Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

('Critical notes on the origin and precise ages of Tertiary wood fossils described from Netherlands Indies')
Nabasir, A., Andriyani S., Hendar S.M., Haruji M.P. & Subagio (1999)- Integrated study of the Telisa shaly
sand in the Bangko Field, C Sumatera Basin. Proc. 28th Ann. Conv. Indon. Assoc. Geol. (IAGI), 2, p. 59-78.
Nainggolan, D.A. (2007)- Tinjauan analisis gaya berat terhadap bentukan struktur bawah permukaan di Lembar
Medan, Sumatera Utara. Jurn. Sumberdaya Geol. 17, 4, p. 243-256.
(Interpretation of Medan sheet, N Sumatra, gravity data)
Nainggolan, D.A. & T. Padmawijaya (2003)- Studi geodinamika lajur akresi daerah Siberut dari data gayaberat.
J. Geol. Sumberdaya Min. (GRDC) 13, 143, p.
('Study of geodynamics of the accretionary prism in the Siberut area from gravity data')
Nakano, M., H. Kumagai, S. Toda, R. Ando, T. Yamashina, H. Inoue & Sunarjo (2010)- Source model of an
earthquake doublet that occurred in a pull-apart basin along the Sumatran fault, Indonesia. Geoph. J. Int. 181,
p.141-153.
(2007 earthquake doublet along Sumatran fault near Padang Panjang, C Sumatra. Focal mechanisms indicate
right-lateral strike-slip faults, consistent with geometry of Sumatran fault. Both nucleated below N end of Lake
Singkarak, which is in pull-apart basin between Sumani and Sianok segments of Sumatran fault system)
Napitupulu, H. & W.S. Sadirsan (2000)-The origin of light oil and condensates in the Musi Block- South
Sumatra Basin. AAPG Ann.Mtg. New Orleans 2000, p. (Abstract only)
(S Sumatra Basin oil, biomarker, carbon isotope analyses show hydrocarbons mainly from Talang Akar- Lahat
Fms terrestrial source rock. Light oil and condensate formed by evaporative fractionation. Oil formed and
trapped in lower formation, then light fraction migrated into overlying limestone reservoir. This process
responsible for hydrocarbons in Musi and Klingi fields, located in basement high area 20 km W of kitchen)
Nas, D.S. & J.B. Supandjono (1995)- Geological map of the Telo sheet, Sumatra, 1: 250,000. Geol. Res. Dev.
Centre, Bandung.
Nash, J.M.W. (1929)- Radiolarienhoudende gesteenten van Sumatra. De Mijningenieur 10, p. 249-255.
('Radiolarian-bearing rocks from Sumatra'. New localities with radiolarians in S Sumatra; no true radiolarites)
Nash, J.M.W. (1930)- De Trias ten zuiden van Sawah Loento. De Mijningenieur 11, 8, p. 159-164.
(‘The Triassic S of Sawahlunto’. Triassic sediments intruded by diorite porphyry in Jurassic-Cretaceous during
or after folding)
Natawidjaja, D.H. (2002)- Neotectonics of the Sumatran Fault and paleogeodesy of the Sumatran subduction
zone. Ph.D.Thesis California Inst. Technology, Pasadena, 289p.
(Online at: http://etd.caltech.edu/etd/available/etd-05222003-155554/unrestricted/DHN_Thesis.pdf. Collection
of typescripts; no figures)
Natawidjaja, D.H., K. Sieh, S.N. Ward, H. Cheng, R.L. Edwards et al. (2004)- Paleogeodetic records of seismic
and aseismic subduction from central Sumatran microatolls, Indonesia. J. Geophys. Res. 109, B04306,
doi:10.1029/2003JB002398, 34 p.
(Coral microatolls in W Sumatra used to document recent vertical deformation associated with subduction)
Natawidjaja, D.H., K. Sieh, J. Galetzka, B.W. Suwargadi, H. Cheng, R.L. Edwards & M. Chlieh (2007)-
Interseismic deformation above the Sunda Megathrust recorded in coral microatolls of the Mentawai islands,
west Sumatra, J. Geophys. Res. 112, B02404, doi:10.1029/2006JB004450, p.
Natawidjaja, D.H. & W. Triyoso (2007)- The Sumatran fault zone- from source to hazard. J. Earthquake and
Tsunami 1, 1, p. 21-47.
Bibliography of Indonesia Geology v. 4.1 72 www.vangorselslist.com July 2012