Isotopic characteristics of simulated meteoritic organic matter: 1--Kerogen-like material.
Carbonaceous residues from a variety of laboratory syntheses yield release patterns for C and H isotopes during stepwise combustion that fail to mimic the striking patterns characteristic of meteoritic kerogen-like residues that otherwise superficially resemble them.  It seems likely that the meteoritic material comprises a complex mixture of substances having different origins and/or synthesis conditions.
Kerridge
J F
JF
Institute of Geophysics, UCLA 90024, USA.
Mariner
R
R
Flores
J
J
Chang
S
S
D002244:Carbon / Q000737:chemistry*; D002247:Carbon Isotopes; D003903:Deuterium / Q000737:chemistry*; D006838:Hydrocarbons / Q000737:chemistry*; D006859:Hydrogen / Q000737:chemistry*; D019110:Meteoroids; D013696:Temperature
D002247:Carbon Isotopes; D006838:Hydrocarbons; D002244:Carbon; D006859:Hydrogen; D003903:Deuterium