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High temperature acid rocks associated with serpentinite in Eastern Quebec
Study of acid rocks found in highly serpentinized peridotite at Asbestos in Eastern Quebec indicates that they are metasomatically altered gabbro bodies; initial alteration was to biotite-saussurite which was further altered to microcline-diopside-albite-quartz rock; degree of alteration was dependent on structural attitude; these rocks represent high temperature alteration in amphibolite facies.
High temperature acid rocks associated with serpentinite in Eastern Quebec
Study of acid rocks found in highly serpentinized peridotite at Asbestos in Eastern Quebec indicates that they are metasomatically altered gabbro bodies; initial alteration was to biotite-saussurite which was further altered to microcline-diopside-albite-quartz rock; degree of alteration was dependent on structural attitude; these rocks represent high temperature alteration in amphibolite facies.
High temperature acid rocks associated with serpentinite in Eastern Quebec
Am J Science
Olsen, E.J. (author)
1961
19 pages
Article (Journal)
English
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