METAMORPHIC CONDITIONS OF THE AUREOLE ROCKS FROM DHUNAGHAT AREA, KUMAUN LESSER HIMALAYA

Citation
M. Joshi et al., METAMORPHIC CONDITIONS OF THE AUREOLE ROCKS FROM DHUNAGHAT AREA, KUMAUN LESSER HIMALAYA, Current Science, 67(3), 1994, pp. 185-188
Citations number
12
Categorie Soggetti
Multidisciplinary Sciences
Journal title
ISSN journal
00113891
Volume
67
Issue
3
Year of publication
1994
Pages
185 - 188
Database
ISI
SICI code
0011-3891(1994)67:3<185:MCOTAR>2.0.ZU;2-J
Abstract
In Dhunaghat area of Kumaun Lesser Himalaya, Precambrian greenschist m etapelites of the Almora Group show evidence of contact metamorphism c aused by intrusion of the hot Cambrian Champawat Granitoids plutonic b ody. Mineral assemblages indicate hornblende-hornfels facies condition s of contact metamorphism. Temperatures between 600 and 650-degrees-C and pressures around 3 kb are suggested for the contact metamorphism.