HIGHLIGHTS
SUMMARY
The development of geochemistry helped the kerogen to produce hydrocarbon or gas; this was achieved by experimental tests (e_g, Rock-Eval VI pyrolize), where models were simulated to process maturation, generation, and migration. Detailed geochemical studies in the Kastos Island (external Ionian sub-basin) and the Araxos peninsula (internal Ionian sub-basin) were compared with previous studies from the Gotzikas area (middle Ionian sub-basin) and the Ioannina well (internal Ionian sub-basin). It seems that the richness in Kastos Island (external Ionian sub-basin) and the poorness in the Araxos peninsula (internal Ionian . . .
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