Alteration of volcanic glass to well-crystallized ferrosaponite in the vesicles of the Deccan trap basalts at Bhuleshwar Ghat section, Pune district, Maharashtra.

Autor: Sarkar, Pradeep, Upasani, Devdutt, Wani, Vibhuti
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Zdroj: Journal of the Geological Society of India; Jul2016, Vol. 88 Issue 1, p22-28, 7p
Abstrakt: Clay minerals formed mainly by the alteration of volcanic glass are reported by many workers. The commonly formed minerals belonging to the smectite group especially nontronite and ferrosaponite are widely reported by many in basalts. However, most of the reports suggest the formation of ferrosaponite in marine conditions (Zhou et al., 1992; Chen et al., 1996) or by hydrothermal solutions (Shayan et. al., (1988)). Origin of ferrosaponite in continental flood basalts by a mechanism of alteration of volcanic glass to ferrosaponite is reported in the paper. The different stages involved in the alteration process are also highlighted. [ABSTRACT FROM AUTHOR]
Databáze: Complementary Index
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