Larvikite: Difference between revisions
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{{short description|An igneous rock, specifically a variety of monzonite}} |
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[[File:Larvikite.jpg|thumb|Larvikite from Larvik, Norway]] |
[[File:Larvikite.jpg|thumb|Larvikite from Larvik, Norway]] |
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[[File:Larvikite quarry Larvik.jpg|thumb|Larvikite quarry, [[Larvik]], 2008.]] |
[[File:Larvikite quarry Larvik.jpg|thumb|Larvikite quarry, [[Larvik]], 2008.]] |
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Revision as of 06:58, 20 October 2018
_Larvik_Batholith_Norway.jpg)
Larvikite is an igneous rock, specifically a variety of monzonite,[1] notable for the presence of thumbnail-sized crystals of feldspar. These feldspars are known as ternary because they contain significant components of all three endmember feldspars.[1] The feldspar has partly unmixed on the micro-scale to form a perthite, and the presence of the alternating alkali feldspar and plagioclase layers give its characteristic silver blue sheen (Schiller effect, labradorescence) on polished surfaces. Olivine can be present along with apatite, and locally quartz. Larvikite is usually rich in titanium, with titanaugite and/or titanomagnetite present.
Larvikite occurs in the Larvik Batholith (a.k.a. Larvik Plutonic Complex), a suite of 10 igneous plutons emplaced in the Oslo Rift (Oslo Graben) surrounded by ~1.1 billion year old Sveconorwegian gneisses. The Larvik Batholith is of Permian age, about 292–298 million years old.[2] Larvikite is also found in the Killala Lake Alkalic Rock Complex near Thunder Bay in Ontario, Canada.[3]
The name originates from the town of Larvik in Norway, where this type of igneous rock is found. Many quarries exploit larvikite in the vicinity of Larvik.
Formation
Intrusions of larvikite in Norway form part of the suite of igneous rocks that were emplaced during the Permian period, associated with the formation of the Oslo Rift. The crystallisation of a ternary feldspar indicates that this rock began to crystallise under lower crustal conditions.[1]
Uses
Larvikite is prized for its high polish and the labradorescence of its feldspar crystals, and is used as dimension stone, often cladding the facades of commercial buildings and corporate headquarters.[1] It is known informally as Blue Pearl Granite, although this is not an accurate description.
References
- ^ a b c d Ramberg, I. B., Bryhni, I., Nottvedt, A. and Rangnes, K. (editors) (2008). The Making of a Land: Geology of Norway. Trondheim: Norsk Geologisk Forening (Norwegian Geological Association). p. 268. ISBN 978-82-92-39442-7.
{{cite book}}:|author=has generic name (help)CS1 maint: multiple names: authors list (link) - ^ Larvikite geology
- ^ Sage, R.P. (1988). Geology of Carbonatite - Alkalic Rock Complexes in Ontario: Killala Lake Alkalic Rock Complex, District of Thunder Bay, Ontario Geological Survey Study 45 (PDF). Toronto: Ontario Geological Survey and the Ministry of Northern Development and Mines. pp. 9–18. ISBN 0-7729-0580-0.
External links
- Petrogenesis of the Oslo Region Larvikites and Associated Rocks (abstract) Journal of Petrology, 1980, volume 21, Number 3, pages 499-531
- Structure of the larvikite-lardalite complex, Oslo-region, Norway, and its evolution (abstract) International Journal of Earth Sciences, 1978, volume 67, number 1, pages 330-342
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