Examples of amphibolite

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There is a continuum apparent between the amphibolites and intermediate gneisses, whilst the felsic gneisses form a separate, high-silica group.
Partial melting of two amphibolites: contrasting experimental results under fluid-absent conditions.
They do not present planar contact with amphibolite.
Fabrics within the amphibolites are emplacement-related ductile shear fabrics which are parallel to the fabrics along the base of the ophiolite.
Finally, in all three bodies, amphibolite-facies retrogression is more widespread than eclogitization, even though the former may require more fluid.
Virtually unaltered amphibolites may have subordinate, late, randomly oriented biotite laths overgrowing the main foliation.
The eclogite sheets and pods are generally sheared and retrogressed to amphibolites at the margins of such bodies.
The main lithology of the metamor phic sole is amphibolite, with subordinate greenschist, marble and meta-chert.
Magnetic investigation of an amphibolite boulder found on the white line showed that a strong electric current indeed traversed the boulder.
Some amphibolites represent monomineralic hornblendites; others contain layers of hornblende and plagioclase.
Highly non-cylindrical folds and sheath folds with amphibolite-facies axial planar fabrics are locally developed.

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