The Bravo Lake Formation is a mafic volcanic belt and large igneous province [1] located at the northern margin of the Trans-Hudson orogeny on central Baffin Island, Nunavut, Canada. It is exposed along a nearly continuous east–west passage for 120 km (75 mi) and changes in stratigraphic thickness from 1 to 2.5 kilometers. [2] The formation is a rare alkaline-suite that formed as a result of submarine rifting during the Paleoproterozoic period. [3] The Bravo Lake Formation is surprisingly undeformed by the Himalayan-scale forming event during the Trans-Hudsonian orogeny.
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. [2]
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. [2]
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. [2]
See also
References
- ^ Igneous rock associations in Canada 3. Large Igneous Provinces (LIPs) in Canada and adjacent regions: 3 Retrieved on 2007-01-10
- ^ a b c d 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
 | This article about a specific Canadian geological feature is a stub. You can help Wikipedia by expanding it. |
 | This article about a specific stratigraphic formation in Canada is a stub. You can help Wikipedia by expanding it. |
The Bravo Lake Formation is a mafic volcanic belt and large igneous province [1] located at the northern margin of the Trans-Hudson orogeny on central Baffin Island, Nunavut, Canada. It is exposed along a nearly continuous east–west passage for 120 km (75 mi) and changes in stratigraphic thickness from 1 to 2.5 kilometers. [2] The formation is a rare alkaline-suite that formed as a result of submarine rifting during the Paleoproterozoic period. [3] The Bravo Lake Formation is surprisingly undeformed by the Himalayan-scale forming event during the Trans-Hudsonian orogeny.
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. [2]
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. [2]
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. [2]
See also
References
- ^ Igneous rock associations in Canada 3. Large Igneous Provinces (LIPs) in Canada and adjacent regions: 3 Retrieved on 2007-01-10
- ^ a b c d 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
| This article about a specific Canadian geological feature is a stub. You can help Wikipedia by expanding it. |
|
| This article about a specific stratigraphic formation in Canada is a stub. You can help Wikipedia by expanding it. |