Abstract Views :180 |
PDF Views:142
Authors
Affiliations
1 Regional Research Laboratory, Pappanamcode. Trivandrum, IN
2 Centre for Earth Science Studies, Trivandrum 695031, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 30, No 3 (1987), Pagination: 239-243
Abstract
SEM and DT A investigations of the clays from the famous clay mine at Kundara show that kaolinite and halloysite constitute the clay minerals, and that halloysite is transformed into well-crystalline kaolinite. This indicates that kaolinite formation is preceded by the formation of halloysite in the weathering crust at Kundara. This finding is consistent with the recent experimental results of halloysite-kaolinite transformation.
Full Text