Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/43320
Title: Character and provenance of aeolian sediments in northeast Thailand
Authors: Nichol, JE 
Nichol, DW
Keywords: Aeolian
Geochemical analysis
Khorat plateau
Thailand
Issue Date: 2015
Publisher: Elsevier
Source: Aeolian research, 2015, v. 19, p. 5-14 How to cite?
Journal: Aeolian research 
Abstract: Aeolian activity is not generally associated with the humid tropics, and although reports of loess-like soils in various locations in southeast Asia exist, these mainly lack the detailed analysis to set them in meaningful spatial or historical context. This paper examines the red and yellow sandy sediments of the Khorat Plateau in northeast Thailand which have been variously referred to as 'cover sands', 'loessial soils' or 'loess'. The sediments are referred to as having alluvial, biological as well as aeolian origin, and a date of 9-35. ka is reported. The study compares the Khorat sediments physically and geochemically with loess and aeolian sediments from other regions, as well as with other sites in southeast Asia which are reported here. The moderate degree of particle sorting and unimodal sizes of the sediments along with a sub-spherical sub-rounded form, supports previous diagnoses of an aeolian origin. Geochemical analysis of the Khorat sediments indicates severe depletion in both mobile and immobile elements, which are even more depleted than other southeast Asian loessic soils examined. This depletion, along with the only moderate particle sorting, suggests the source of the sediments to be the local weathered sandstones outcropping around the edge of the Khorat Plateau. The dissimilarity of the Khorat sediments from Upper Continental Crust (UCC) elemental values supports this, as homogenisation would occur if diverse source areas were involved. The study suggests that aeolian sediments of humid tropical regions warrant more attention as climate proxy markers, due to the dissimilarity between the present climate and conditions required for their formation.
URI: http://hdl.handle.net/10397/43320
ISSN: 1875-9637
DOI: 10.1016/j.aeolia.2015.09.001
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