Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Pudjowalujo, H. (1990)- Cenozoic tectonics of North Sumatra with particular reference to the Sumatran fault
system. Proc. Pacific Rim Congress 90, Gold Coast 1990, Australasian Inst. Mining Metallurgy, Parkville, p.
209-215.
Pujasmadi, B., H. Alley & Shofiyuddin (2002)- Suban gas field, South Sumatra- example of a fractured
basement reservoir. In: F.H. Sidi & A. Setiawan (eds.) Proc. Giant Field and New Exploration Concepts
Seminar, Indon. Assoc. Geol. (IAGI), Jakarta, October 2002, p. 25-44.
(Suban gas field 1998 discovery 165km WNW of Palembang. Over 1000m gas column between 1800-3300m,
straddling E Miocene Baturaja Fm reefal limestone (33% of reserves), Oligocene Talang Akar Fm sandstones
and Eocene- Oligocene Lemat Fm conglomerates (19%) and fractured basement composed of M Jurassic
andesites, E Cretaceous granitoids and Permo-Carboniferous marine metasediments (48% of reserves))
Pujobroto, A. (1997)- Organic petrology and geochemistry of Bukit Asam coal, South Sumatra, Indonesia,
Ph.D. Thesis, School of Geosciences, University of Wollongong, p.
Pulunggono, A. (1969)- Basement configuration in the South Palembang basinal area: its signficance to
depositional conditions and oil-trappping. In: Fourth ECAFE Symp. Development of petroleum resources Asia
and Far East, Canberra 1969, 16p.
Pulunggono, A. (1986)- Tertiary structural features related to extensional and compressive tectonics in the
Palembang Basin, South Sumatra. Proc.15th Ann. Conv. Indon. Petrol. Assoc. 1, p. 187-213.
(Tertiary basin history. Tensional phase in Late Oligocene- E Miocene, coinciding with standstill of Indian
oceanic plate subduction below Sundaland. Oblique compression of N-ward converging Indian Ocean plate
solely accomodated by NW-SE trending proto-Barisan by lateral movements. The early M Miocene onset of
compression connected with renewed subduction. Diastrophism in Palembang Basin mainly confined to narrow
N-S zone with highest heatflow and most fields)
Pulunggono, A. & N.R. Cameron (1984)- Sumatran microplates, their characteristics and their role in the
evolution of Central and South Sumatra basins. Proc. 13 th Ann. Conv. Indon. Petrol. Assoc., p. 121-143.
(Milestone paper on Sumatra Pre-Tertiary mosaic of basement terranes. Mergui, Malacca and East Malaya
continental microplates joined in Late Triassic to form Sundaland, followed by Late Cretaceous accretion of W
coast Woyla volcanic arc terrain(s). Suture zone between Mergui and Malacca microplates, named Mutus
assemblage, major zone of weakness during formation of Tertiary C and S Sumatra basins. It is a zone of high
heat flow and underlies ~95% of two basin's oil production. Young Tertiary structures in this zone are related
to wrenching in N and S, and to compressional reactivation of cross cutting WNW-ESE faults formed during the
accretion of Woyla Terrains )
Pulunggono, A., A. Haryo S. & C.G. Kosuma (1992)- Pre-Tertiary and Tertiary fault systems as a framework of
the South Sumatra Basin; a study of SAR-maps. Proc. 21st Ann. Conv. Indon. Petrol. Assoc., p. 339-360.
(S Sumatra dominant trends WNW-ESE, N-S, NW-SE and ± N 30°E. Distribution of Jurassic and Cretaceous
granites important to explain geological evolution of Sundaland. Paleogene initiation of S Sumatra back-arc
basin by way of subsiding "block-areas" along WNW-ESE (Lematang) and N-S trending strike-slip faults of
Pre-Tertiary origin, rejuvenated as normal faults. Neogene compressive tectonics marked S Sumatran back-arc
basin development a.o. inducing inversion along WNW-ESE faults. NW-SE (Barisan or Semangko) trend offsets
WNW-ESE trend and presently active strike-slip fault zone at crestal parts of Barisan Mountain Range)
Pulunggono, A., C.I. Abdullah, D. Noeradi, E. Suparka, Djuhaeni & L. Samuel (1999)- Sumatran megashears;
Their crucial role in (Tertiary) sedimentary basin development. In: FOSI 1st Regional Seminar: Tectonics and
sedimentation of SE Asia, Bandung 1999. (Abstract only?)
Purucker, M. & T. Ishihara (2005)- Magnetic images of the Sumatra region crust. EOS 86, 10, p.
(Magnetic images near Great Sumatra earthquake. Along fault rupture magnetic crustal thicknesses increase to
E and NE. Island arc and subducting slab are magnetic, and subducting slab is diving into mantle at steep
angle, increasing magnetic thickness. Between Singapore and S coast Borneo, a previously unrecognized first-
Bibliography of Indonesia Geology v. 4.1 80 www.vangorselslist.com July 2012