Results 121 to 130 of about 12,511 (212)
Superthermal gas giant planets or their progenitor cores are known to open deep gaps in protoplanetary disks, which stop large, drifting dust particles on their way to the inner disk.
Thomas Pfeil +2 more
doaj +1 more source
Molecular Distribution, 13C-Isotope, and Enantiomeric Compositions of Carbonaceous Chondrite Monocarboxylic Acids [PDF]
The watersoluble organic compounds in carbonaceous chondrite meteorites constitute a record of the synthetic reactions occurring at the birth of the solar system and those taking place during parent body alteration and may have been important for the ...
Abreu, Neyda M. +4 more
core +1 more source
Amino acids in Antarctic CM1 meteorites and their relationship to other carbonaceous chondrites [PDF]
Oliver Botta +2 more
openalex +1 more source
Forming the Noncarbonaceous Chondrite Parent Bodies in the Presence of the Jupiter Barrier
Meteorites can be divided into two groups—noncarbonaceous chondrite like (NC) and carbonaceous chondrite like (CC)—with distinct stable-isotope compositions. Parent bodies of NC and CC meteorites have overlapping formation ages. This suggests they formed
John Chambers
doaj +1 more source
Analyses of Aliphatic Aldehydes and Ketones in Carbonaceous Chondrites. [PDF]
Aponte JC +4 more
europepmc +1 more source
Molecular distribution and
José C. Aponte +7 more
openalex +1 more source
On the origins of organic matter in carbonaceous chondrites [PDF]
Jacques Reisse, Françoise Mullie
openalex +1 more source
Spectroscopy of the Hamburg Meteorite, Michigan H4
Spectroscopic studies of the Hamburg (Michigan H4) meteorite using visible–near-infrared (VNIR), mid-infrared (MIR), Raman, and Mössbauer data reproduce the results of more conventional laboratory measurements of petrology and geochemistry.
M. Darby Dyar +12 more
doaj +1 more source

