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Haida Gwaii (British Columbia, Canada): a Phanerozoic analogue of a subduction-unrelated Archean greenstone belt
J. Gregory Shellnutt
*
, Jaroslav Dostal
*
Corresponding author for this work
Department of Earth Sciences (Include Institute of Marine Environmental Science and Technology)
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Article
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peer-review
6
Citations (Scopus)
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INIS
rocks
100%
volcanic rocks
100%
canada
100%
british columbia
100%
geochemistry
66%
tectonics
33%
carbonates
33%
silicon oxides
33%
crystallization
33%
magma
33%
basalt
33%
volcanoes
33%
lead isotopes
33%
sandstones
33%
triassic period
33%
andesites
33%
intrusive rocks
33%
Earth and Planetary Sciences
Phanerozoic
100%
Greenstone Belt
100%
British Columbia
100%
Canada
100%
Volcanic Rock
33%
Precambrian
33%
Tectonics
16%
Basalt
16%
Magma
16%
Mantle Source
16%
Paleogene
16%
Andesite
16%
Early Triassic
16%
Sedimentary Sequence
16%
Calc Alkaline Rock
16%
Fractional Crystallization
16%
Sandstone
16%