WorksheetsSoal Batuan Beku
Total questions: 10
Worksheet time: 5mins
Igneous rocks are formed through the main process ...
Weathering of minerals at the surface
Deposition of clastic particles in basins
Freezing of magma/lava into crystalline rocks
Metamorphism under high directed pressure
Chemical precipitation from hydrothermal solutions
Phaneritic texture in igneous rocks indicates ...
Very rapid cooling at the surface
Slow cooling so that crystals are clearly visible
Two-stage cooling with phenocrysts
Explosive pyroclastic processes
Formation of volcanic glass without crystals
The intrusive-extrusive pairs that are compositionally equivalent are ...
Granite - Basalt
Diorite - Rhyolite
Gabbro - Basalt
Peridotite - Andesite
Syenite - Obsidian
The QAPF diagram is most appropriately used to classify ...
Phaneritic plutonic rocks with measurable modal Q-A-P-F percentages
Pure volcanic glass rocks
Fragmental pyroclastic deposits
Foliated metamorphic rocks
Tectonic breccia
The correct order of the discontinuous branches of the Bowen Reaction Series is ...
Olivine → Amphibole → Pyroxene → Biotite
Olivine → Pyroxene → Amphibole → Biotite
Pyroxene → Olivine → Biotite → Amphibole
Amphibole → Biotite → Olivine → Pyroxene
Biotite → Amphibole → Pyroxene → Olivine
Porphyritic texture indicates ...
Uniform very rapid cooling
Slow cooling throughout
Two-stage cooling: slow at depth then rapid during eruption
Post-magmatic recrystallization
Degassing results in glassy texture
Extrusive igneous rocks with glassy, amorphous, and very fine texture are ...
Andesite
Obsidian
Crystalline tuff
Agglomerate
Dacite
The dark-colored mafic rocks that predominantly compose the oceanic crust and are commonly aphanitic in extrusive settings are ...
Rhyolite
Andesite
Basalt
Dacite
Trachyte
The main geometric difference between a sill and a dike is ...
Sill cuts across layering, dike is parallel to layering
Sill is parallel/concordant to layering, dike cuts across layering (discordant)
Sill is always phaneritic, dike is always aphanitic
Sill only forms in volcanic arcs
Dike only exists in oceanic crust
Texture with very coarse crystals (often >1 cm) in shallow intrusive bodies rich in volatiles is called ...
Aphanitic
Phaneritic
Pegmatitic
Vesicular
Pyroclastic
