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Basal member [of The Straits Schist]

Basal member [of The Straits Schist] ( = Russell Mountain Formation of Massachusetts) - Distinguished by presence of layers of amphibolite, marble, calc-silicate rock, and quartzite within more uniform schist like that on either side. Minor, unevenly distributed mineralization in W, Bi, Cu, Ni, and other metals.
StateConnecticut
NameBasal member [of The Straits Schist]
Geologic ageSilurian
Original map labelStb
CommentsPart of Central Lowlands; Iapetus (Oceanic) Terrane - Connecticut Valley Synclinorium; Hartland Belt
Primary rock typeschist
Secondary rock typeamphibolite
Other rock typesmarble; calc-silicate rock; quartzite
Lithologic constituents
Minor
Metamorphic > Schist
Metamorphic > Metasedimentary > Metaclastic > Quartzite
Metamorphic > Metasedimentary > Calc-silicate-rockcalc-silicate rock
Metamorphic > Metasedimentary > Metacarbonate > Marble
Metamorphic > Amphibolite
Map references
Connecticut Geological and Natural History Survey, DEP, in cooperation with the U.S. Geological Survey, 2000, Bedrock Geology of Connecticut, data format: shapefile, file name: bedrock, downloaded from: http://magic.lib.uconn.edu/cgi-bin/MAGIC_DBsearch2.pl?Geography=37800&Loc=0000 on 9/18/2003, scale 1:50,000.
Unit references
Rodgers, John, compiler, 1985, Bedrock Geological Map of Connecticut: Connecticut Geological and Natural History Survey, Hartford, Connecticut, 2 sheets, scale 125,000.
Geographic coverageFairfield - Hartford - Litchfield - New Haven

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