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Troctolite

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troctolite [′träk·tə‚līt]
(petrology)
A gabbro composed principally of calcic plagioclase and olivine. Also known as forellenstein.

Troctolite 

an igneous rock of the gabbro group, consisting mainly of basic plagioclase (labradorite or bytownite) and small amounts of olivine. Pyroxenes are either present in negligible amounts or completely absent. Serpentinization of the olivine is sometimes accompanied by the formation of characteristic fissures, which radiate from the olivine grains, in the plagioclase.



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1991, Syn- and post-kinematic intrusions of troctolite, gabbro, and peridotite into layered gabbroic cumulates in the Bay of Islands ophiolite: genesis of anorthosite by partial assimilation, and troctolite by hybridization: Geological Survey of Canada, Current Research, Paper 91-1, part D, p.
Bogatikov & Birkis (1973) subdivided the mafic rocks distributed in the southern part of the Riga batholith into two groups: one consists almost exclusively of anorthosites, while the other features a more complex association of rocks, including anorthosite, gabbro-anorthosite, gabbronorite, troctolite, and melatroctolite.
Troctolites are primitive cumulates, assemblages of olivine and plagioclase crystals together with a small fraction of crystallized trapped liquid, that formed during the early stages of magma crystallization.
 
 
 
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