A First Attempt to Simulate the Natural Formation of Meteoritic Organics

Computer Science

Scientific paper

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Scientific paper

Amorphous iron silicates are used as to convert CO, N2 and H2 to complex
hydrocarbons on the surfaces of the grains at 675K, 775K and 875K.
Samples of these grains are then either vacuum annealed at 875K and 975K
or hydrated at 300K or 350K. The resultant organics are analyzed via
pyrolysis GC-MS.

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