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Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

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ejuvenation and strike-slip faulting. Interplay <strong>of</strong> lines <strong>of</strong> basement weakness with structural grain and<br />

compression have produced variety <strong>of</strong> features: en echelon folds, chains <strong>of</strong> anticlines and <strong>Sunda</strong> Folds)<br />

Mount, V. & J. Suppe (1992)- Present-day stress orientations adjacent to active strike-slip faults: California and<br />

<strong>Sumatra</strong>. J. Geophys. Res. 97, B8, p. 11,995-12,013.<br />

(Present-day stress directions from well bore breakouts near crustal-scale strike-slip faults (San Andreas in<br />

California and Great <strong>Sumatra</strong>n fault in <strong>Sumatra</strong>) indicate maximum horizontal stress direction (SH) at high<br />

angle (70°-90°) to both faults. Young deformation in C and S <strong>Sumatra</strong> is compressional, indicating decoupling<br />

<strong>of</strong> strike-slip and compressional components <strong>of</strong> deformation within broadly transpressive zones)<br />

Muchsin, A.M., C.C.Johnson, M.J. Crow, A. Djumsari & Sumartono (1997)- Geochemical atlas <strong>of</strong> southern<br />

<strong>Sumatra</strong> (Atlas geokimia daerah Sumatera bagian selatan). regional geochemical Atlas series <strong>of</strong> <strong>Indonesia</strong> 2,<br />

Bandung, p.<br />

Mujito, S. Hadipandoyo & J.B. Rachmat (1990)- Middle Baong Sandstone turbidite play, North <strong>Sumatra</strong> Basin,<br />

<strong>Indonesia</strong>. In: CCOP/WRGA Play modelling exercise 1989-1990, CCOP Techn. Publ. 23, p. 17-38.<br />

(Description and hydrocarbon assessment <strong>of</strong> M-L Miocene Middle Baong Sst depwater sand play, N <strong>Sumatra</strong>)<br />

Mujito, S. Hadipandoyo & T.H. Sunarsono (1990)- Hydrocarbon resources assesment in the North <strong>Sumatra</strong><br />

Basin. United Nations CCOP Techn. Bull. 21, p. 97-116.<br />

(Lemigas assessment <strong>of</strong> undiscovered oil and gas in four plays in N <strong>Sumatra</strong> basin. Keutapang Wedge Top Play<br />

ranked highest, with undiscovered oil ranging from 0.37- 504 MMBO)<br />

Mukherjee, A.N. (1935)- Ein Beitrag zur Kenntnis der pliocanen Braunkohle des Tandjoeng Kohlenfeldes<br />

Palembang, Sud-<strong>Sumatra</strong>. Diss. Sachsischen Bergakademie Freiburg. 30 p.<br />

(‘A contribution to the knowledge <strong>of</strong> the Pliocene lignites <strong>of</strong> the Tanjung coalfield, Palembang, S <strong>Sumatra</strong>’.<br />

Early Pliocene Middle Palembang Fm lignites at Bukit Asam locally altered into coal- anthracite by heat from<br />

andesite intrusion. Coals composed <strong>of</strong> wood (incl. palm), cork, amber, leaves and cuticles, fungi, pyite. Good<br />

thin section photos)<br />

Mukti, M.M., S.C. Singh, N.D. Hananto, D. Ghosal & I. Deighton (2011)- Structural style and evolution <strong>of</strong> the<br />

<strong>Sumatra</strong>n forearc basins. Proc. 35 th Ann. Conv. Indon. Petrol. Assoc., IPA11-G-082, p. 1-7.<br />

(Crust beneath <strong>Sumatra</strong> fore arc basin thin (~20 km), thickens towards mainland. NE-SW extensional structures<br />

with probably Late Eocene- E Oligocene syn-rift sediments. Late Oligocene- E Miocene post-rift sediments in<br />

grabens and slopes. Grabens exhibit transtensional structures. Inversion <strong>of</strong> structures related to transpressional<br />

strike-slip fault zone, followed by M-L Miocene marked subsidence, overprinting older depocenters)<br />

Mukti, M.M., S.C. Singh, R. Moeremans, N.D. Hananto, H. Permana & I. Deighton (2012)- Neotectonics <strong>of</strong> the<br />

southern <strong>Sumatra</strong>n Forearc. Proc. 36th Ann.Conv. Indon. Petrol. Assoc. IPA, Jakarta, IPA12-G-074, p. 1-10.<br />

Mulhadiono (1976)- Depositional study <strong>of</strong> the Lower Keutupang sandstone in the Aru area, North <strong>Sumatra</strong>.<br />

Proc. 5 th Ann. Conv. Indon. Petrol. Assoc., p. 115-132.<br />

(U Miocene Lower Keutupang sands in coastal and shallow marine facies. Sourced from SE (Barisan Mts))<br />

Mulhadiono & S. Asikin (1989)- The pull-apart basin <strong>of</strong>fshore Bengkulu promises attractive exploration<br />

ventures. In: B. Situmorang (ed.) Proc. 6th Reg. Conf. <strong>Geology</strong>, Mineral and Hydrocarbon Res. Southeast Asia,<br />

Jakarta, 1987, IAGI, p. 271-289.<br />

(Bengkulu <strong>of</strong>fshore forearc basin probably Oligo-Miocene pull apart feature that may be attractive for<br />

exploration. Nine wells by Marathon and Aminoil, mostly away from kitchen areas. Oil and gas shows in wells,<br />

and seeps around Bengkulu town. Early and Late or Middle Miocene carbonates. Oligocene volcanics<br />

‘basement’. Traditionally thought to be ‘cold’ basin, but wells suggest normal T gradients ?)<br />

Mulhadiono, P. Hartoyo & P.A. Soedaljo (1978)- The Middle Baong Sandstone Unit as one <strong>of</strong> the most<br />

productive units in the Aru area, North <strong>Sumatra</strong>. Proc. 7 th Ann. Conv. Indon. Petrol. Assoc., p. 107-132.<br />

<strong>Bibliography</strong> <strong>of</strong> <strong>Indonesia</strong> <strong>Geology</strong> v. 4.1 69 www.vangorselslist.com July 2012

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