Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology
Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology
Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology
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(Substantial portion <strong>of</strong> <strong>Sumatra</strong>n oblique convergence accommodated by <strong>Sumatra</strong>n fault. 1900 km-long active<br />
strike-slip fault, 20 major segments, which range in length from about 60 to 200 km. Slip rates along fault<br />
increase NW-ward, from ~ 5 mm/yr around <strong>Sunda</strong> Strait to 27 mm/yr around Toba Lake)<br />
Natsir, M., T. Nasiruddin & N. Hasani (2010)- Rejuvenation <strong>of</strong> Niru: an integrated subsurface re-interpretation.<br />
Proc. 34 th Ann. Conv. Indon. Petrol. Assoc., IPA10-G-103, 8p.<br />
(S <strong>Sumatra</strong> Niru field 1949 BPM discovery on flank Limau anticlinorium. Peak production <strong>of</strong> 6000 BOPD<br />
reached in 1958. 2006 step-out drilling found additional reservoir on flank, significantly increasing production)<br />
Nayoan, G.A.S., D. Arpandi & M. Sumawa (1984)- Geological notes on hydrocarbon occurences in the<br />
carbonate rocks <strong>of</strong> the Belumai Formation, North <strong>Sumatra</strong>, <strong>Indonesia</strong>. In: The hydrocarbon occurrence in<br />
carbonate rocks, Proc. Joint ASCOPE/CCOP workshop, Surabaya 1982, ASCOPE, Jakarta, p. 383-405.<br />
Neeb, E.A. (1902)- Verslag omtrent het onderzoek naar tinertsafzettingen in een gedeelte van Midden- <strong>Sumatra</strong>,<br />
omvattende de landschappen V. Kota, III. Kota Kampar, IV. Kota di Mudik, VII. Kota Kampar di Ilir, Rokan<br />
Kiri, IV. Kota, Kunto, Ramba, Dalu-Dalu, Kampennan en aangrenzende streken. Jaarboek Mijnwezen Nederl.<br />
Oost-Indie 31 (1902), p. 113-145.<br />
('Report on the investigation <strong>of</strong> tin ore deposits in a part <strong>of</strong> C <strong>Sumatra</strong>, in the areas <strong>of</strong> Kota, Kota Kampar, etc.'.<br />
Concludes that, despite some local exploitation, there are no commercial tin deposits in this part <strong>of</strong> C <strong>Sumatra</strong>.<br />
With two 1:100,000 scale geologic maps <strong>of</strong> Upper Kampar, Rokan Kiri rivers areas)<br />
Nelson, H. F., M. Abdullah, C.F. Jordan & A.J. Jenik (1982)- Petrography <strong>of</strong> the Arun gas field, Aceh Province,<br />
<strong>Indonesia</strong>. In: Joint ASCOPE/CCOP Workshop on hydrocarbon occurrences in carbonates, Surabaya 1982, 38<br />
p.<br />
Newcomb, K.R. & W.R. McCann (1987)- Seismic history and seismotectonics <strong>of</strong> the <strong>Sunda</strong> arc. J. Geophys.<br />
Res. 92, p. 421-439.<br />
Nicholson, R.A. & S. Soekapradja (1990)- Organic geochemical studies in the North <strong>Sumatra</strong> Basin. In:<br />
Scientific contribution on petroleum science and technology, Spec. Publ. LEMIGAS, Jakarta, p. 45-67.<br />
Ninkovich, D. (1976)- Late Cenozoic clockwise rotation <strong>of</strong> <strong>Sumatra</strong>. Earth Planet. Sci. Lett. 29, p. 269-275.<br />
(Clockwise rotation <strong>of</strong> <strong>Sumatra</strong> <strong>of</strong> ~20° about axis near <strong>Sunda</strong> Strait inferred from: (1) <strong>Sumatra</strong> volcanic arc at<br />
angle <strong>of</strong> 20° with volcanic arc farther E; (2) Beni<strong>of</strong>f zone maximum depth <strong>of</strong> 600 km E <strong>of</strong> <strong>Sunda</strong> Strait, but<br />
decreases to 200 km NW along <strong>Sumatra</strong> island; (3) age <strong>of</strong> volcanic activity younging to NW (?))<br />
Ninkovich, D., N.J. Shackleton, A.A. Abdel-Monem, J.D. Obradovich & G. Izett (1978)- K-Ar age <strong>of</strong> the<br />
Pleistocene eruption <strong>of</strong> Toba, North <strong>Sumatra</strong>. Nature 276, p. 574-577.<br />
(Late Pleistocene eruption <strong>of</strong> Toba is largest explosive eruption documented from Quaternary. K–Ar dating <strong>of</strong><br />
the uppermost Toba Tuff gives age <strong>of</strong> ~ 75,000 yr)<br />
Ninkovich, D., R.S.J. Sparks & M.T. Ledbetter (1978)- The exceptional magnitude and intensity <strong>of</strong> the Toba<br />
eruption, <strong>Sumatra</strong>: an example <strong>of</strong> the use <strong>of</strong> deep-sea tephra layers as a geological tool. Bull. Volcanologique<br />
41, p. 285-298.<br />
Nishimura, S., E. Abe, J. Nishida, T. Yokoyama, A. Dharma, P. Hehanussa & F. Hehuwat (1984)- A gravity<br />
and volcanostratigraphic interpretation <strong>of</strong> the Lake Toba region, North <strong>Sumatra</strong>, <strong>Indonesia</strong>. Tectonophysics,<br />
109, p. 253-261, 265-272.<br />
Nishimura, S. & H. Harjono (1992)- The Krakatau Islands: the geotectonic setting. GeoJournal 28, p. 87-98.<br />
(<strong>Sunda</strong> Strait transitional zone between Java frontal and <strong>Sumatra</strong> oblique subductions. Krakatau complex at<br />
intersection <strong>of</strong> two graben zones and N-S active fracture zone with fissure extrusion <strong>of</strong> alkali basaltic rocks<br />
commencing at Sukadana and continuing S as far as Panaitan island through Rajabasa, Sebuku and Krakatau)<br />
<strong>Bibliography</strong> <strong>of</strong> <strong>Indonesia</strong> <strong>Geology</strong> v. 4.1 73 www.vangorselslist.com July 2012