The influence of organic sources and environments on source rock deposition during the periods of Cretaceous-Eocene and Oligocene-Miocene, northern Kalimantan

The sedimentary system of Kalimantan has undergone significant development since the Oligocene. Previous research have largely ignored the capacity of the Cretaceous-Eocene sediments to produce hydrocarbons, focusing instead primarily on the Oligocene-Miocene coal as the principal source rocks. Shal...

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