Schistose amphibolite and metagabbro are represented by fine-grained, equigranular rocks of granonematoblastic, nematoblastic
, relict gabbro, poikilitic texture.
The compositional banding is reflected by alternating nematoblastic (hornblende) and granoblastic (plagioclase) bands, within which epidote-group minerals and garnet porphyroblasts occurs.
The compositional banding is reflected in alternating hornblende-bearing nematoblastic and plagioclase-bearing granoblastic bands, within which epidote-group minerals and garnet porphyroblasts occur.
The metamorphic units comprise garnet-glaucophane schist (lepi-doporphyroblastic texture), epidote-chlorite schist (lepidoblastic texture), garnet-lawsonite-glaucophane schist and epidotite (nematoblastic
Staurolite metabasites are characterized by alternating nematoblastic bands composed of hornblende and staurolite (with penetration twinning) and granoblastic bands composed of quartz and plagioclase (Figures 3k-l).
Alternating nematoblastic bands of hornblende and staurolite and granoblastic bands of quartz and plagioclase in the staurolite metabasites.
However, most of the studied metabasites are nematoblastic
amphibolites, consisting of Amp, Ep, Rt, Chl, Qz [+ or -] Grt [+ or -] white-mica [+ or -] Cb and Ilm [+ or -] Ttn after Rt.
The textures in the rocks are nematoblastic and granoblastic.
The textures found in the rocks are nematoblastic, granoblastic and porphyroblastic.
The existent textures include nematoblastic, granoblastic, porphyroblastic and poikiloblastic.