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Viqueque Formation

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Journal Article
Published: 01 March 1968
Journal of Sedimentary Research (1968) 38 (1): 271–273.
Journal Article
Published: 01 March 1967
Journal of Sedimentary Research (1967) 37 (1): 5–11.
...M. G. Audley-Charles Abstract The silt-clay matrix of the greywackes in the Viqueque Formation of Timor is considered to be an original detrital deposit and not the result of post-depositional diagenesis of sand grains. These late-Tertiary greywackes from Timor are associated with calcilutites...
Image
A: Plate boundary setting of the island of Timor. Faults follow  Hinschberg...
Published: 01 February 2013
—Sulawesi; WT—Wetar thrust; WS—Wetar suture. B: Topography and distribution of the Synorogenic Megasequence (SM) in Timor-Leste. C: Viqueque (Vqq) area, showing location of the type section of the Viqueque Formation and orientation of paleocurrent indicators (arrows). BP—Batu Putih Formation; VF—Viqueque
Image
Permian to present stratigraphy of Savu compared with that of Timor. Most o...
Published: 01 June 2009
Figure 4. Permian to present stratigraphy of Savu compared with that of Timor. Most of the Australian continental units found on Savu are correlative with the Babulu, Wai Luli, and Viqueque Formations of Timor. Palynomorph data from the Wai Luli Formation on Savu indicate an age of Kimmeridgian
Journal Article
Journal: Geology
Published: 01 February 2013
Geology (2013) 41 (2): 179–182.
...—Sulawesi; WT—Wetar thrust; WS—Wetar suture. B: Topography and distribution of the Synorogenic Megasequence (SM) in Timor-Leste. C: Viqueque (Vqq) area, showing location of the type section of the Viqueque Formation and orientation of paleocurrent indicators (arrows). BP—Batu Putih Formation; VF—Viqueque...
FIGURES | View All (4)
Image
Tectono-stratigraphic diagramm of West Timor. 1. Plio-Quaternary deposits o...
Published: 01 November 2013
(Unit 4, group G7, sub-autochthon), 5. Aileu complex of East Timor (Unit 4, group G7, sub-autochthon), 6. Viqueque group (Unit 4, group G8, sub-autochthon), 7. Dioritic intrusions (Unit 4, group G8, sub-autochthon), 8. Batuputih formation and Bobonaro conglomeratic complex (Unit 4, group G6, sub
Journal Article
Published: 01 November 2013
Bulletin de la Société Géologique de France (2013) 184 (6): 569–582.
... (Unit 4, group G7, sub-autochthon), 5. Aileu complex of East Timor (Unit 4, group G7, sub-autochthon), 6. Viqueque group (Unit 4, group G8, sub-autochthon), 7. Dioritic intrusions (Unit 4, group G8, sub-autochthon), 8. Batuputih formation and Bobonaro conglomeratic complex (Unit 4, group G6, sub...
FIGURES | View All (6)
Journal Article
Journal: AAPG Bulletin
Published: 01 November 1986
AAPG Bulletin (1986) 70 (11): 1729–1741.
..., as are the outer slopes ofthe island. Dominant among the blocks are fragments of Upper Triassic sandstone and Permian red clay ironstone, but theyalso include cross-bedded volcaniclastic sandstones of the Pliocene-Pleistocene Viqueque Formation, as well as fragmentsof Holocene coral reef and rare vein quartz...
FIGURES | View All (6)
Image
Sequential restoration of eastern cross section. No vertical exaggeration. ...
Published: 01 December 2015
of steep north side causes exhumation past muscovite 40 Ar/ 39 Ar closure; 8 km of shortening. 7.1–4.5 Ma: Duplexing of Aileu slate and much of Gondwana Sequence; steep flanks of duplex allow slumping of Kolbano to foreland and formation of Viqueque basin; out-of-sequence thrusting during duplexing allows
Journal Article
Published: 01 January 1986
Journal of the Geological Society (1986) 143 (1): 161–175.
...) Soe subsidence was a (early-middle N.23) phase of relative subsidence (it may have been in part a reflection of a eustatic sea level rise) that affected the whole island. It resulted in the widespread reef limestone deposition over the eroded Viqueque Noele Mar1 Formation. ( 5 ) Noilbesi uplift lasted...
Journal Article
Journal: Geosphere
Published: 01 December 2015
Geosphere (2015) 11 (6): 1860–1883.
... of steep north side causes exhumation past muscovite 40 Ar/ 39 Ar closure; 8 km of shortening. 7.1–4.5 Ma: Duplexing of Aileu slate and much of Gondwana Sequence; steep flanks of duplex allow slumping of Kolbano to foreland and formation of Viqueque basin; out-of-sequence thrusting during duplexing allows...
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Journal Article
Published: 01 April 1976
Journal of the Geological Society (1976) 132 (2): 179–198.
... of the bathyal sedimentary ocks having been overthrust to their present position. The youngest rocks involved in these imbri- cate thrust sheets are late Miocene (early N. I8 zone of Blow I969) planktonic calcilutites, which correlate with the lower part of the Batu Putih Limestone at the base of the Viqueque...
Image
Cartoon depicting the geodynamic evolution of Timor in 4 main steps.  a. Tr...
Published: 01 November 2013
- Viqueque group (Unit 4, group G8, autochthon), 3- Manamas complex (Unit 4, group G7, sub-autochthon), 4- Atapupu complex, (Unit 4, group G7, sub-autochthon), 5- Noetoko group (Unit 3, group G5, allochthon), 6-Cablac formation (Unit 3, group G5, allochthon), 7-Upper Miocene dioritic intrusions (Unit 4
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1979
AAPG Bulletin (1979) 63 (2): 249–251.
... Putih Limestone ( Kenyon, 1974 ) dated as N.18 to N.19. This must now be distinguished from a “reworked” Bobonaro, containing microfossils of N.18 age, which is overlain by Viqueque Group (molasse) of N.21 age. This distinction was not made in the original description of the Bobonaro by Audley-Charles...
FIGURES
Series: Geological Society, London, Special Publications
Published: 01 January 2005
DOI: 10.1144/GSL.SP.2005.250.01.16
EISBN: 9781862394988
... to Upper Pliocene 300 Poorly sorted sandy conglomerate with a dark red lateritic crust - - Lari Guti Limestone Upper Miocene to Upper Pliocene 75 Sequence of yellow calcarenites and thin coral reef rocks Biocalciclastic limestone Chemical industry, lime Viqueque Formation Upper Miocene...
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Journal Article
Journal: Geosphere
Published: 01 June 2009
Geosphere (2009) 5 (3): 152–171.
...Figure 4. Permian to present stratigraphy of Savu compared with that of Timor. Most of the Australian continental units found on Savu are correlative with the Babulu, Wai Luli, and Viqueque Formations of Timor. Palynomorph data from the Wai Luli Formation on Savu indicate an age of Kimmeridgian...
FIGURES | View All (13)
Journal Article
Published: 13 December 2023
Journal of the Geological Society (2024) 181 (1): jgs2023-079.
... ‘Néocrétacé et Tertaire Les Calcaires Fatu’ Jurassic Baguia Formation Upper Cretaceous Borolalo Limestone Banda Terrane (Forearc) + Banda Mélange ( Harris 2011 ) Fine-grained limestone of varying colour with pelagic microfauna ( Globotruncana of Late Cretaceous; Globorotalia of Eocene) Oligocene...
FIGURES | View All (12)
Series: Geological Society, London, Special Publications
Published: 01 January 2011
DOI: 10.1144/SP355.12
EISBN: 9781862396036
.... Principal features of Timor geology simplified after Standley & Harris (2009) . Line AB is shown on Figure  8 . Banda Sea volcanic rocks are part of the Banda Terrane. The Gondwana mega-sequence shown here includes the Bobonaro Melange, its related broken formation facies, matrix mixed facies...
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Journal Article
Journal: AAPG Bulletin
Published: 01 April 2016
AAPG Bulletin (2016) 100 (4): 565–595.
... reactivation of the Malita graben. In the center of the ISB, carbonate aggradation resulted in the formation of isolated carbonate platforms separated by deeper water seaways and interplatform areas. Wider and more numerous carbonate platforms developed on the edges of the ISB. During the late Quaternary...
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Series: Geohazards in Indonesia
Published: 01 January 2017
EISBN: 9781862399709
... in the Supplementary material to this paper. For ease of comparison and consistency, the English translation is formatted and paginated in the same way as the original document. Footnotes with abbreviations used and works commonly cited are included with the translation. The Index, containing mostly locations...