Gneiss
is a metamorphic rock with a banded or foliated structure, typically coarse-grained (crystalline) and consisting mainly of feldspar, quartz, mica, and may have mafic minerals.
What is a strong parallel alignment of coarse mica flakes?
What term describes a strong, parallel alignment of coarse mice flakes and/or different bands in a metamorphic rock?
Foliation
.
What is the name given to the parallel alignment of mica minerals?
What Is
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.
Which metamorphic rock is composed of only mica?
| Texture Characteristics Rock Name | foliated (banded) thin layers of mica Schist | foliated (banded) thick layers of quartz, feldspar, and mica Gneiss | non-foliated (massive) welded quartz sandstone Quartzite | non-foliated (massive) sugary to course crystals, fizzes in HCl acid Marble |
|---|
Does slate have abundant coarse-grained mica?
Slate has
abundant, coarse-grained mica
. Slate forms from shales and mudstones. In slate, rock cleavage is common. Sedimentary features may be visible in slates.
What are the two main categories of metamorphic rock?
Metamorphic rocks are broadly classified as
foliated or non-foliated
. Non-foliated metamorphic rocks do not have aligned mineral crystals.
Is a strong parallel alignment of coarse Mica?
Answer:
Foliation
is a strong, parallel alignment of coarse mica flakes and/or of different mineral bands in a metamorphic rock.
What is the difference between banding and mineral alignment?
This parallel alignment causes the
rock to split easily into thin layers or sheets
. Foliation is common in aphanitic as well as phaneritic metamorphic rocks. … Banding means that the rock consists of alternating, thin layers (typically 1 mm to 1 cm) of two different mineral compositions.
What are the four types of foliation?
The various types of foliated metamorphic rocks, listed in order of the grade or intensity of metamorphism and the type of foliation are
slate, phyllite, schist, and gneiss
(Figure 7.8).
What are the 3 main types of metamorphic rocks?
The three types of metamorphism are
Contact, Regional, and Dynamic metamorphism
. Contact Metamorphism occurs when magma comes in contact with an already existing body of rock. When this happens the existing rocks temperature rises and also becomes infiltrated with fluid from the magma.
How can you identify a metamorphic rock?
Metamorphic rocks are rocks that have become changed by intense heat or pressure while forming. One way to tell if a rock sample is metamorphic is
to see if the crystals within it are arranged in bands
. Examples of metamorphic rocks are marble, schist, gneiss, and slate.
What are the characteristics of metamorphic rocks?
Metamorphic rocks were once igneous or sedimentary rocks, but have been changed (metamorphosed) as a result of intense heat and/or pressure within the Earth’s crust. They are
crystalline and often have a “squashed” (foliated or banded) texture
.
What are the 4 main types of metamorphism?
- Type # 1. Contact Metamorphism:
- Type # 2. Regional Metamorphism:
- Type # 3. Hydro-Metamorphism:
- Type # 4. Hydro-Thermo-Metamorphism:
What grade of metamorphism is phyllite?
Phyllites are said to have a texture called “phyllitic sheen,” and are usually classified as having formed through
low-grade metamorphic conditions
through regional metamorphism metamorphic facies. Phyllite has good fissility (a tendency to split into sheets).
What is the major source of heat for contact metamorphism?
Contact metamorphism occurs to solid rock next to an igneous intrusion and is caused by the heat
from the nearby body of magma
.
