There are three branches of petrology, corresponding to the three types of rocks:
igneous,
metamorphic, and
sedimentary, and another dealing with experimental techniques: •
Igneous petrology focuses on the composition and texture of
igneous rocks (rocks such as
granite or
basalt which have crystallized from molten rock or
magma). Igneous rocks include
volcanic and
plutonic rocks. • Sedimentary petrology focuses on the composition and texture of
sedimentary rocks (rocks such as
sandstone,
shale, or
limestone which consist of pieces or particles derived from other rocks or biological or chemical deposits, and are usually bound together in a
matrix of finer material). • Metamorphic petrology focuses on the composition and texture of
metamorphic rocks (rocks such as
slate,
marble,
gneiss, or
schist) which have undergone chemical, mineralogical or textural changes due to the effects of pressure, temperature, or both). The original rock, prior to change (called the protolith), may be of any sort. •
Experimental petrology employs high-pressure, high-temperature apparatus to investigate the geochemistry and
phase relations of natural or synthetic materials at elevated pressures and temperatures. Experiments are particularly useful for investigating rocks of the lower
crust and
upper mantle that rarely survive the journey to the surface in pristine condition. They are also one of the prime sources of information about completely inaccessible rocks, such as those in the Earth's
lower mantle and in the mantles of the other
terrestrial planets and the
Moon. The work of experimental petrologists has laid a foundation on which modern understanding of igneous and metamorphic processes has been built. ==See also==