화성 관입암
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Q1: What is the difference between intrusive and extrusive igneous rocks?
Intrusive igneous rocks form when magma cools and crystallizes beneath Earth's surface, while extrusive igneous rocks form when magma reaches the surface through volcanic eruption. The key difference is location: intrusive rocks solidify underground in the subsurface, whereas extrusive rocks cool rapidly at or above the surface. This difference in cooling environment directly affects rock texture and crystal size.
Q2: How does cooling rate affect igneous rock crystal size?
Rapid cooling produces very small crystals in a texture called aphanitic, while slow cooling generates larger, visible crystals in a phaneritic texture. Intrusive igneous rocks cool slowly underground, creating coarse grain sizes, whereas surface cooling happens quickly, producing fine-grained rocks. The speed of cooling directly determines the crystal size and overall rock texture.
Q3: What are the main compositional categories of igneous rocks?
Igneous rocks are classified as felsic, intermediate, or mafic based on silica and mineral content. Felsic rocks contain 60-75% silicon dioxide and are rich in aluminum and silica, called granitic. Mafic rocks contain 45-60% silicon dioxide with more iron and magnesium, called basaltic. Intermediate rocks at 55-63% silicon dioxide are andesitic in composition.
Q4: What does partial melting demonstrate about magma composition?
Partial melting shows that the first liquid formed during rock melting has a different composition than the parent rock. The initial melt is enriched in felsic components, while the remaining solid becomes more mafic. When this liquid separates from the system, it creates compositional differences between the extracted magma and the residual rock.
Q5: How can intrusive igneous rocks help identify ore deposits?
Felsic to intermediate intrusive magma bodies are often associated with copper, molybdenum, gold, and silver ore formation. Mafic intrusions are linked to chromium, platinum, and nickel deposits. Identifying these rock types allows geologists to target drilling and mining efforts efficiently, reducing costs and environmental impact while improving exploration success rates.
Q6: Why are intrusive igneous rocks useful for understanding Earth's history?
Intrusive igneous rocks are relatively easy to date using radiogenic isotope ratios, revealing when melting occurred. The presence of these rocks indicates past regions of melting within continental crust, subduction zone activity, and rift zones. This information helps geologists infer the tectonic settings and volcanic activity that existed during rock formation.
Q7: What does the thymol crystal experiment reveal about igneous rock formation?
The thymol experiment demonstrates how cooling rate affects crystal size in igneous rocks. Slow cooling produces larger, mixed crystals resembling intrusive igneous rocks formed in Earth's subsurface. Rapid cooling generates smaller crystals similar to extrusive igneous rocks, also known as aphanitic rocks, which form after volcanic eruption.