Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

egional dextral wrenching; F3- M Miocene-Recent WSW-directed compression along older NNW-striking
wrench faults and transtension along N-NNE-striking elements)
Heidrick, T.L., K. Aulia, B. Mertani & Yarmanto (1996)- Petroleum geology of Indonesian basins, II: Central
Sumatra basin. Pertamina BPPKA, 232p.
Heim, A. & R. Potonie (1932)- Beobachtungen uber die Entstehung der Tertiaren Kohlen (Humolithe und
Saprohumilithe) in Zentral Sumatra. Geol. Rundschau 23, p. 145-172.
(‘Observations on the origin of Tertiary coals in Central Sumatra’. Rel. young Oligocene coals reach
anthracite stage due to elevated temperature only)
Hendrian, D. & A. Fadly (2010)- Development drilling at fault zone in Pedada field, Central Sumatra Basin.
Proc. 39th Ann. Conv. Indon. Assoc. Geol. (IAGI), Lombok, PIT-IAGI-2010-219, 7p.
Hennings, P., P. Allwardt, P. Paul, C. Zahm, R. Reid, H. Alley, R. Kirschner, Bob Lee & E. Hough (2012)-
Relationship between fractures, fault zones, stress, and reservoir productivity in the Suban gas field, Sumatra,
Indonesia. AAPG Bull. 96, 4 , p. 753-772.
(Analysis of fractured Miocene carbonate and Pre-Tertiary crystalline basement reservoirs of Suban gas field,
S Sumatra. Structures composite of Paleogene extensional elements, modified by Neogene contraction. Faults
along W flank of field show classic oblique-compressional geometry. Reservoir potential most enhanced in
areas of field that are in strike-slip stress style and lower in areas of thrust-fault stress)
Henstock, T.J, L.C. McNeill & D.R.Tappin (2006)- Seafloor morphology of the Sumatran subduction zone;
surface rupture during megathrust earthquakes? Geology 34, 6, p. 485-488.
(High-resolution multibeam bathymetry data from Sumatran subduction zone)
Heriana, N. (1996)- Prospektifitas hidrokarbon di tepian cekungan Sumatra Utara berdasarkan aspek batuan
induk. Proc. 25th Ann. Conv. Indon. Assoc. Geol. (IAGI), 2, p. 459-477.
('Hydrocarbon prospectivity on the margin of the North Sumatra basin based on aspects of source rocks')
Heriana, N. (1999)- Gas habitat in the southern part of the North Sumatra Basin. In: C.A. Caughey & J.V.C.
Howes (eds.) Proc. Conf. Gas Habitats of SE Asia and Australasia, Jakarta, Indon. Petrol. Assoc., p. 135-144
(Gas in S part N Sumatra Basin in Keutapang, Mid-Baong Sandstone (MBS), and Belumai Fms. Usually gas
with oil or condensate; Wampu Field gas without associated liquids. Gases two groups: Rantau in N with
condensate, Aru-Langkat in S from non-associated sapropelic organic matter. Bampo Fm black shales reached
gas generation phase and possible gas source. Traps formed in Plio-Pleistocene and may still be filling)
Heriana, N. & R. Ryacudu (1993)- Structural evaluation of onshore Northern Sumatra. Proc. 22nd Ann. Conv.
Indon. Assoc. Geol. (IAGI), Bandung 1993, 1, p. 112-125.
Hermiyanto, H.M. (2008)- Coalbed methane potential and coal characteristics in Kuantan Singingi, Central
Sumatera Basin, Riau. J. Sumber Daya Geol. (GRDC) 18, 4, p. 239-251.
(Analysis of Eocene coal from Keruh Fm in small intra-montane basin at SW side of C Sumatra basin)
Hermiyanto, H.M. & N.S. Ningrum (2009)- Organic petrology and Rock-Eval characteristics in selected
surficial sampes of the Tertiary formation, South Sumatra basin. J. Geol. Indonesia 4, 3, p. 215-227.
(Study of organic matter types and maturation of Oligocene- Miocene outcrop samples from S Sumatra)
Hermiyanto, H.M. & H. Panggabean (2008)- Karakteristik oil shale di kawasan Bukit Susah, Riau. J. Sumber
Daya Geol. (GRDC) 18, 1, p. 3-13.
('Characteristics of oil shale in the Bukit Susah District, Riau'. C Sumatra basin Kelesa Fm at Bukit Susah with
~28m of oil shale. Vitrinite reflectance 0,27- 0,43% (immature). Palynology suggests M-L Eocene age)
Bibliography of Indonesia Geology v. 4.1 42 www.vangorselslist.com July 2012