2012
DOI: 10.1016/j.jas.2012.04.005
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Unearthing an Atlantean myth in Angkor: geoarchaeological investigation of the ‘underwater road’ crossing the Tonle Sap Lake, Cambodia

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Cited by 2 publications
(2 citation statements)
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“…Indeed, the disconformity can be traced across the entire Tonlé Sap lake, with the facies above this surface characterised by parallel-bedded sediments that contain individual point reflectors (Table 1; labelled 'p' in Figures 2 and 3B). These point reflectors likely represent siderite concretions (Pottier et al, 2012) or accumulations of the Asiatic clam Corbicula fluminaea (Penny, 2006) that are commonly found in the upper layer of the Tonlé Sap lake sediments. If the thickness of the parallel reflectors in Facies 3 that are truncated by the erosion surface are examined (Figure 2, inset X), it is evident that erosion of c. 1.2 m of lacustrine sediment must have taken place before the resumption of lacustrine sedimentation in Facies 4, a key point that is returned to below.…”
Section: Overview Of Pes Faciesmentioning
confidence: 99%
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“…Indeed, the disconformity can be traced across the entire Tonlé Sap lake, with the facies above this surface characterised by parallel-bedded sediments that contain individual point reflectors (Table 1; labelled 'p' in Figures 2 and 3B). These point reflectors likely represent siderite concretions (Pottier et al, 2012) or accumulations of the Asiatic clam Corbicula fluminaea (Penny, 2006) that are commonly found in the upper layer of the Tonlé Sap lake sediments. If the thickness of the parallel reflectors in Facies 3 that are truncated by the erosion surface are examined (Figure 2, inset X), it is evident that erosion of c. 1.2 m of lacustrine sediment must have taken place before the resumption of lacustrine sedimentation in Facies 4, a key point that is returned to below.…”
Section: Overview Of Pes Faciesmentioning
confidence: 99%
“…Sedimentation in Tonlé Sap lake due to sediment suspension settling, but after a period of widespread erosion that generated the extensive erosion surface that separates PES Facies 3 and 4 across all of the Tonlé Sap lake. Parabolic point reflections generated from diagenetic siderite concretions, of siderite and manganese (Pottier et al, 2012),, or accumulations of the clam Corbicula fluminaea (Penny, 2006) within the sediments.…”
mentioning
confidence: 99%