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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along SFS. <strong>Sumatra</strong>n magmatic arc commenced at least in Mesozoic. Offset <strong>of</strong> current arc to E at Lake Toba<br />
ascribed to change in angle <strong>of</strong> Beni<strong>of</strong>f Zone, divided by split in descending plate coincident with prolongation<br />
<strong>of</strong> Investigator transform fault)<br />
Page, B.G.N. & R.D. Young (1981)- Anomalous geochemical patterns from northern <strong>Sumatra</strong>: their assessment<br />
in terms <strong>of</strong> mineral exploration and regional geology. J. Geochem. Expl. 15, p. 325-365.<br />
(Stream sediment geochemical survey in <strong>Sumatra</strong> N <strong>of</strong> 4°N. Linear high-copper zone along axial Barisan Mts,<br />
derived from ophiolites and copper-rich calc-alkaline intrusives. High chromium over ophiolites. High lead E<br />
<strong>of</strong> linear copper zone and along oil and gas basins <strong>of</strong> E coast strip. High tin values W <strong>of</strong> copper rich intrusives.<br />
Pattern does not conform to classic zonation <strong>of</strong> mineral deposits across simple subduction system)<br />
Panggabean, H. & R. Heryanto (2009)- An appraisal for the petroleum source rocks on oil seep and rock<br />
samples <strong>of</strong> the Tertiary Seblat and Lemau Formations, Bengkulu Basin. Jurnal Geol. <strong>Indonesia</strong> 4, 1, p. 43-55.<br />
(online at: http://www.bgl.esdm.go.id/dmdocuments/jurnal20090105.pdf)<br />
(Bengkulu Basin Eocene-Oligocene fore-arc basin. Oldest ‘Lahat-equivalent’ formation unconformably<br />
overlain by Oligocene-Miocene Hulusimpang Fm volcanic rocks, then by siliciclastics and minor carbonates <strong>of</strong><br />
E-M Miocene Seblat Fm. Geochemistry on selected outcrop samples and Padangcapo village oil seep indicates<br />
potential source rocks may occurred in Lahat- equivalent Seblat, and Lemau Fms)<br />
Panguriseng, M.J., E. Nurjadi, W.S. Sadirsan, B.W.H. Adibrata & D. Priambodo (2011)- Determination <strong>of</strong><br />
turbidite "lobe" distribtion and geometry in Middle baong sand, North <strong>Sumatra</strong> Basin: artificial neural network<br />
approach <strong>of</strong> multi-atribute analysis. Proc. Joint 36 th HAGI and 40th IAGI Ann. Conv., Makassar, JCM2011-<br />
389, 12p.<br />
(In <strong>Indonesia</strong>n. M Miocene Middle Baong Sand prolific reservoir in N <strong>Sumatra</strong> Basin. Deep marine sand, with<br />
lateral discontinuity major issue. Artificial Neural Network method <strong>of</strong> seismic multi-attribute analysis used for<br />
reservoir characterization and geometry analysis)<br />
Panjaitan, S. (2006)- Struktur dan geometri cekungan oil shale di daerah Taluk, Riau, berdasarkan metode gaya<br />
berat. J. Sumber Daya Geol. (GRDC), 16, 2, p. 75-93.<br />
('Structure and geometry <strong>of</strong> the oil shale basin in the area <strong>of</strong> Taluk, Riau, based on gravity method')<br />
Pannetier, W. (1994)- Diachronism <strong>of</strong> drowning event on Baturaja limestone in the Tertiary Palembang subbasin,<br />
South <strong>Sumatra</strong>, <strong>Indonesia</strong>. J. Southeast Asian Earth Sci. 10, 3-4, p. 143-157.<br />
(Oligocene-E Miocene transgression in Lahat and Talang Akar formations from W to E. Deposition <strong>of</strong> Baturaja<br />
carbonate on tectonic uplifts interpreted as lowstand system tract. Drowning <strong>of</strong> carbonate platform by Gumai<br />
shales diachronous. Carbonate drowning coincides with renewed volcanic and tectonic activities and cooling)<br />
Paramita, D. & R. Santoso (2011)- Sequence stratigraphy and facies distribution analyses to define reservoir<br />
lateral distribution in Meruap Field, Jambi. Proc. 35 th Ann. Conv. Indon. Petrol. Assoc., IPA11-G-154, 12p.<br />
(Meruap Field in Jambi Sub-basin, discovered in 1974. Main oil reservoir is sand <strong>of</strong> M Miocene Air Benakat<br />
Fm. Total oil produced 10.3 MMBO. Sequence stratigraphy study suggests five sequence boundaries. Sands<br />
deposited in deposited in tide- dominated delta, with three depositional facies: tidal channel, tidal sand bar,<br />
and tidal sand flat, with depositional trend oriented SW-NE)<br />
Pardede, R., T.C. Amin & S. Gafoer (1986)- Geologic map <strong>of</strong> the Bengkulu Quadrangle, <strong>Sumatra</strong>, 1:250,000.<br />
Geol. Res. Dev. Centre, Bandung, p.<br />
Pardede, R. & K. Brata (1984)- Geologic Map <strong>of</strong> the Sungaipenuh and Ketaun Quadrangles, <strong>Sumatra</strong><br />
(Quadrangle 0812 and 0813), 1:250,000. Geol. Res. Dev. Centre, Bandung, Open File.<br />
Permana, A.K. (2008)- Coal characteristics <strong>of</strong> Sarolangun- Pauh region: implication for coalbed methane<br />
potential. Jurnal Sumber Daya Geol. 14, 6, p. 351-360.<br />
<strong>Bibliography</strong> <strong>of</strong> <strong>Indonesia</strong> <strong>Geology</strong> v. 4.1 76 www.vangorselslist.com July 2012