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Rajang River

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Series: SEPM Special Publication
Published: 01 January 2003
DOI: 10.2110/pec.03.76.0071
EISBN: 9781565762138
...Introduction Physiographic Setting, Climate, and Previous Work Fig. 1.— Map of Sarawak, East Malaysia, showing the locations of the major peat-forming regions and all peat deposits greater than 1 m thick (from Staub et al., 2000 ). The location of the Rajang River delta, the drainage...
FIGURES | View All (17)
Journal Article
Journal: Palynology
Published: 01 October 1997
Palynology (1997) 21 (1): 145–172.
Journal Article
Journal: PALAIOS
Published: 01 June 1996
PALAIOS (1996) 11 (3): 266–279.
Image
FIGURE 6 —Exposed lateral channel barform in the Lassa <span class="search-highlight">River</span>, <span class="search-highlight">Rajang</span> <span class="search-highlight">River</span> ...
Published: 01 December 2004
FIGURE 6 —Exposed lateral channel barform in the Lassa River, Rajang River delta, Sarawak. (A) Photomosaic of the exposed barform on October 19, 1992, with CWD concentrated in the dune troughs. Tandjung Sidau is the forested area in the upper left; photograph looking North. (B) Coarse woody
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The island of Borneo on which the <span class="search-highlight">Rajang</span> <span class="search-highlight">River</span> Delta is located. A) The Raj...
Published: 01 November 2012
FIGURE 2 The island of Borneo on which the Rajang River Delta is located. A) The Rajang River Delta (outlined) in Sarawak, East Malaysia, receives its discharge from the Borneo Central Massif (gray), and empties in the South China Sea. B) Map showing the location of the distributary channels
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Location maps of the <span class="search-highlight">Rajang</span> <span class="search-highlight">River</span> Delta, Sarawak, East Malaysia. A) Sites w...
Published: 01 November 2012
FIGURE 7 Location maps of the Rajang River Delta, Sarawak, East Malaysia. A) Sites where water-column (surface and depth), bottom grab samples, or both were collected that form the basis of the study. B) Distribution map of bottom sediment, grain-size fractions as determined from grab samples
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Distribution of palynomorph concentrations across the <span class="search-highlight">Rajang</span> <span class="search-highlight">River</span> Delta du...
Published: 01 November 2012
FIGURE 8 Distribution of palynomorph concentrations across the Rajang River Delta during the dry season sampling in July–August 1992. The demarcation between fresh-water and salt-water (estuarine) areas in the delta marks the landward limit of mangrove taxa along channel margins. A) Concentration
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FIGURE 3 —Locality map of the <span class="search-highlight">Rajang</span> <span class="search-highlight">River</span> delta, Sarawak, East Malaysia. T...
Published: 01 December 2004
FIGURE 3 —Locality map of the Rajang River delta, Sarawak, East Malaysia. The lateral channel bar exposed at low tide on which Coarse Woody Debris (CWD) was analyzed occurs east of Tandjung Sidau, adjacent to Tg. Pandan (insert). Tidal-range data for October 18 th and 20 th , 1992, the days before
Journal Article
Journal: PALAIOS
Published: 01 November 2012
PALAIOS (2012) 27 (11): 798–810.
...FIGURE 2 The island of Borneo on which the Rajang River Delta is located. A) The Rajang River Delta (outlined) in Sarawak, East Malaysia, receives its discharge from the Borneo Central Massif (gray), and empties in the South China Sea. B) Map showing the location of the distributary channels...
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Journal Article
Journal: PALAIOS
Published: 01 December 2004
PALAIOS (2004) 19 (6): 587–597.
...FIGURE 6 —Exposed lateral channel barform in the Lassa River, Rajang River delta, Sarawak. (A) Photomosaic of the exposed barform on October 19, 1992, with CWD concentrated in the dune troughs. Tandjung Sidau is the forested area in the upper left; photograph looking North. (B) Coarse woody...
FIGURES | View All (10)
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Proportion of mangrove taxa identified in sediment samples in the brackish ...
Published: 01 November 2012
FIGURE 11 Proportion of mangrove taxa identified in sediment samples in the brackish and fresh-water collection sites in the Rajang River Delta during the dry season. Collection sites are labeled as R*; N in the each pie diagram represents the number of mangrove pollen grains and spores counted
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Two interpretive plan-view maps in Unit 6.  A)  The type of channels observ...
Published: 01 January 2017
part of the study area were eroded off by the latest deep incision of Unit 7. Paleocurrent directions are represented by rose diagram for each part of this unit. C) A part of a combination of time and coherence slice illustrating a large low-sinuosity channel. D) A part of the modern Rajang River
Journal Article
Published: 01 June 1998
Journal of the Geological Society (1998) 155 (3): 509–524.
... (1989) has previously suggested a proto-Mekong river system fed the Rajang Embaluh Group basin. Further work is in progress on the sandstone provenance in Borneo. Structural development Southeasterly dips (Fig. 6a) in the western part of the study area swing progressively to south-southwest toward...
Series: Geological Society, London, Special Publications
Published: 01 January 2017
DOI: 10.1144/SP444.12
EISBN: 978-1-78620-374-8
... demonstrate that cycle II consists of a tide-dominated delta system that is partly analogous to the modern Rajang Delta and Lupar Embayment of southern Sarawak. Fluvio-tidal channel and tide-dominated delta successions represent periods of river-fed progradation. Wave-dominated shoreface and barrier lagoon...
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Journal Article
Published: 01 July 2000
Journal of the Geological Society (2000) 157 (4): 783–793.
... and deserving of wider attention ( Fig. 1). It is constructed of Oligocene–Lower Miocene sandy turbiditic flysch, elevated to 1800 m in the Crocker Range; intruded by the granitoid stock of Mount Kinabalu, which rises spectacularly to 4101 m, the highest peak in SE Asia. The Late Cretaceous–Eocene Rajang Group...
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Journal Article
Published: 01 February 2010
Petroleum Geoscience (2010) 16 (1): 3–29.
... are predominantly composed of the Rajang-Embaluh Group, a thick succession of strongly deformed Upper Cretaceous to Palaeogene deep-water clastic deposits that crop out in a series of belts from Kalimantan to northern Sabah ( Tate 2001 and references therein). Early workers lacking concrete field evidence...
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Journal Article
Published: 01 January 2008
Journal of the Geological Society (2008) 165 (1): 353–366.
... of the data reviewed above are as follows. (1) By the Oligocene, the northern part of the Rajang Group was uplifted sufficiently to form a sediment source for basins further north. During the Early and Middle Miocene this area grew, apparently propagating to the north and probably linking with an island chain...
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Journal Article
Journal: PALAIOS
Published: 01 May 2011
PALAIOS (2011) 26 (5): 264–274.
... and Paleoecological Analyses , Dowden, Hutchinson & Ross, Inc Stroudsburg , Pennsylvania p.. 171 – 183 . Staub , J. R. , Among , H. L. , and Gastaldo , R. A. , 2000 , Seasonal sediment transport and deposition in the Rajang River delta, Sarawak, East Malaysia : Sedimentary Geology , v. 133...
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Journal Article
Published: 04 October 2022
Environmental & Engineering Geoscience (2022) 28 (4): 347–360.
.... The study area covered three different sites near the estuaries of Rajang River in the Sarawak region of northern Borneo, Malaysia: Muara Lassa (location 1, 2°26′48″ N., 111°31′24″ E.), Batang Paloh (location 2, 2°22′4″ N., 111°25′47″ E.), and Batang Rajang (location 3, 2°11′22″ N., 111°33′50″ E...
Journal Article
Journal: Interpretation
Published: 10 June 2020
Interpretation (2020) 8 (3): T555–T567.
... Miocene, and neritic/bathyal facies during the Late Miocene to Quaternary ( Wang et al., 2000 ; Zhang et al., 2003 ; Yang et al., 2015 ). The Zengmu Basin in the northern margin of Borneo has developed delta facies since the Oligocene. The Rajang Delta, which has developed from the large Rajang River...
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