Process of change undergone by an existing rock (protolith) in solid state to another rock
Metamorphism
Agents of metamorphism
Heat, pressure, deviatoric stress, chemically active fluids
Source of heat
Geothermal gradient (20-30 C per km)
Intrusive bodies
Radioactive decay
Pressure
Confining pressure vs deviatoric stress
Equal force in all directions
There us a dominant axis
Chemically active fluids must be
Hot
Type of metamorphism
- area or volume affected
Local metamorphism: small volume (<300 km3)
Regional metamorphism: thousands of km
Type of metamorphism
Chemical processes
Isochemical - no change in the bulk chemistry of the rock
Allochemical - there is change
Dominant metamorphic agent
Classification of metamorphic rock
Texture - size, shape and relationships of constituent minerals
Protolith - original rock that was transformed by metamorphism
Mineralogy - mineral assemblage present
Based on texture
Foliated - parallel alignment of minerals
Nonfoliated - no preferred mineral alignment (metamorphism – transformation of one mineral to another)
Why is parent rock important?
Other metamorphic rocks in Philippines
Amphibolite
serpentine
migmatite
Other metamorphic rocks in Philippines
foliated, plagioclases
hydrothermally, peridotites
quartz and feldspar