (sub 4) -H (sub 2) O-NaCl (sub 2) -CaCl (sub 2) room temperatures pressures 1,000 psia
Solubility neutral nickel silicate melts implications Earth's siderophile element budget
Solubility nickel diverse minerals
Solubility niobium scheme CaCO (sub 3) -Ca(OH) (sub 2) -NaNbO (sub 3) 0.1 GPa pressure
Solubility niobium scheme CaCO (sub 3) -CaF (sub 2) -NaNbO (sub 3) 0.1 GPa pressure; implications crystallization pyrochlore carbonatite magma
Solubility nitrogen noble gases silicate melt
Solubility nitrogen aqueous NaCl temperatures 125 degrees C pressures 9000 psi
Solubility nitrogen aqueous salt solutions pressures 1,000 PSIA
Solubility nitrogen magmatic melts; problem redox regime Earth's upper mantle
Solubility nitrogen melts CaO-MgO-Al (sub 2) O (sub 3) -SiO (sub 2) scheme
Solubility noble gases nitrogen silicate melts 5000 bars
Solubility noble gases basalt melt; results 1300 degrees C, 1 bar
Solubility noble gases fresh water NaCl brines
Solubility ore minerals complexation ore metals hydrothermal solutions
Solubility orpiment Na (sub 2) S-H (sub 2) O solutions 25 degrees C 200 degrees C 100 bars 1500 bars pressure
Solubility oxygen liquid iron high pressure consequences early differentiation Earth Mars
Solubility petroleum forming hydrocarbons aqueous solutions applied primary petroleum migration
Solubility petroleum oil-field waters role oxidation condition scheme
Solubility petroleum water significance petroleum migration
Solubility petroleum water role temperature salinity significance primary petroleum migration
Solubility platinum aqueous fluids buffered manganese oxides
Solubility platinum-group elements late-stage magmatic/ hydrothermal solutions
Solubility potassium phosphorous Ca-silicates 2 13 GPa
Solubility potassium muscovite microbial effect
Solubility powellite CaMoO (sub 4) aqueous NaCl 50-300 degrees C
Solubility pyrrhotite, galena sphalerite aqueous solutions NH (sub 4) Cl+NaCl high temperatures pressures
Solubility quartz H (sub 2) O-CO (sub 2) mixtures 700 degrees C pressures 3 5 kbar
Solubility quartz crustal fluids; experiments general equations salt solutions H (sub 2) O-CO (sub 2) mixtures 400-800 degrees C 0.1-0.9 GPa
Solubility quartz dilute HF solutions 600 degrees C 1 kbar
Solubility quartz dilute NaOH solutions 325 degrees C
Solubility quartz hypersaline brine; implications fracture permeability brittle-ductile transition
Solubility quartz supercritical water
Solubility quartz water temperature interval 25 degrees C. 300 degrees C
Solubility rare earth elements transition metals role increasing pH unsaturated-zone transport tests Busted Butte, Nevada
Solubility rock-forming minerals hydrothermal systems (thermodynamic analysis)
Solubility ruthenium sulphide melt; implications IPGE alloy stability
Solubility scheelite hydrothermal chloride solutions
Solubility secondary uranium minerals
Solubility siderite (FeCO (sub 3) ) concentrated NaCl Na (sub 2) SO (sub 4) solutions 25 degrees C
Solubility silica concentrated aqueous solutions formamide lithium chloride; measurement coefficient activity silica solution
Solubility silicate melts water; speciation problems
Solubility silicon oxygen Earth's core
Solubility silicon hcp-iron
Solubility simple pelitic granitic mineral assemblages chloride rich aqueous solutions 2 kbar, 400 degrees -650 degrees C
Solubility sodalite aqueous solutions NaOH hydrothermal conditions
Solubility soil samples geochemical studies copper, nickel cobalt
Solubility solid solutions water; comments F. Lippmann's paper Aqueous solubility magnesian calcites diverse endmembers
Solubility solids gases vapors
Solubility solids superheated steam
Solubility ore-forming sulfides hydrothermal conditions
Solubility sphalerite galena solutions H (sub 2) O-NaCl system; experimental theoretical investigations
Solubility sphalerite aqueous solutions 80 degrees C
Solubility stibnite (Sb (sub 2) S (sub 3) ) water hydrogen sulfide solutions temperatures 200-300 degrees C vapor-saturated conditions pressure 500 Bar
Solubility stibnite H (sub 3) BO (sub 3) NaB(OH) (sub 4) solutions 100 degrees C 250 degrees C 100 1000 bars
Solubility stibnite, realgar, orpiment alkaline solutions 100 degrees C 1 bar
Solubility stibnite, solution species balance constants 25 350 degrees C
Solubility sulfates ground water Paleozoic deposits Kuibyshev part Volga area
Solubility sulfides chloride solutions 500 degrees C
Solubility sulfur sulfide immiscibility synthetic tholeiitic melts relevance Bushveld-Complex rocks
Solubility sulfur CaMgSi (sub 2) O (sub 6) NaAlSi (sub 3) O (sub 8) melts high pressure temperature controlled (sub O2) (sub S2)
Solubility sulfur ultramafic melt relevance scheme Fe-S-O
Solubility sulfur silicate liquids high fO (sub 2ú
Solubility sulfur silicate melts role S (sub 2) silicate bulk composition high pressures
Solubility sulfur silicate melts high pressure temperature role (sub S2) (sub O2)
Solubility sulfur silicate melts simulating magmas
Solubility sulfur ultramafic melts relevance scheme Fe-S-O
Solubility sulphides precipitation hydrothermal solutions data thermodynamic examination
Solubility sulphur stability pyrrhotite anhydrite role f(O (sub 2) ) f(S (sub 2) ) andesites
Solubility symplesite (ferrous arsenate); implications reduced groundwaters geochemical environments
Solubility synthetic sphalerite aqueous solutions phosphoric acid
Solubility assemblage pyrite-pyrrhotite-magnetite-sphalerite-galena-gold-stibnite-bismuthinite-argen- tite-molybdenite H (sub 2) O-NaCl-CO (sub 2) solutions 200 degrees 350 degrees C degrees
Solubility gold sulfides Au (sub 2) S AuAgS solutions hydrogen sulfide 25-80 degrees C pressures 1-500 bar
Solubility hematite neutral weak-acidic aqueous solutions
Solubility magnetite+hematite buffer assemblage HCl solutions 300 degrees C 500 bars
Solubility magnetite+hematite buffer assemblage NaCl solution 300 degrees C 500 bar
Solubility magnetite-hematite buffer assemblage HCl solutions 300 degrees C 500 bars
Solubility metastable sheet-type silica hydrothermal solutions
Solubility titanium rutile effect oxalic acid
Solubility thorianite water solutions
Solubility tin dioxide dry sodium-rich granite metals
Solubility tin, tungsten molybdenum oxides felsic magmas
Solubility titanium basalt melt (experimental data)
Solubility titanium chloride fluoride hydrothermal solutions
Solubility titanium molten basalt, experimental data
Solubility trace elements coal fly ash
Solubility tugarinovite water solutions 250 degrees C 450 degrees C
Solubility tungstic oxide molybdenum oxide basalt melt
Solubility tungstic oxide granite melts
Solubility high-Mg high-Fe chlorites multiple equilibria
Solubility high-Mg chlorites multiple equilibria
Solubility ulexite CO (sub 2) -containing water
Solubility unirradiated uranium oxide granitic groundwater
Solubility uraninite acid hydrothermal solutions balance mineral associations zonally altered rocks
Solubility uraninite reducing conditions elevated temperatures pressures
Solubility uranium dioxide acidic chloride fluids 400-600 degrees C 1 kbar
Solubility uranium dioxide hydrochloric acids 400-600 degrees 1kbar
Solubility uranium granitic melts
Solubility uranium rocks bacteria belong genus Thiobacillus
Solubility uranium oxides water 773K 100 MPa
Solubility uranyl brine
Solubility volatile electrolytes multicomponent solutions atmospheric functions
Solubility volatile scheme C-O-H-N magmatic melts crystals; problems fluid regimes upper mantle
Solubility volatiles silicate melts high pressure temperature; function carbon dioxide water feldspar, pyroxene, feldspathoid melts
Solubility volatiles silicate melts pressure temperature conditions partial melting upper mantle
Solubility water carbon dioxide acidic basic magmas
Solubility water carbon dioxide icelandite 1400 degrees C 10 kilobars
Solubility water carbon dioxide felsic mafic magmas
Solubility water carbon dioxide granitic basaltic melts high pressures
Solubility water albite-melt determined volume loss method; discussion reply
Solubility water albite-melt determined weight-loss technique
Solubility water alpha , beta gamma (Mg,Fe) (sub 2) SiO (sub 4) high pressures
Solubility water carbonatite magmas partitioning F Cl magma aqueous fluid
Solubility water igneous rock melts
Solubility water magmas 2 kbar
Solubility water melts systems Na (sub 2) O-Al (sub 2) O (sub 3) -SiO (sub 2) K (sub 2) O-Al (sub 2) O (sub 3) -SiO (sub 2)
Solubility water melts plagioclase-like compositions scheme CaO-Na (sub 2) O-Al (sub 2) O (sub 3) -SiO (sub 2) -H (sub 2) O
Solubility water olivine single crystals
Solubility water quartz; revision
Solubility water silicate melts high pressure
Solubility water alpha , beta gamma phases (Mg,Fe) (sub 2) SiO (sub 4)
Solubility zeolites 4A 13X basic aqueous solutions; effect liquid/ solid ratio
Solubility zincite hydrothermal conditions
Solubility predictions complex mineral systems
Solubility product olivine silicate melts
Solubility products stoichiometric solubilities minerals hydrothermal systems
Solubility products calcium molybdate calcium tungstate; ratio powellite scheelite mineralization hydrothermal conditions
Solubility products calcium molybdate tungstate relationship powellite scheelite mineralization hydrothermal conditions
Solubility products solid phases variable composition geochemical significance
Solubility relations scheme NaCL-KCl-H (sub 2) O; experimental measurement computer programme
Solubility relations scheme NaCl-CsCl-H (sub 2úO 25 degrees C
Solubility relations scheme NaCl-FeCl (sub 2ú-H (sub 2úO 25 degrees 70 degrees C 1 atm
Solubility relations ternary scheme NaCl-CsCl-H (sub 2) O 1 atm; 1, Solubilities halite 20 100 degrees C
Solubility relations ternary scheme NaCl-CsCl-H (sub 2) O 1 atm; 2, Solubility relations 25 degrees C
Solubility relations ternary scheme NaCl-CsCl-H (sub 2) O 1 atm; 3, Solubility relations 50 75 degrees C
Solubility relationships NaCl-KCl-H (sub 2) O scheme
Solubility relationships aluminum iron minerals acid drainage
Solubility investigations potential high-level nuclear waste repository Yucca Mountain, Nevada