A geochemical study of crude oils from the Guafita oil field, Apure st
ate, Venezuela, was undertaken in order to obtain information concerni
ng the organic matter that gave origin to them, their degree of maturi
ty, the possible source rock that originated them, and the alteration
processes that they may have suffered in the reservoir. The concentrat
ion of total sulfur, saturated hydrocarbons, aromatic hydrocarbons, re
sins and asphaltenes, in these oils, were determined. The distribution
of saturated hydrocarbons was determined by gas chromatography. The d
istribution of steranes and terpanes (m/z 191 and 217), and aromatic c
ompounds (m/z 178, 192, and 198) was determined by mass spectrometry.
Results indicate that the crude oils analyzed are paraffinic-naphtheni
c, unaltered, and derived predominantly from marine organic matter wit
h a small contribution of continental organic matter. These crude oils
were generated by a mature, clastic, source rock.