Here we describe the colonization of heavily shockedgneissby heterotrophic bacteria in a natural setting.From theCambridge English Corpus
The country rock was typically coarse crystalline granitegneiss, strongly weathered, ventifacted, and partly polished, and outcrops were 'crumbled' and without strength.From theCambridge English Corpus
In weakly deformedgneiss, the mafic minerals (biotite, augite and hornblende) occur as irregular clusters, locally separated from plagioclase by coronas of garnet.From theCambridge English Corpus
Samples from the normal smooth surface of thegneissboulder show that the surface has been ground and polished during glacial transportation.From theCambridge English Corpus
These gneisses have been multiply deformed at granulite-facies conditions.From theCambridge English Corpus
In general, eclogites are predominantly mafic and are preserved as boudins within felsic gneisses.From theCambridge English Corpus
These pass up into a 150 m thick homogeneous granite that is bound by planar surfaces parallel to the foliation in the underlyinggneiss.From theCambridge English Corpus
The kinematic evidence is interpreted to mean that the contact between thegneissand the biotite schist has a normal-shear (hangingwall down) geometry.From theCambridge English Corpus
To the south, the meta-gabbro is bounded by felsicgneiss.From theCambridge English Corpus
There is a continuum apparent between the amphibolites and intermediate gneisses, whilst the felsic gneisses form a separate, high-silica group.From theCambridge English Corpus
However, few recognizable trends are apparent within the data clusters for the siliceous gneisses.From theCambridge English Corpus
In thin-sections, the gneisses are cut by narrow pressure solution seams and narrow cataclastic shear zones.From theCambridge English Corpus
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