Interpretation of Micromorphological Features of Soils and Regoliths 2010
DOI: 10.1016/b978-0-444-53156-8.00007-6
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Cited by 38 publications
(32 citation statements)
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“…Important is the presence of many phytoliths and some volcanic glass fragments in the coarse fraction of the bleached horizons. Especially the open porphyric c/f related distribution pattern of the Bw horizons, with the strongly expressed striated b-fabric, the disorthic, nearly opaque nodules and the stress deformed clay coatings (striated orientation, locally kink-band fabric) correspond to a typical vertic material as described by Kovda and Mermut (2010). An important pedofeature of these soils are the iron oxide nodules; diffuse and moderately impregnated nodules ( Fig.…”
Section: Contentsmentioning
confidence: 91%
“…Important is the presence of many phytoliths and some volcanic glass fragments in the coarse fraction of the bleached horizons. Especially the open porphyric c/f related distribution pattern of the Bw horizons, with the strongly expressed striated b-fabric, the disorthic, nearly opaque nodules and the stress deformed clay coatings (striated orientation, locally kink-band fabric) correspond to a typical vertic material as described by Kovda and Mermut (2010). An important pedofeature of these soils are the iron oxide nodules; diffuse and moderately impregnated nodules ( Fig.…”
Section: Contentsmentioning
confidence: 91%
“…Microscopic fabrics and structures indicative of mixing due to bioturbation, human and animal trampling or pedoturbation can be observed in thin section (Banerjea et al 2013;Kooistra and Pulleman 2010;Kovda and Mermut 2010;Miller et al 2009). Gravitational settling, seasonal down profile seepage and redistribution of water can cause downward movement of fine sedimentary particles, which can also be observed using micromorphology.…”
Section: Integrated Approaches To the Study Of Sedimentation In Rocksmentioning
confidence: 95%
“…Sedimentary characteristics of semi-permanent water saturation include a prismatic structure, slickensides and redoximorphic features (mottling, Fe-Mn coatings, hypocoatings and nodules). These are more frequent in the deeper units (3a and 3b) due to their proximity to the groundwater table (Kovda and Mermut 2010;Lindbo et al 2010). The higher organic carbon content in Unit 3a may relate to its more permanent saturation conditions relative to the other sedimentary units.…”
Section: Depositional Processes and Environmentsmentioning
confidence: 99%
“…Calcite nodules are disorthic (i.e., with sharp boundaries) and rounded (Fig. 7a), features that are common in vertisols, resulting from argilliturbation (Blokhuis et al 1969;Kovda and Mermut 2010). They are commonly iron-impregnated (except for sparry domains).…”
Section: Sedimentologymentioning
confidence: 99%
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