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West Timor

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Journal Article
Published: 01 November 2013
Bulletin de la Société Géologique de France (2013) 184 (6): 569-582.
... main superimposed structural units are distinguished in West Timor. The today structure is the result of three main tectonic events that occurred during the Late Oligocene, Late Early Pliocene and Late Pliocene-Early Pleistocene times, respectively. Our field investigations in the 1990 to 2000 decade...
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Journal Article
Published: 01 September 1999
Journal of Paleontology (1999) 73 (5): 765-786.
...K. Sashida; Y. Kamata; S. Adachi; Munasri Abstract Moderately well-preserved Middle Triassic radiolarians were recovered from bedded limestone exposed at about 3 km west of Kefamenanu, West Timor, Indonesia. This limestone probably from the Aitutu Formation is considered to be an allochthonous...
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a. Location of <b>West</b> <b>Timor</b> in eastern Indonesia. NBB = North Banda basin, SB...
Published: 01 November 2013
Fig. 1 a. Location of West Timor in eastern Indonesia. NBB = North Banda basin, SBB = South Banda basin, SW = West Sulawesi, SE = East Sulawesi, HL = Halmahera, TB = Tukang Besi platform, LR = Lucipara ridge, BA = Savu basin. b. Geological sketch map of West Timor [modified from Rosidi et al
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a. Crustal geological cross section of <b>West</b> <b>Timor</b> (modified from  Villeneuv...
Published: 01 November 2013
Fig. 2 a. Crustal geological cross section of West Timor (modified from Villeneuve et al. [2005] ). 1. Central basin (Unit 5, group G9), 2. Manamas complex (Unit 4, group G7), 3. Late Miocene dioritic intrusion (Unit 4), 4. Batuputih group (Unit 4, group G6), 5. Cablac formation (Unit 3, group
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Tectono-stratigraphic diagramm of <b>West</b> <b>Timor</b>. 1. Plio-Quaternary deposits o...
Published: 01 November 2013
Fig. 3 Tectono-stratigraphic diagramm of West Timor. 1. Plio-Quaternary deposits of the Noele group (Unit 5, group G9, autochthon), 2. Reef limestones of the Noele group (Unit 5, group G9, autochthon), 3. Manamas volcanic complex (Unit 4, group G7, sub-autochthon), 4. Ultrabasic Atapupu complex
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K-Ar ages carried on <b>West</b> <b>Timor</b> samples (ages were performed in Brest Unive...
Published: 01 November 2013
Table I K-Ar ages carried on West Timor samples (ages were performed in Brest University at UMR CNRS 6538 “Domaines océaniques”). Geographical coordinates: in column 2.
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Corrugatoblastus savilli  n. gen. n. sp., Early Permian, <b>West</b> <b>Timor</b>, Indone...
Published: 01 November 2013
Figure 2 Corrugatoblastus savilli n. gen. n. sp., Early Permian, West Timor, Indonesia; type specimens coated with ammonium chloride sublimate. 1–4 , summit, basal, and two side views of NHMUK EE 15361 showing ambulacra on summit, ridges and furrows on thecal side, and BB-RR sutures in 4
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—Simplified geologic map of <b>West</b> <b>Timor</b> showing location of mud volcanoes an...
Published: 01 November 1986
Figure 2 —Simplified geologic map of West Timor showing location of mud volcanoes and shale diapirs (after Rosidi et al, 1981 , with additions from Tjokrosapoetro, 1978 ). Note that unlike mud volcanoes, shale diapirs are apparently restricted to rocks younger than N20 (middle Pliocene
Series: SEPM Special Publication
Published: 01 January 2003
DOI: 10.2110/pec.03.77.0029
EISBN: 9781565762145
..., East, Central, and West Kalimantan, and Seram, to humid in Irian Jaya, to dry-subhumid in Timor and Java, among which are settings that represent the same tectonic system in two different climates. Most Indonesian rivers in our study have similar-size catchment basins and stream gradients, and all...
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Journal Article
Published: 07 September 2016
Seismological Research Letters (2016) 87 (6): 1417-1423.
...‐Leste. (b)  STS ‐2/Q330 instrumentation at station LEGO in Lelogama, West Timor, Indonesia.The color version of this figure is available only in the electronic edition. The deployment (as of June 2016) has already recorded over 600 local earthquakes with magnitude greater than M w  4.5...
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Journal Article
Published: 01 April 1997
Journal of the Geological Society (1997) 154 (2): 169-172.
...T. R. CHARLTON Abstract The recently published BIRPS BANDA deep seismic profiles across the Banda arc-continent collision complex indicate major backthrusting both internal to the volcanic arc and between the volcanic arc and forearc ridge. This is significantly different from the West Timor-Savu...
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1980
AAPG Bulletin (1980) 64 (6): 868-915.
... and the Aru and Timor Troughs is best demonstrated by the pattern of gravity anomalies. The discontinuity between the Seram and Aru Troughs supports the seismic evidence that the Seram subduction zone is separate from the Southern Banda subduction zone that is continuous with that beneath Java on the west...
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Journal Article
Published: 01 September 2017
The Canadian Mineralogist (2017) 55 (5): 875-908.
... 1979 , Keep & Haig 2010 ), and is divided into West Timor (part of the Nusa Tenggara Province of Indonesia) and Timor Leste/East Timor (an independent sovereign country) with the political boundary extending some 100 km north–south and located approximately in the center of the island ( Fig. 1 B...
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Series: Geological Society, London, Petroleum Geology Conference series
Published: 01 January 2005
DOI: 10.1144/0060861
EISBN: 9781862394124
... and the North West Shelf, although older plume activity may have some affect along parts of the North West Shelf ( Doré & Stewart, 2002 ; Müller et al. 2002 ). Fig. 8 Conceptual evolution of Neogene architecture of the Timor Sea region. Elastic amplification of deep-seated basement topology...
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Series: AAPG Hedberg Series
Published: 01 January 2005
DOI: 10.1306/1060754H23160
EISBN: 9781629810423
... jogs in the faults. Located at the southern end of the Timor Sea between the Londonderry High and the Ashmore Platform, the Vulcan Subbasin has a complex architecture comprising southwest-northeast and east-northeast-west- southwest-trending, asymmetrical, en echelon subgrabens flanked...
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Series: Geophysical Developments Series
Published: 01 January 2013
DOI: 10.1190/1.9781560803119.ch2
EISBN: 9781560803119
... to extensional reactivation and to assess hydrocarbon upfault seepage on the Laminaria High (Timor Sea, Australian North West Shelf). Fluid inclusion data are consistent with the presence of paleo-oil columns below the current accumulations in the Laminaria and Corallina fields. Evidence for other partially...
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Journal Article
Journal: AAPG Bulletin
Published: 01 April 2010
AAPG Bulletin (2010) 94 (4): 567-591.
... and to investigate hydrocarbon preservation risk for structural traps in the offshore Bonaparte Basin (Laminaria High, the Timor Sea, Australian North West Shelf). The model results show that the distributions of shear strain and dilation as well as fluid flux are heterogeneous along fault planes inferring lateral...
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Journal Article
Published: 01 December 2003
Journal of the Geological Society (2003) 160 (6): 991-1001.
... subtle sag of that graben during the late Cretaceous or early Tertiary. Timor Sea Neogene collision orogenesis The Timor Sea encompasses that portion of Australia's North West Shelf facing collision with the Eurasia–Pacific oceanic arc ( Fig. 1 ). Diachronous collision between outliers...
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Journal Article
Published: 01 March 2009
Journal of Paleontology (2009) 83 (2): 313.
... – Naturalis, Leiden (NNM), of more than 10,000 specimens of Permian fossils, mainly marine invertebrates, from West Timor, Indonesia. Together with the collections already present at Naturalis, this easily forms the largest concentration of fossils from Timor in any museum. Already present in NNM were...
Series: Geological Society Special Publications
Published: 01 January 2011
DOI: 10.1144/SP355.12
EISBN: 9781862396036
... of 75–100 km (150 km wide with its submarine southern slope). Without including the volcanic islands, East and West Timor are together larger than the 280×100 km Swiss Alps. The Banda Arcs are 2300 km long, a length equivalent to the European Alps in France, Italy, Switzerland and Austria as well...
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