gneiss

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Примери за gneiss

  • Here we describe the colonization of heavily shocked gneiss by heterotrophic bacteria in a natural setting.

  • The country rock was typically coarse crystalline granite gneiss, strongly weathered, ventifacted, and partly polished, and outcrops were 'crumbled' and without strength.

  • In weakly deformed gneiss, the mafic minerals (biotite, augite and hornblende) occur as irregular clusters, locally separated from plagioclase by coronas of garnet.

  • Samples from the normal smooth surface of the gneiss boulder show that the surface has been ground and polished during glacial transportation.

  • These gneisses have been multiply deformed at granulite-facies conditions.

  • In general, eclogites are predominantly mafic and are preserved as boudins within felsic gneisses.

  • These pass up into a 150 m thick homogeneous granite that is bound by planar surfaces parallel to the foliation in the underlying gneiss.

  • The kinematic evidence is interpreted to mean that the contact between the gneiss and the biotite schist has a normal-shear (hangingwall down) geometry.

  • To the south, the meta-gabbro is bounded by felsic gneiss.

  • There is a continuum apparent between the amphibolites and intermediate gneisses, whilst the felsic gneisses form a separate, high-silica group.

  • However, few recognizable trends are apparent within the data clusters for the siliceous gneisses.

  • In thin-sections, the gneisses are cut by narrow pressure solution seams and narrow cataclastic shear zones.

Значение на gneiss

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