A. Filippidis et al., NATROLITE THOMSONITE INTERGROWTHS FROM BASALTIC ROCKS OF DECCAN TRAPS(WESTERN INDIA)/, Neues Jahrbuch fur Mineralogie Monatshefte, (4), 1996, pp. 161-170
Natrolite/thomsonite intergrowths developed inside basalt cavities fro
m Deccan Traps (Western India), described for the first time, have bee
n investigated using a combination of microscopic, diffraction, spectr
oscopic and thermal techniques. The XRD and chemical analyses showed t
hat the zeolitic material consisted of natrolite and thomsonite. The S
i-29 MAS NMR and FT-IR measurements indicated the coexistence of two d
iscernible zeolite phases in the material. The main endothermic peaks
of the material were recorded at 323 degrees C, 380 degrees C and 420
degrees C. The SEM-EDS study proved that the two minerals form epitaxi
al overgrowths joined at an interface parallel to their c axes and int
ergrowths joined at an interface unparallel to the c axes. The formati
on of the two-phase natural zeolitic material is mainly attributed to
crystallographic similarities between the two phases and their crystal
lization under the same conditions.