Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

(Structure and stratigraphy of trench slope basins W of Nias Island)
Stockmal G.S. (1983)- Modeling of large-scale accretionary wedge deformation. J. Geoph. Res. 88, B10, p.
8271-8287.
(Physical modeling of accretionary wedge deformation, loosely based on C Sumatra forearc)
Streiff, A. (1877)- Over petroleum van de afdeeling Lematang Ilir, Res. Palembang. Natuurk. Tijdschrift
Nederl. Indie 37, p. 238-240.
('On petroleum of the Lematang Ilir department, Palembang residency', Early description of two S Sumatra oil
seeps, in area subsequently explored by 'Muara Enim Petroleum Co' which became part of Royal Dutch/ Shell)
Subagyo Pramumijoyo & M. Sebrier (1991)- Neogene and Quaternary fault kinematics around the Sunda Strait
area, Indonesia. J. Southeast Asian Earth Sci. 6, 2, p. 137-145.
Subandrio, A.S. (2006)- The possibility Archean- Proterozoic sedimentary rocks in Indonesian island arc related
to controversial discovery of banded iron formation (BIF) in Tanggumas, Lampung. Proc. 35 th Ann. Conv.
Indon. Assoc. Geol. (IAGI), Pekanbaru, 20p.
(Banded Iron ore Formation deposits generally associated with old craton or shield of Archaen- Proterozoic
age. First discovery of thin 'BIF-like' outcrops in Tanggamus area of Lampung, SE Sumatra, presumably in
Permian magmatic arc deposits. Characterized by intercalation of laminations meta-quartzite and iron oxide.
Two different kinds of iron formation recognized)
Subandrio, A.S. (2007)- Indonesian Banded Iron Formation (BIF): a controversial in age and tectonic setting of
BIF formation in Tanggamus area- Lampung, South Sumatra. Proc. Joint Conv. 32 nd HAGI, 36 th IAGI and 29 th
IATMI, Bali 2007, JCB2007-024, p. 1-12.
(Banded Iron Formation mineralization in Tanggamus area, Lampung, presumably associated with Permian-
Cretaceous magmatism. Classified on Algoma type iron formation, rel. small, and associated with submarine
rift hydrothermalism. Oldest rock units in S Sumatra Permian (286-248 Ma))
Subandrio, A.S., R. Gatzweiler & G. Friedrich (2007)- Relationship between magnetite- ilmenite series and
porphyry copper-tin metallogenic province of Sumatra Island- with special aspects of Sibolga and Bangka
granitoid complex. Proc. Joint Conv. 32 nd HAGI, 36 th IAGI and 29 th IATMI, Bali 2007, JCB2007-027 p. 1-10.
(Sibolga granitoid plutons in area of 50 x 50 km2 along W coast of N Sumatra, intruded into Kluet Fm.
Radiometric ages 257±24 Ma (K/Ar, biotite; late Permian) and 217.4±4.4 Ma (Rb/Sr, biotite; Triassic). Mainly
A-type biotite granites. Most Sibolga igneous rocks in Magnetite-Series, different from SE-Asia/ Bangka tin
granites, which fall in I & S-type, Ilmenite-Series)
Subandrio, A.S. & R. Soeria-Atmadja (1995)- Petrologic relations and Uranium distribution in the Sibolga
granitoid complex, North Sumatra, Indonesia. Eighth Reg. Congr. Geology, Mineral and Energy Resources of
Southeast Asia, GEOSEA 95, Manila 1995, 19p.
Subandrio, A.S., A. Sudradjat, M.F. Rosana & I. Syafri (2010)- Uranium mineralisation hosted by albite-rich
granitoid rocks of Sibolga- North Sumatra. Proc. 39th Ann. Conv. Indon. Assoc. Geol. (IAGI), Lombok, PIT-
IAGI-2010-266, 15p.
(On uranium mineralisation in albite-rich granitoids of Permo-Carboniferous crystalline- metasedimentary
Tapanuli Group)
Subandrio, A.S. & M.E. Suparka (1994)- Petrological and geochemical characteristics of A-type Sibolga
granitoid rock, North Sumatra, Indonesia. Proc. 23rd Ann. Conv. Indon. Assoc. Geol. (IAGI), Jakarta, 1, p. 334-
354.
Subandrio, A.S. & K.N. Tabri (2006)- Indonesian Banded Iron Formation (BIF): a new controversial discovery
of BIF deposit associated with island arc system in Tanggamus Area- Lampung, South Sumatra. Jurnal
Geoaplika 1, 1, p. 55-70. (online at http://fosi.iagi.or.id/bsarchives/geoaplika_55_70_2006.pdf)
Bibliography of Indonesia Geology v. 4.1 94 www.vangorselslist.com July 2012