Geochemistry and stable isotopic variations of water and dissolved sulfate from landslide areas in Niigata and Nagano Prefectures, Japan. A case study
Author:
Affiliation:
1. Department of Environmental Biology and Chemistry, University of Toyama
2. Research Institute for Natural Hazards & Disaster Recovery, University of Niigata
Publisher
Geochemical Society of Japan
Subject
Geochemistry and Petrology,Geophysics
Link
https://www.jstage.jst.go.jp/article/geochemj/57/2/57_GJ23008/_pdf
Reference15 articles.
1. Bogaard, T., Guglielmi, Y., Marc, V., Emblanch, C. Bertland, C. and Mudry, J. (2007) Hydrogeochemistry in landslide research: A review. Bull. Soc.Géol. Fr. 178, 113–126. https://doi.org/10.2113/gssgfbull.178.2.113
2. Chihara, K. (1974) Neogene tertiary volcanostratigraphy in the Niigata Sedimentary Basin—Tectonic Province and Volcanic Province—. J. Japanese Assoc. Petrol. Technol. 39, 201–215. (in Japanese with English abstract). https://doi.org/10.3720/japt.39.201
3. Fujita, T. (1990) Landslide (3): Geological features that lead landslide. J. Groundwater Hydrology 32, 91–100. (in Japanese). https://doi.org/10.5917/jagh1987.32.91
4. Giggenbach, W. F. (1988) Geothermal solute equilibria. Derivation of Na-K-Mg-Ca geoindicators. Geochim. Cosmochim. Acta 52, 2749–2765. https://doi.org/10.1016/0016-7037(88)90143-3
5. Japan Meteorological Agency (2020) Various meteorological data (monthly averages). (in Japanese). https://www.data.jma.go.jp/obd/stats/etrn/view/nml_amd_ym.php?prec_no=54&block_no=0529&year=&month=&day=&view=
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