Meso/Micro-texture analysis of the landslide-dam outburst sediments in the Upper Jinsha River, SE Tibetan Plateau

• Published in: Geologia Croatica Vol. 72; no. Special issue; pp. 81 - 91
• Main Authors: Chen, Jian, Cui, Zhijiu, Liu, Chao, Zhou, Wendy, Chen, Ruichen
• Format: Journal Article Web Resource
• Language: English
• Published: Zagreb Institut za Geoloska Istrazivanja 01.01.2019; Hrvatskigeološkiinstitut
• Subjects: Chatter; Cracks; Crevasses; Dams; Distance; Etch pits; Floods; Fluvial deposits; Fluvial sediments; Gravel; Hydrodynamics; Laboratories; Landslides; Meandering; Microtexture; Particle size; Particle size distribution; Percussion; Quartz; Rivers; Scanning electron microscopy; Sedimentary environments; Sediments; Shape; Size distribution; Transport; Underwater; Tibetan Plateau; Jinsha River; Tibet; China
• ISSN: 1330-030X; 1333-4875
• DOI: 10.4154/gc.2019.29

Outburst sediments are widely distributed in the Upper Jinsha River in the Southeastern (SE) Tibetan Plateau. In order to understand the sedimentary characteristics of these sediments, gravel fabric, particle size distribution and quartz sand surface textures were used to analyze the mesotextures and microtextures of the Xuelongnang outburst sediments. It was determined that these sediments usually have a short transport distance, and are distributed over a distance of approximately 3.5 km. The gravel fabric and particle size distribution analysis represent the different meso-characteristics with different transport distances and suggest gradually changing hydrodynamic conditions. The statistical data of quartz surface textures exhibit the transformation process of quartz sands by outburst flood. The variation from abundant sub-angular shapes (> 75%); to common V-shaped percussion cracks, solution crevasse, medium relief, and chatter marks (50% to 75%); to rare meandering ridge, underwater polished surface, large conchoidal fracture (> 100 |jm), directional etch pits, and crystalline overgrowths (<5%), present the features in different combinations to other sedimentary environments. The microtexture characteristics of landslide-dam outburst deposits are also consistent with those of the mesotextures. As the distance from the residual dam increased, the quartz grain microtextures showed gradual or abrupt changes, such as increased frequencies of V-shaped percussion cracks, decreased frequencies of the adhering particles, and growth of the solution crevasses. These findings could potentially be used as a discriminant mark to distinguish outburst sediment from other types of sediments, e.g., subaqueous, eolian, glacial, etc.