『Abstract
Sedimentary basins located in the continent-to-ocean transition
zones with an active tectonic regime are extremely different in
terms of both geological structure and composition of rocks with
the hydrocarbon-hosting potential. Oil-and-gas fields in such
zones are confined not only to the deltaic, coastal-marine, and
submarine-slope sandstones, as well as limestones and dolomites
of buried carbonate banks, but also to silicic and volcanic rocks.
Such fields have been discovered in weathering crusts of granite
plutons, metamorphic rocks of the basement, fissured basalts,
and other magmatic rocks. This is demonstrated vividly by the
Southeast Asia region, including Indonesia, Malaysia, Vietnam,
Bangladesh, and other countries, where fore-arc, back-arc, inter-arc,
and marginal-rift sedimentary basins are assigned to petroliferous
areas.』
(Introduction)
The Brunei basin
The south Sumatra basin
The north Java basin
The east Java basin
The Kutei basin (east Kalimantan)
The Mekong basin
Conclusions
References