Results 81 to 90 of about 1,510 (199)
Combustion and Pyrolysis EA‐IRMS Techniques to Determine the δ2H of Diamonds
ABSTRACT Rationale Diamonds are generally considered to be metasomatic minerals originating from the Earth's mantle. They formed through the interaction of carbon‐bearing fluids or melts with the surrounding deep lithology. Most knowledge about the formation of diamonds comes from studying their mineral inclusions or stable isotopes.
François Fourel +4 more
wiley +1 more source
Resolving the Internal Magnetic Domain Structure of Cloudy Zone Tetrataenite
Abstract Recent advances in magnetic imaging can directly capture the internal magnetization of natural and synthetic materials at resolutions <10 nm. This capability opens new possibilities to determine the magnetic domain state of ferromagnetic minerals that are fundamental for recording and retaining paleomagnetic records.
Elias N. Mansbach +5 more
wiley +1 more source
Primitive meteorite groups such as the Vigarano, Mighei, and Karoonda carbonaceous chondrites have enigmatic patterns of elemental abundances, with moderately volatile elements—those that transition from vapor to condensate between ∼400 and ∼900 K ...
Jeremy W. Boyce +3 more
doaj +1 more source
Pułtusk H5 Chondrite—A Compilation of Chemical, Physical, and Thermophysical Data
The Pułtusk meteorite, classified as an H5 ordinary chondrite, is one of the best documented Polish falls, yet some important data on its physical and thermophysical properties remain limited.
Katarzyna Łuszczek, Radosław A. Wach
doaj +1 more source
The analysis of samples returned from the C-type asteroid Ryugu has drastically advanced our knowledge of the evolution of early solar system materials.
Ryoji Tanaka +25 more
doaj +1 more source
Modeling Carbon Outgassing from Chondritic Planetesimals
The thermochemical evolution of planetesimals is an underprobed stage of volatile delivery to terrestrial planets during their formation, and may contribute to the volatile depletion of the Earth relative to primitive chondrites.
Bo Peng, Diana Valencia
doaj +1 more source
Bioweathering of a reduced chondritic material : implications for Enstatite chondrite
The aim of this study is to investigate the mineralogical and chemical processes which take place during the bioweathering of an enstatite chondrite by bacteria. Synthetic enstatite chondrites were made in laboratory in order to begin this complex study with simplified and well-defined materials.
openaire +1 more source
Phosphorus-nitrogen systematics of first-generation planetesimals constrain life-essential element delivery to Earth. [PDF]
Pathak D, Dasgupta R, Iyer N.
europepmc +1 more source
When wet meets dry: An Ivuna-like impactor triggered volatile loss on the angrite parent body. [PDF]
Zhu 朱柯 K +5 more
europepmc +1 more source
Non-equilibrium condensation of the first Solar System solids. [PDF]
Charnoz S +5 more
europepmc +1 more source

