it changes it in to amphibolite and schist
Basalt when metamorphosed turns to the following rocks: (LEAST PRESSURE AND TEMPERATURE TO THE MOST) + mineralogy -Greenschist-albite, epidote, chlorite -Amphibolite-amphioble, plagioclase feldspar -Granulite-calcium-rich pyroxene and plagioclase feldspar -Eclogite-sodium-rich pyroxene and garnet
At a temperature of 600 degrees Celsius and 14 kilobars pressure, basalt metamorphism typically produces minerals such as amphibole, pyroxene, and plagioclase feldspar, resulting in the formation of greenschist or amphibolite facies metamorphic rocks. These minerals form in response to the high temperature and pressure conditions, leading to changes in the original basaltic rock composition.
It doesn't. They have different chemical compositions. Limestone is CaCO3. Basalt is mainly SiO4 and Fe. There is however an igneous rock composed predominantly of carbonate minerals known as carbonatite. This tends to form at zones of continental rifting. It isn't basalt however!
Amphibolite is typically formed from the metamorphism of basalt or gabbro, which are both mafic igneous rocks. The high temperatures and pressures during metamorphism lead to the formation of amphibole minerals, giving rise to the rock type known as amphibolite.
Yes, amphibolite is a foliated metamorphic rock. It forms through the metamorphism of basalt or gabbro and typically exhibits a well-developed foliation called schistosity due to the alignment of its mineral grains.
Extreme metamorphism of oceanic crustal basalt.
A metamorphic rock formed from Basalt is Schist. a.k.a. Green Schist
Sandstone is changed into quartzite and basalt is changed into schist or gneiss through the process of metamorphism.
Basalt when metamorphosed turns to the following rocks: (LEAST PRESSURE AND TEMPERATURE TO THE MOST) + mineralogy -Greenschist-albite, epidote, chlorite -Amphibolite-amphioble, plagioclase feldspar -Granulite-calcium-rich pyroxene and plagioclase feldspar -Eclogite-sodium-rich pyroxene and garnet
When shale and basalt are subjected to low-grade metamorphism, the mineral formed is typically clay minerals, particularly illite or chlorite. In the case of basalt, the alteration can lead to the formation of minerals like zeolites as well. The metamorphic process involves the recrystallization of existing minerals under heat and pressure, resulting in these secondary minerals.
Basalt will not change it the future. Basalt will always be basalt. As rocks unlike humans or animals do not evolve. As they are inanimate objects. The however can be turned back into magma or lava, They can be eroded, or undergo metamorphism. Then then will change in shape and form but basalt will always have the same chemical composure as if it had a different one it would be a different rock.
When basalt undergoes metamorphism, it can change into a metamorphic rock called greenstone. Greenstone is a fine-grained metamorphic rock that forms from the alteration of basalt through metamorphic processes like recrystallization and the growth of new minerals.
At a temperature of 600 degrees Celsius and 14 kilobars pressure, basalt metamorphism typically produces minerals such as amphibole, pyroxene, and plagioclase feldspar, resulting in the formation of greenschist or amphibolite facies metamorphic rocks. These minerals form in response to the high temperature and pressure conditions, leading to changes in the original basaltic rock composition.
contact metamorphism, regional metamorphism, dynamic metamorphism
It doesn't. They have different chemical compositions. Limestone is CaCO3. Basalt is mainly SiO4 and Fe. There is however an igneous rock composed predominantly of carbonate minerals known as carbonatite. This tends to form at zones of continental rifting. It isn't basalt however!
Amphibolite is typically formed from the metamorphism of basalt or gabbro, which are both mafic igneous rocks. The high temperatures and pressures during metamorphism lead to the formation of amphibole minerals, giving rise to the rock type known as amphibolite.
Yes, amphibolite is a foliated metamorphic rock. It forms through the metamorphism of basalt or gabbro and typically exhibits a well-developed foliation called schistosity due to the alignment of its mineral grains.