Igneous Rocks and
Processes
Other minerals are important for the full description of igneous rocks:
Olivine, Pyroxene, Hornblende, Biotite and Muscovite
General Classification of Igneous Rocks
Extrusive Rocks(Volcanic)
Intrusive Rocks (Plutonic)
General Classification of Igneous Rocks
MaficFelsic Intermediate
Increasing Fe & Mg
Increasing Si & Al
Common Igneous Rocks
Fine
Grained
(Extrusive)
Coarse
Grained
(Intrusive)
Felsic Intermediate Mafic
Rhyolite Andesite Basalt
Granite Diorite Gabbro
Classification of Igneous Rocks
Streckheisen classification is based on only three minerals:
Quartz, Plagioclase, Potassium Feldspar
Norman Bowen (1887-1956)Father of Experimental Petrology
Bowen’s Reaction SeriesPredictable Mineral Associations
Bowen’s Reaction Series
Discontinuous Series
Bowen’s Reaction SeriesWhat is the trend in silicate structures? Why?
Discontinuous Series
Bowen’s Reaction Series
Continuous Series
Bowen’s Reaction SeriesWhy would aspects of this igneous concept apply to
sedimentary rocks as well?
Least Common Minerals in Sediments
Most Common Minerals in Sediments
Metamorphic Rocks
and Metamorphic Processes
General Rules of Metamorphism
Metamorphism is due to solid-state reactions between minerals due to change in temperature and pressure
Most metamorphic reactions liberate volatiles(H2O and CO2)
The minerals in low-grade metamorphic rocks have more volatiles than high-grade metamorphic rocks e.g., micas amphiboles pyroxenes
Increasing metamorphic grade generally corresponds to increasing grain size e.g., clays micas
Classification of Metamorphic Rocks
Foliated (Banded) Non-Foliated (Massive)
Classification of
Foliated Metamorphic Rocks
Slate Schist Gneiss
Increasing Temperature
Metamorphic Texture Changes
Granite Gneiss
Formation of
Foliated Metamorphic Rocks
Shale Gneiss
Mic
roscope
Hand S
am
ple
Schist
Classification of
Non-Foliated Metamorphic Rocks
Quartzite Marble Serpentinite
Sandstone Limestone Peridotite
Metamorphic Texture Changes
Quartz Arenite
Quartzite
Metamorphic Texture Changes
Quartz Arenite
Quartzite
Limestone Marble
Metamorphic Facies
Identifying Rocks
Foliated/Layered Non-Foliated/Non-Layered
Sedimentary Metamorphic Igneous
Identifying Rocks
Grains Crystals
Sedimentary Metamorphic Igneous
Composition of the Crust
GraniteBasalt,
Gabbro
Si, Al,
Na, KSi, Al,
Ca, Fe, Mg
Composition of the Earth
Distribution of Late Paleozoic
Fossils
Bathymetry of the Ocean Floor
Volcanoes of the World
Volcanoes Correlate Globally with
Deep Earthquakes
Benioff Zone of Seismicity
Plate Tectonic Model
Mantle Convection