ophitic


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o·phit·ic

 (ŏ-fĭt′ĭk, ō-fĭt′-)
adj.
1. Of or relating to ophite.
2. Having a texture composed of lath-shaped plagioclase feldspar crystals in a matrix of pyroxene crystals.
American Heritage® Dictionary of the English Language, Fifth Edition. Copyright © 2016 by Houghton Mifflin Harcourt Publishing Company. Published by Houghton Mifflin Harcourt Publishing Company. All rights reserved.

ophitic

(əʊˈfɪtɪk)
adj
(Geological Science) (of the texture of rocks such as dolerite) having small elongated unorientated feldspar crystals enclosed within pyroxene grains
Collins English Dictionary – Complete and Unabridged, 12th Edition 2014 © HarperCollins Publishers 1991, 1994, 1998, 2000, 2003, 2006, 2007, 2009, 2011, 2014
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References in periodicals archive ?
Petrographically, these rocks, known as black granites in commercial market, are fine to medium-grained having ophitic to sub-ophitic texture with plagioclase and clinopyroxene as the major mineral phases, while opaques, quartz, biotite, amphibole, olivine, apatite, chlorite, orthopyroxene and epidote occur as minor to accessory phases.
The Talavera sample shows large anhedral poikilitic orthopyroxene crystals, leading to a hypidiomorphic subophitic to ophitic texture.
Basalt is medium-grained, with ophitic texture formed by plagioclase and clinopyroxene and matrix consisting of chlorite, zeolite, Ti-magnetite, titanite, ilmenite, apatite and pyrite.
Bituminous mixtures have an AC 16 S grain-size distribution with ophitic aggregate and a void percentage that depends on the filler used.
Ophitic basalt predominates In the Aberdare; its radiating crystals of feldspar recall Dandelions in seed.
Phenocryst sequence = olivine, Phenocryst sequence = olivine, augite, plagioclase such that plagioclase, augite locally plagioclase phenocrysts are less yielding ophitic and subophitic common than in tholeiites.
These zones also control the location of minor bodies of rapakivi in southern Finland and an ophitic gabbro body (Sigula) in the Tallinn zone.
Texture of the groundmass is most often ophitic. Examined granodiorite porphyries were also characterized by content of normative minerals (CIPW norm).
Most of the basalts are porphyritic and textures range from very fine-grained to very coarse-grained, using these terms in the volcanic sense (Table 1), and include ophitic, subophitic, intergranular and intersertal varieties.
The author of our greatest poetic theodicy, moreover, refuses to accept the Ophitic Gnostic notion that identified the serpent with Christ.
The flow is a coarse-grained, ophitic basalt containing heavily altered plagioclase and relatively unaltered clinopyroxene.