Aliphatic Hydrocarbons in Meteorites

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Scientific paper

Naturally occurring mixtures of terrestrial isoprenoids and other aliphatic hydrocarbons give the same chromatographic patterns as aliphatic hydrocarbons from carbonaceous chondrites; carbonaceous chondrites Wiik Types II and III show substantially higher contents of aliphatic hydrocarbons than meteoritic graphite nodules and Type I carbonaceous chondrites. Any theory of the origin of hydrocarbons in meteorites must explain these features.

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