Metamorphism Flashcards
Define metamorphism
Changes in the mineralogy and/or texture of any pre existing rock in response to changing conditions (usually burial/heating). It is isochemical
What changes may be seen during metamorphism using micro and macro observation?
Mineralogical, textural and development of new fabrics in response to deformation
What are the controls of metamorphism? (7)
Temperature, T
Pressure, P (measured in kbars)
Stress, S (directed pressure, usually from plate collisions)
Fluids, F
Time, t
Composition X
Tectonic processes
What is metamorphic grade?
The intensity of metamorphism in response to the degree of pressure and or heat applied
Draw the graph representing the rock type in relation to depth and heat as seen on page 2
What are the results of the metamorphic process? (5)
Destruction of fossils, beds and sedimentary structures
Hardening of the rock
Change in colour
Alignment of minerals
Growth of new metamorphic minerals
Is burial metamorphism attainable in the crust?
No
What is the approximate geothermal gradient with depth?
25°C km-1
When are hornfels formed?
During contact metamorphism at shallow depths
II - What happens to a rock during metamorphism? (7)
Porosity reduction
Dehydration - hydration
Compaction and volume reduction
Grain growth (diffusion, nucleation, growth)
Grain size increase
Chemical reactions
Destruction of primary fabrics
Explain the development of a metamorphic rock from fresh sediment on the ocean floor (P5)
Fresh sediment is deposited in the ocean floor. It undergoes COMPACTION and DIAGENESIS including PORE WATER EXPULSION, DEHYDRATION, POROSITY REDUCTION (including pressure solution between grains)
BEYOND 200°C the rock undergoes RECRYSTALLISATION. quartz recrystallises into new shapes, quartz growth and mica growth occurs and existing grains undergo DISSOLUTION.
The pressure and heat causes ENHANCED DIFFUSION RATES and therefore GRAIN GROWTH
a GRANOBLASTIC POLYGONAL MATRIX develops. There may be PORPHYROBLAST GROWTH including andalusite or garnet.
overall there is VOLUME REDUCTION.
Describe the fluid release curves in regards to mudstone and basalt
Describe the development of granoblastic fabrics
Under higher pressure and temperature conditions, there is any greater rate of ion diffusion and solution within rocks. Some of these ions begin to nucleate at nucleation sites between crystals, growing outwards until they come into contact with other crystals resulting in an interlocked, equidimensional texture. This texture characterised by 120° triple junctions is called granoblastic (grains) polygonal texture
Describe the formation of porphyroblasts/poikiloblasts
Mica and quartz can recrystallise into garnet and H2O under the right conditions. White mica and quartz breakdown and migration of ions occurs along the grain boundary - this is GRAIN BOUNDARY DIFFUSION. Inclusions of quartz (when in excess) remain in the centre of the garnet. Over time, slow growth and volume diffusion occurs. There is a depletion halo within the garnet
Which ions correspond to which colour in a garnet?
Ca - green
Mg, Fe - red
Ma - Orange
Give two examples of contact metamorphism in Britain
Rinsey Cove, Cornwall
Skiddaw, Lake District
Describe the qualities of spotted rock
Medium gray ground mass with dark grey spots
Fine grained <1mm
Mica, clays and cordierite composition
Spotted texture
In what grade of metamorphism are spotted rocks found?
Low grade
What is a baked margin?
A zone a few mm in width surrounding an igneous intrusions where a portion of the country rocks have been metamorphosed due to the intense temperature of the intrusion.
What is the term for the alteration of rocks by the action of hot fluids?
Metasomatism
Explain the role of granite in metasomatism.
As granite in an intrusion cools it releases fluids. These fluids permeate the surrounding rock, which causes mineralogical changes or growth of new minerals. Fluid from the granite may also contain metal ions and form metal rich veins and larger metallic deposits or “skarns”
How are hornfels formed during contact metamorphism?
When the country rock surrounding an intrusion is made up of shale, the rock subjected to the highest grade contact metamorphism (the part of the aureole closest to the intrusion), the shale is recrystallised into a hard, fine grained, splintery, granoblastic rock called hornfel.
How does andalusite form?
During medium grade metamorphism of shale. The shale is partially recrystallised and clusters of andalusite porphyroblasts formed, forming an andalusite slate
How are spotter rocks formed?
In low grade contact metamorphism of shale, in the outer part of the aureole. Temperatures are low and cause the growth of dark minerals in spots - which can be biotite mica, carbon or iron.