Clay Minerals in the Weathering Profile of a Quartz-Muscovite Schist in the Seremban area, Negeri Sembilan
X-ray diffractograms show that randomly interstratified illite-montmorillonite and kaolinite are the clay minerals present in the upper morphological horizons of the weathering profile, while illite is the only clay mineral present in the lowest morphological horizon. In the intermediate morphologi...
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| Format: | Article |
| Language: | English |
| Published: |
Universiti Putra Malaysia Press
1993
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| Online Access: | http://psasir.upm.edu.my/id/eprint/3095/1/Clay_Minerals_in_the_Weathering_ProFile_of_a_Quartz-Muscovite_Schist.pdf http://psasir.upm.edu.my/id/eprint/3095/ http://www.pertanika.upm.edu.my/Pertanika%20PAPERS/JTAS%20Vol.%2016%20(2)%20Aug.%201993/09%20JTAS%20Vol.16%20(2)%201993%20(Pg%20129-136).pdf |
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Internet
http://psasir.upm.edu.my/id/eprint/3095/1/Clay_Minerals_in_the_Weathering_ProFile_of_a_Quartz-Muscovite_Schist.pdfhttp://psasir.upm.edu.my/id/eprint/3095/
http://www.pertanika.upm.edu.my/Pertanika%20PAPERS/JTAS%20Vol.%2016%20(2)%20Aug.%201993/09%20JTAS%20Vol.16%20(2)%201993%20(Pg%20129-136).pdf