Brian Mason

TL;DR: In this article, the authors reported that the resulting densities in the lower mantle are in good agreement with shock-wave measurements on rocks having FeO contents in the range 10 ± 2% by weight.

TL;DR: I: Geochemistry of Crystal Phases 1: Elemental Properties and Crystal Chemistry 2: Concepts of Chemical Thermodynamics 3: Thermochemistry of Crystalline Solids 4: Some Concepts of Defect Chemistry 5: Silicates II: Geochemical of Silicate Melts 6: SilicateMelts 7: Introduction to Petrogenetic Systems III: Geochemics of Fluids 8: Geography of Aqueous Phases 9: Chemical Chemistry of Gaseous Phasing IV: Methods 10: Trace Element Geochemistry 11: Isotope Geochemistry Appendix 1:

TL;DR: The first season of observations with the Degree Angular Scale Interferometer (DASI) was conducted at the South Pole in the austral summer 1999-2000, and observations throughout the following austral winter.

TL;DR: In this article, the authors present measurements of anisotropy in the Cosmic Microwave Background (CMB) from the first season of observations with the Degree Angular Scale Interferometer (DASI) and find no evidence of foregrounds other than point sources in the data.

TL;DR: Using the Cosmic Background Imager, a 13-element interferometer array operating in the 26-36 GHz frequency band, the authors observed 40 deg (sup 2) of sky in three pairs of fields, each approximately 145 feet x 165 feet, using overlapping pointings.