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Baddeleyite (ZrO2) and zircon (ZrSiO4) from anorthositic rocks of the Laramie anorthosite complex, Wyoming: Petrologic consequences and U-Pb ages
-
James S. Scoates
und Kevin R. Chamberlain
Veröffentlicht/Copyright:
13. November 2015
Received: 1994-10-24
Accepted: 1995-6-6
Published Online: 2015-11-13
Published in Print: 1995-11-1
© 2015 by Walter de Gruyter Berlin/Boston
Artikel in diesem Heft
- Asbestiform riebeckite (crocidolite) dissolution in the presence of Fe chelators: Implications for mineral-induced disease
- Derivation and identification of nonstandard serpentine polytypes
- Complex polytypism: Relationships between serpentine structural characteristics and deformation
- Parallel electron energy-losss pectroscopy( PEELS) study of B in minerals: The electron energy-loss near-edge structure (ELNES) of the B K edge
- Single-crystal IR spectroscopy of grossular-andradite garnets
- Raman study at high pressure and the thermodynamic properties of corundum: Application of Kieffer's model
- Annealing of synthetic hammarite, Cu2Pb2Bi4S9, and the nature of cation-ordering processes in the bismuthinite-aikinite series
- High-angle annular dark-field microscopy of franckeite
- A simple model for sector zoning in slowly grown crystals: Implications for growth rate and lattice diffusion, with emphasis on accessory minerals in crustal rocks
- Simulations of convection with crystallization in the system KAlSi2O6-CaMgSi2O6: Implications for compositionally zoned magma bodies
- SIMS studies of planetary cumulates: Orthopyroxene from the Stillwater Complex Montana
- Role of fluid flow in the contact metamorphism of siliceous dolomitic limestones- Discussion
- Role of fluid flow in the contact metamorphism of siliceous dolomitic limestones-Reply to Hanson
- An experimental study of element partitioning among biotite, muscovite, and coexisting peraluminous silicic melt at 200 MPa (H2O)
- Experimental determination of the reactions magnesite + quartz = enstatite + CO2 and magnesite = periclase + CO2, and enthalpies of formation of enstatite and magnesite
- Experimental study of the solid solution between monazite-(La) and (Ca0.5U0.5)PO4 at 780 °C and 200 MPa
- Stability and structure of a new high-pressure silicate, Na1.8Ca1.1Si6O14
- Low-temperature phase transitions and the role of hydrogen bonds in lawsonite
- Lawsonite: Upper pressure stability and formation of higher density hydrous phases
- The fate of olivine in subductings labs: A reconnaissance study
- Techniques for determining pressure in the hydrothermal diamond-anvil cell: Behavior and identification of ice polymorphs (I, III, V, VI)
- Inclusions of phlogopite and phlogopite hydrates in chromite from the Hongguleleng ophiolite in Xinjiang, northwest China
- Baddeleyite (ZrO2) and zircon (ZrSiO4) from anorthositic rocks of the Laramie anorthosite complex, Wyoming: Petrologic consequences and U-Pb ages
- New Mineral Names
- Book Review
- Infrared spectroscopy of hydrous silicate melts to 1000 °C and 10 kbar: Direct observation of H2O speciation in a diamond-anvil cell
- Determination of the molar absorptivity of dissolved carbonate in basanitic glass
- The Stillwater Complex, Montana: A subvolcanic magma chamber?
- H deficiency in kaersutitic amphiboles: Experimental verification
- Author Index, Volume 80, 1995
- Subject Index, Volume 80, 1995
Artikel in diesem Heft
- Asbestiform riebeckite (crocidolite) dissolution in the presence of Fe chelators: Implications for mineral-induced disease
- Derivation and identification of nonstandard serpentine polytypes
- Complex polytypism: Relationships between serpentine structural characteristics and deformation
- Parallel electron energy-losss pectroscopy( PEELS) study of B in minerals: The electron energy-loss near-edge structure (ELNES) of the B K edge
- Single-crystal IR spectroscopy of grossular-andradite garnets
- Raman study at high pressure and the thermodynamic properties of corundum: Application of Kieffer's model
- Annealing of synthetic hammarite, Cu2Pb2Bi4S9, and the nature of cation-ordering processes in the bismuthinite-aikinite series
- High-angle annular dark-field microscopy of franckeite
- A simple model for sector zoning in slowly grown crystals: Implications for growth rate and lattice diffusion, with emphasis on accessory minerals in crustal rocks
- Simulations of convection with crystallization in the system KAlSi2O6-CaMgSi2O6: Implications for compositionally zoned magma bodies
- SIMS studies of planetary cumulates: Orthopyroxene from the Stillwater Complex Montana
- Role of fluid flow in the contact metamorphism of siliceous dolomitic limestones- Discussion
- Role of fluid flow in the contact metamorphism of siliceous dolomitic limestones-Reply to Hanson
- An experimental study of element partitioning among biotite, muscovite, and coexisting peraluminous silicic melt at 200 MPa (H2O)
- Experimental determination of the reactions magnesite + quartz = enstatite + CO2 and magnesite = periclase + CO2, and enthalpies of formation of enstatite and magnesite
- Experimental study of the solid solution between monazite-(La) and (Ca0.5U0.5)PO4 at 780 °C and 200 MPa
- Stability and structure of a new high-pressure silicate, Na1.8Ca1.1Si6O14
- Low-temperature phase transitions and the role of hydrogen bonds in lawsonite
- Lawsonite: Upper pressure stability and formation of higher density hydrous phases
- The fate of olivine in subductings labs: A reconnaissance study
- Techniques for determining pressure in the hydrothermal diamond-anvil cell: Behavior and identification of ice polymorphs (I, III, V, VI)
- Inclusions of phlogopite and phlogopite hydrates in chromite from the Hongguleleng ophiolite in Xinjiang, northwest China
- Baddeleyite (ZrO2) and zircon (ZrSiO4) from anorthositic rocks of the Laramie anorthosite complex, Wyoming: Petrologic consequences and U-Pb ages
- New Mineral Names
- Book Review
- Infrared spectroscopy of hydrous silicate melts to 1000 °C and 10 kbar: Direct observation of H2O speciation in a diamond-anvil cell
- Determination of the molar absorptivity of dissolved carbonate in basanitic glass
- The Stillwater Complex, Montana: A subvolcanic magma chamber?
- H deficiency in kaersutitic amphiboles: Experimental verification
- Author Index, Volume 80, 1995
- Subject Index, Volume 80, 1995