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Geology 12 Plate Boundaries
Geology 12 Plate Boundaries

... other There are three possible collisions: Oceanic crust colliding with oceanic crust causes one to dive under the other (often forming deep trenches or island ...
Plate boundaries| sample answer
Plate boundaries| sample answer

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Ch 9 3 Actions at Plate Boundaries

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Earth`s Interior - Union Beach School District

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Chapter 8: Major Elements

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Chapter 6: Igneous Rocks
Chapter 6: Igneous Rocks

... the size, shape and arrangement of its grains. • Extrusive rocks are typically fine-grained (grains smaller than 1mm). The grains are small because the magma cooled rapidly at the surface, and large crystals did not have time to form. Some intrusive rocks are fine grained, but these would have forme ...
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Kusky Tim

... Phanerozoic times but absent in the Precambrian, but overall, there have been few changes in the style of OPS accretion with time. Komatiites and banded iron formations occur predominantly in Archean orogenic belts, reflecting higher mantle temperatures and less oxic seawater composition, respective ...
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Large igneous province



A large igneous province (LIP) is an extremely large accumulation of igneous rocks, including liquid rock (intrusive) or volcanic rock formations (extrusive), when hot magma extrudes from inside the Earth and flows out. The source of many or all LIPs is variously attributed to mantle plumes or to processes associated with plate tectonics. Types of LIPs can include large volcanic provinces (LVP), created through flood basalt and large plutonic provinces (LPP). Eleven distinct flood basalt episodes occurred in the past 250 million years, creating volcanic provinces, which coincided with mass extinctions in prehistoric times. Formation depends on a range of factors, such as continental configuration, latitude, volume, rate, duration of eruption, style and setting (continental vs. oceanic), the preexisting climate state, and the biota resilience to change.
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