chapter 7 Flashcards
__ are important economic resources for lead, zinc, gold, silver, tungsten, tin and mercury.
meteor impact sites, hydrothermal veins or marble?
hydrothermal veins
___ forces the constituents of a rock to become parallel to one another.
pressure, strain, differential stress or starch?
differential stress
__ forms when a limestone recrystallizes during metamorphism.
marble, gneiss, or coal
marble
because of the ease with which it can be split into thin flat sheets, this metamorphic rock is used for making chalkboard, pool tables, and roofs.
granite, marble, slate or quartzite?
slate
when a rock is buried to increasing depth it is subject to increasingly greater temp and pressure and will undergo ___.
contact metamorphism, shock metamorphism, or prograde metamorphism?
prograde metamorphism
the most important factors controlling the characters of metamorphic rocks include __.
temperature, pressure, water, composition of parent rock, or all or the above?
all of the above
___stress is a type of differential stress.
shearing, confining, or hydrostatic
shearing
shock metamorphism can occur as a result of __.
tsunami, earthquakes, meteor impacts or tornadoes
meteor impacts
__ is metamorphism coupled with the introduction of ions (charged atoms) from an external source.
blending, metasomatism or differentiation?
metasomatism
__ is the lowest-grade rock in progressive metamorphism.
schist, gneiss, marble or slate?
slate
__ is a very fine-grained metamorphic rock that splits along parallel planes.
slate, sandstone, or marble?
slate
the major __ classification of metamorphic rocks divides them into foliated and non-foliated groups.
crystal size, textural, mineral or genetic.
textural
the light-color layers within a typical gneiss are formed by __.
amphiboles, feldspars, olivine, or calcite?
feldspars
the deeper a rock is below the earth’s surface __.
the hotter it will be, the cooler it will be, or has no influence on temperature?
the hotter it will be
metamorphic rocks are prevalent __.
in intensely deformed portions of large mountain ranges, where the continental crust is subjected to high temperatures, pressures, and tectonic stress.