A Note to the Lignite occurrence in Lukundol, Kathmandu
DOI:
https://doi.org/10.3126/jngs.v2i1.32529Keywords:
Lignites, Lukundol Formation, Quaternary fluvio-lacustrine, Kathmandu valleyAbstract
The Quaternary fluvio-lacustrme sediments of Kathmandu Valley arc characterized by the occurrence of low quality lignite. The lignites are more confined to the lower part of this deposition in the Lukundol Formation, consisting of clay, silt, sand and coarse sand. These lignites show ambivalent characters between lignite and peat.
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Published
1982-06-30
How to Cite
Tuladhar, R. M. (1982). A Note to the Lignite occurrence in Lukundol, Kathmandu. Journal of Nepal Geological Society, 2(1), 47–51. https://doi.org/10.3126/jngs.v2i1.32529
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