Buff coloured rock.
Almost pure quartz, which has been very well recrystallised.
Faint banding could be original bedding.
Fine to medium grained recrystallised quartz with sutured contacts.
The sutured (ragged) grain boundaries and undulose extinction of the quartz grains indicate that this rock formed under relatively low temperature metamorphism. Had the rock been raised to higher temperatures perfect 120° grain boundaries would have formed, and the quartz would not be strained.
Inserting the sensitive tint plate results in the vast majority of grains changing colour in the same way – most of the grains simultaneously display higher interference colours in one orientation, and lower interference colours in the other orientation. This strong fabric was produced by recrystallisation under directed stress, which caused all the grains to elongate in one direction.
Precambrian
Braemar, Aberdeenshire
Buff coloured rock.
Almost pure quartz, which has been very well recrystallised.
Faint banding could be original bedding.
Fine to medium grained recrystallised quartz with sutured contacts.
The sutured (ragged) grain boundaries and undulose extinction of the quartz grains indicate that this rock formed under relatively low temperature metamorphism. Had the rock been raised to higher temperatures perfect 120° grain boundaries would have formed, and the quartz would not be strained.
Inserting the sensitive tint plate results in the vast majority of grains changing colour in the same way – most of the grains simultaneously display higher interference colours in one orientation, and lower interference colours in the other orientation. This strong fabric was produced by recrystallisation under directed stress, which caused all the grains to elongate in one direction.
Strongly developed planar fabric made up of platy biotite mica and muscovite mica grains and lenses of quartz grains. Fabric wraps around large, euhedral garnets, typically ~2mm across. Quartz, the most soluble mineral, has recrystallised at the corners of the “eyes”, in the pressure shadows of the garnets.
Bands of interlocking quartz grains and some feldspar (plagioclase and alkali, lamellar twinning and alteration), alternate with bands composed of needles of biotite mica and muscovite mica, about 50:50.
Quartz displays undulose extinction, and being the most soluble mineral in this rock has recrystallised into the pressure shadows around the garnets.
The fabric is interrupted by large euhedral garnet crystals. Characteristically the garnets are isotropic and have high relief. They contain inclusions of quartz and mica.
Accessory minerals:
- chlorite
- staurolite
- tourmaline
This schist contains large quantities of muscovite indicating that it had a pelitic protolith. This pelite was subjected to high pressures and temperatures during regional metamorphism, resulting in the crystallisation and alignment of metamorphic minerals.
The foliation of this schist may be due to original compositional banding in the pelite; the quartz-rich layers having been sandy layers, while the mica-rich layers were muddy.
Some evidence for post-metamorphic deformation: quartz displaying undulose extinction; micas are wrapped around the garnet grains.
Tiny grains of chlorite found around the edges of the garnets indicate that some retrogradation has taken place. Chlorite is a common break-down product of garnets.
In thin-section staurolite is pale-golden in colour. It has high relief, and displays straight extinction and 1st order birefringence colours.
Pre-Devonian
Ny-Friesland, Spitsbergen
Strongly developed planar fabric made up of platy biotite mica and muscovite mica grains and lenses of quartz grains. Fabric wraps around large, euhedral garnets, typically ~2mm across. Quartz, the most soluble mineral, has recrystallised at the corners of the “eyes”, in the pressure shadows of the garnets.
Bands of interlocking quartz grains and some feldspar (plagioclase and alkali, lamellar twinning and alteration), alternate with bands composed of needles of biotite mica and muscovite mica, about 50:50.
Quartz displays undulose extinction, and being the most soluble mineral in this rock has recrystallised into the pressure shadows around the garnets.
The fabric is interrupted by large euhedral garnet crystals. Characteristically the garnets are isotropic and have high relief. They contain inclusions of quartz and mica.
Accessory minerals:
- chlorite
- staurolite
- tourmaline
This schist contains large quantities of muscovite indicating that it had a pelitic protolith. This pelite was subjected to high pressures and temperatures during regional metamorphism, resulting in the crystallisation and alignment of metamorphic minerals.
The foliation of this schist may be due to original compositional banding in the pelite; the quartz-rich layers having been sandy layers, while the mica-rich layers were muddy.
Some evidence for post-metamorphic deformation: quartz displaying undulose extinction; micas are wrapped around the garnet grains.
Tiny grains of chlorite found around the edges of the garnets indicate that some retrogradation has taken place. Chlorite is a common break-down product of garnets.
In thin-section staurolite is pale-golden in colour. It has high relief, and displays straight extinction and 1st order birefringence colours.