Abstract
Geochemical investigations of the slip zones of a landslide in granitic saprolite revealed that they have signatures distinct from their host materials. These distinctions include stronger Si depletion, higher Al enrichment, greater LOI, significant fixations of Mn, Ba and Ce, stronger negative Eu anomalies, and greater accumulations of other rare earth elements (REE). Altogether, these geochemical characteristics indicate that: (a) the slip zones have greater abundance of clays, consistent with field and microscopic observations; (b) concentration of clay size particles within the slip zones may have been from downward leaching and deposition, and lateral transportation of Al-Si solutions and colloids through pores and fractures within the saprolite; and (c) there were prevailing oxidation and poor drainage, and occasional reduction conditions within the slip zones. It was concluded that geochemical analyses could be effective in gathering clues for understanding the development and nature of slip zones in landslide investigations.
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Acknowledgements
The work described in this paper was partially supported by a grant from the Research Grants Council of the Hong Kong Special Administrative Region, China (Project No. HKU 7002/03P). The authors acknowledge kind assistance provided by Mr. Liang Qi and the supporting staff of the Department of Earth Sciences and Electron Microscopy Unit of the University of Hong Kong in carrying out XRF, ICP-MS and EDS analyses.
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Appendix: List of Abbreviations
Appendix: List of Abbreviations
Material weathering grades within the host granitic saprolite:
CDG: Completely Decomposed Granite (Weathering Grade of V)
HDG: Highly Decomposed Granite (Weathering Grade of IV)
MDG: Moderately Decomposed Granite (Weathering Grade of III)
SDG: Slightly Decomposed Granite (Weathering Grade of IV)
Field-scale deformational divisions of the investigated landslide:
NDZ: Northern Distressed Zone
SDZ: Southern Distressed Zone
Seams differentiated within SDZ:
DGS: Dark Gray Seam (Slip Zone)
WS: White Clay Seam(s)
Exploratory excavations:
AP: Trial Pit
TT: Trial Trench
SS: Surface Strip
Techniques:
XRF: X-Ray Fluorescence Spectrometry
SEM: Scanning Electron Microscopy
ICP-MS: Inductively Coupled Plasma-Mass Spectrometry
EDS: Energy Dispersive X-Ray Spectrometry
Chemical elements/indices:
LOI: Loss on Ignition
REE: Rare Earth Element(s)
LREE: Light REE
HREE: Heavy REE
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Wen, BP., Duzgoren-Aydin, N.S. & Aydin, A. Geochemical characteristics of the slip zones of a landslide in granitic saprolite, Hong Kong: implications for their development and microenvironments. Env Geol 47, 140–154 (2004). https://doi.org/10.1007/s00254-004-1145-6
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DOI: https://doi.org/10.1007/s00254-004-1145-6