What are the different metamorphic textures?
The five basic metamorphic textures with typical rock types are slaty (includes slate and phyllite; the foliation is called “slaty cleavage”), schistose (includes schist; the foliation is called “schistosity”), gneissose (gneiss; the foliation is called “gneissosity”), granoblastic (includes granulite, some marbles andClick to see full answer. Similarly, it is asked, what are the different textures…
The five basic metamorphic textures with typical rock types are slaty (includes slate and phyllite; the foliation is called “slaty cleavage”), schistose (includes schist; the foliation is called “schistosity”), gneissose (gneiss; the foliation is called “gneissosity”), granoblastic (includes granulite, some marbles andClick to see full answer. Similarly, it is asked, what are the different textures of metamorphic rocks?TEXTURES Textures of metamorphic rocks fall into two broad groups, FOLIATED and NON-FOLIATED. Foliation is produced in a rock by the parallel alignment of platy minerals (e.g., muscovite, biotite, chlorite), needle-like minerals (e.g., hornblende), or tabular minerals (e.g., feldspars).Secondly, what causes the metamorphic texture? Metamorphic textures Foliation is caused by the re-alignment of minerals when they are subjected to high pressure and temperature. Individual minerals align themselves perpendicular to the stress field such that their long axes are in the direction of these planes (which may look like the cleavage planes of minerals). Likewise, people ask, what metamorphic texture does phyllite? Phyllite is a foliated metamorphic rock that has been subjected to low levels of heat, pressure and chemical activity. It is composed mainly of flake-shaped mica minerals in parallel alignment. The strong parallel alignment of the mica grains allows the rock to be easily split into sheets or slabs.What are the types of foliation?There are three types of foliated rocks: slate, schist, and gneiss. Each type varies based on the size of the mineral grain and how foliation is characterized.
