Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Philippi, H. (1923)- Contributions a la geologie de la partie meridionale de Sumatra: gisements de fer dans les
districts des Lampongs. Univ. Geneve Fac. Sci., Thesis 720, 42p.
('Contributions to the geology of the southern part of Sumatra; iron-bearing beds in the Lampung District.' Rel.
little detailed description of iron-bearing rocks near Sukadana/ Telukbetung)
Philippi, H. (1925)- Beschrijving van ijzerertsafzettingen op de hellingen van den Radjabasa (Lampongsche
Districten). Verhand. Geol. Mijnbouwk. Gen. Nederl. Kol., Geol. Ser. 8 (Verbeek volume), p. 393-403.
('Description of iron ore deposits on the slopes of the Rajabasa (Lampong Districts)'. On non-commercial iron
ore deposits on N slope Rajabasa volcano, S Sumatra)
Poerwanto, J.H., C.F. Sugembong, J.M. Bagzis & A.D. Martinez (1995)- Application of hydraulic fracturing
technologies to the shallow Telisa Formation. SPE Asia Pacific Oil Gas Conf., Kuala Lumpur 1995, p. 277-284.
(On fracturing treatments in shallow (600'), high permeability (10-100 mD) laminated sandstone reservoir in E
Miocene Telisa Fm, South Balam Field, 50 km NW of Duri, C Sumatra)
Posavec, M., D. Taylor, T. van Leeuwen & A. Spector (1973)- Tectonic controls of volcanism and complex
movements along the Sumatran fault system. Geol. Soc. Malaysia Bull. 6, p. 43-60.
(Rio Tinto work along Sumatra fault zone. Igneous activity along E-W alignments suggested by magnetic
lineaments. Active volcanic centers spaced at 75-100 km along active fault zone. Total horizontal offset along
fault ~130 km since inception of present volcanic cycle)
Posthumus, O. (1927)- Some remarks concerning the Palaeozoic flora of Djambi, Sumatra. Proc. Kon. Acad.
Wet. Amsterdam 30, 6, p. 628-634.
(Carboniferous or Permian fossil plants from Jambi show most resemblance to Gigantoperis flora of E Asia,
not Gondwana Glossopteris fauna)
Pramumijoyo, S. (1993)- Neotectonique et sismotectonique de la terminaison meridionale de la Grande Faille
de Sumatra et du Detroit de la Sonde (Indonesie). Doct. Thesis, Universite Paris XI, Paris, p.
('Neotectonics and seismotectonics at the southern end of the Great Sumatra Fault and Sunda Straits')
Pramumijoyo, S. & M. Sebrier (1991)- Neogene and Quaternary fault kinematics around the Sunda Strait area,
Indonesia. J. Southeast Asian Earth Sci. 6, 2, p. 137-145.
(Sunda Strait transition zone from orthogonal subduction off Java to oblique subduction off Sumatra. Opening
of Sunda Strait consequence of right lateral movement of Sumatran Fault System-SFS. Two main kinematics on
faults around Sunda Strait area: dextral strike-slip and normal. Strike-slip deformations in Miocene or older
rocks, Pliocene and younger formations only normal faulting. Dextral slip on SFS began during M Miocene and
normal faulting prevailed in Sunda Strait since 5 Ma, controlling bathymetry of Sunda Strait)
Pranyoto, U., B. Setiardja & E. Sjahbuddin (1990)- Pembentukan, migrasi dan terperangkapnya hidrokarbon di
daerah Rantau, Aru dan Langkat-Medan, Cekungan Sumatra Utara. Proc. 19th Ann. Conv. Indon. Assoc. Geol.
(IAGI), 1, p. 175-200.
('Formation, migration and trapping of hydrocarbons in the Rantau, Aru and Langkat-Medan areas, N Sumatra
basin')
Praptono, S.H., R. Dwiputro, I.M. Longley & R.W. Ward (1991)- Kurau: an example of the low-relief structural
play in the Malacca Strait PSC, Sumatra, Indonesia. Proc. 20th Ann. Conv. Indon. Petrol. Assoc., p. 299-318.
(Kurau field two separate low relief anticlinal structures on E margin of Bengkalis Trough. Traps formed by
drape over structures formed in Late Oligocene. These structures, cored by basement and Pematang Group
rocks, remained largely unaffected by Late Miocene- Pliocene tectonism. This later tectonism produced many
high-relief structures which were focus for early exploration. Stacked oil pools, with >150 MMBO in-place,
largest in PSC . Discovered late in exploration history of area due to relatively subtle nature of trap)
Bibliography of Indonesia Geology v. 4.1 78 www.vangorselslist.com July 2012