Petroleum system

Oil and gas in Enrekang Block produced from Tertiary
Eocene age deeper target which is Toraja Formation.
The reservoirs mostly are fluvio-deltaic fine – medium
sandstones, Mio-Pliocene Carbonate and Volcanoclastic.
Source rock of oil and gas of this field believes
derived from organic rich of Lower Toraja. The
kerogene type indicates that Tertiary deposits are
dominated by a type II/III kerogene derived from
higher plant material, with minor algal, exinite or
lipnite influence. Muddy and carbonates Makale
Formation act as seal.

Porosities of Toraja sandstone range up to 20 – 25 % ,
TOC values 31% – 81% and HI values 158 - 758

Both of lateral and vertical oil and gas migration
would have happened in Miocene age. Vertical migration
to shallow reservoirs proceeded by means of fault
conduits extending directly from source rocks to the
reservoirs. Lateral migration would have proceeded
along dip slope. 


Deni Rahayu
Exploration Think Tank Indonesia
www.etti.co.id


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