Pacitan Regency is the westernmost district of the province of East Java which is directly adjacent to the Wonogiri Regency (Central Java) to the west. Pacitan can be reached in about 4 hours from Yogyakarta by land transportation via the southern route of Java. The morphology of the Pacitan district is very unique characterized by semicircular valleys flanked by hills in the east, north, and west. The hills are dominated by rocks of ancient Oligo- Miocene volcanic products known as the Old Andesite Formation. Pacitan stratigraphy, from the older to the younger, consists of Oligocene Volcanics (Mandalika, Watupatok, and Arjosari Formations), Early Miocene Carbonates (Campurdarat and Jaten Formations), Middle Miocene Volcanics (Wuni Formation), Late Miocene-Pliocene Carbonates (Nampol, Oyo, and Wonosari Formations), and Holocene alluvial deposits (Kalipucang Formation). The presence of dominant volcanic rock has been considered as an area without petroleum play prospect. To test this consideration, we study the potential possibility of petroleum system of southern mountainous sub-volcanic deposits which is commonly found in the Pacitan area. Jaten and the Nampol Formations are the interesting formations in terms of petroleum system because they are composed of sandstone, shale, and coal intercalations that are very rich in carbon materials. They also have the potential to be a reservoir because of their physical properties such as good porosity and permeability. This study is purposed to analyze the reservoir potential of sub-volcanic formation on the basis of their porosity and permeability properties. This study using petrographic thin section analysis and lab tests as the method.

1.
Choquette
PW
,
Pray
LC
.,
1970
.,
Geologic Nomenclature and Classification of Porosity in Sedimentary Carbonates
.,
The American Association of Petroleum Geologists Bulletin
v.
54
no.
2
(February,
1970
)., p.
207
250
2.
Koesoemadinata
,
R.P.
,
1978
,
Geologi Minyak Bumi
.,
Bandung
.
ITB Publisher
.
3.
Nahrowi
,
T.
,
Suratman
,
Y.
&
Hidayat
,
S.
,
1978
.,
Geologi Pegunungan Selatan, Jawa Timur
,
Exploration PPTMGB, Lemigas Cepu
.
4.
Pulunggono
,
A.
&
Martodjojo
,
S.
,
1994
.,
Perubahan Tektonik Paleogen – Neogen Merupakan Peristiwa Tektonik Terpenting Di Jawa
,
Proceeding of Geology dan Geotectonic of Java from Late Mesozoic until Quarter, Geology Department, UGM, hal.
37
50
.
5.
Samodro
,
H.
&
Sampurno.
,
1989
,
Tinjauan tatanan stratigrafi dan tektonik Pegunungan Selatan Jawa Timur antara Pacitan – Ponorogo
,
P3G
,
Bandung
.
6.
Sribudiyani.
,
2003
.,
The Collision Of The East Java Microplate And Its Implication For Hydrocarbon Occurrences In The East Java Basin.
,
Proceeding Indonesian Petroleum Association
October
2003
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