The formation of igneous rock from magma
For example the formation of volcanoes or island arcs at convergent plate boundaries. Or mid-ocean ridges and therefore ocean-floor spreading at divergent plate boundaries.
Magmatism is the process by which magma is formed and moves within the Earth's crust. It involves the movement of molten rock beneath the surface, which can eventually lead to volcanic eruptions or the formation of igneous rocks upon cooling and solidification. Magmatism plays a crucial role in shaping the Earth's geology and is responsible for the creation of new crust in tectonic plate boundaries.
Main sources of internal heat are Magmatism and Radioactivity.
First, through metamorphism, then by melting and magmatism.
Deborah A Trimble has written: 'The application of uranium-thorium systematics to rocks from the Lassen Dome Field, California' -- subject(s): Magmatism
Magnat-l'Étrange's population is 229.
Clark M. Johnson has written: 'The Questa magmatic system' -- subject(s): Petrology, Volcanic ash, tuff, Geochemistry, Intrusions (Geology), Magmatism
Chalcophiles combine readilly with sulphur which is predominantly lithophile so chalcophiles are enriched in the mantle and crust, particulary associated with magmatism.
Judith L Hannah has written: 'Magmatic history of the East Tintic Mountains, Utah' -- subject(s): Geology, Structural, Magmatism, Structural Geology
magmatism.
Howard W Oliver has written: 'Locations, descriptions, densities, and magnetic susceptibilities of rock samples collected for analyses of gravity and aeromagnetic anomalies in Yellowstone National Park, Wyoming, Idaho, and Montana' -- subject(s): Magmatism, Gravity anomalies, Volcanism, Magnetic anomalies
The initial source for copper in Arizona were igneous intrusions into native host rock. The copper veins were eventually exposed through erosion at the surface. Copper then leached back into the ground and recrystallized in the form of copper minerals in what is called a supergene enrichment zone. The igneous intrusions were due to a long period of magmatism from the middle of the Mesozoic to the early Cenozoic era.
R. F. Emslie has written: 'Major rock units of the Morin complex, southwestern Quebec' -- subject(s): Geology, Intrusions (Geology) 'Geology and petrology of the Harp Lake Complex, central Labrador' -- subject(s): Geology, Magmatism, Petrology 'Igneous rocks of central Labrador with emphasis on anorthositic and related intrusions' -- subject(s): Geology, Guidebooks, Intrusions (Geology)
John S Pallister has written: 'Isotopic evidence for evolution of sub-continental mantle during Red Sea rifting' -- subject(s): Igneous Rocks, Magmatism, Rocks, Igneous 'Geology of Chiricahua National Monument, a review for the non-specialist' -- subject(s): Geology 'Campground talk and slide show on volcanoes for Chiricahua National Monument' -- subject(s): Slides, Volcanoes