Bravo Lake Formation
The stratigraphy of the Bravo Lake Formation starts with a basic section of iron-oxide rich sandstones, psammites, and semi-pelites which cover a series of deformed pillow lavas which expand in viscosity towards the west, and volcanic/clastic deposits and ultramafic sills. The lower volcanic section is covered by garnet and diopside bearing calc–silicate layers and finely layered metasediments composed of coarse-grained actinolite, hornblende and biotite followed by pelites and semi-pelites that are intruded by separate sills. In the Ridge Lake area, the volcanic belt includes an interlayered series of amphibolite, gabbro, iron formation, sulfidic schist and metasediments.
Geochemical results of pillow lavas and chill boundaries along five transects across the volcanic belt suggest the existence of three chemically different magma types within the Bravo Lake Formation.
Lavas of the volcanic belt display geochemical characteristics similar to modern ocean-island–basalt groups. They range from moderately to intensely fractionated. REE-profiles are similar to those from tholeiitic basalts to extremely alkaline lavas in Hawaii.
See also
References
- ^ Igneous rock associations in Canada 3. Large Igneous Provinces (LIPs) in Canada and adjacent regions: 3 Retrieved on 2007-01-10
- ^ Central Baffin Island 4-D Project - Projects Archived 2009-04-16 at the Wayback Machine: Paleoproterozoic mafic magmatism in central Baffin Island. Retrieved on 2007-10-18
- ^ Volcanology and geochemistry of the Bravo Lake Formation, Baffin Island, Nunavut. Retrieved on 2007-10-18
External links
68°31′N 073°18′W / 68.517°N 73.300°W