Silicates.
Both minerals have a vitreous luster, a white streak, and contain oxygen.
The minerals that form diorite include plagioclase feldspar, biotite, and hornblende. Andesite is primarily composed of plagioclase feldspar, pyroxene, and hornblende. Both rocks are intermediate in composition between granite and basalt.
Oxygen (O) and hydrogen (H) are the only two that are found in both.
Because both crystallize at similar temperatures and pressures according to Bowen's Reaction Series.
The common chemical elements found in both DDT (dichlorodiphenyltrichloroethane) and Freon (chlorofluorocarbons) are carbon, chlorine, and hydrogen.
Gabbro and basalt are both mafic igneous rocks and contain minerals such as pyroxene, plagioclase feldspar, and olivine. Gabbro typically has a coarser grain size compared to basalt, which has a fine-grained texture due to its rapid cooling at the Earth's surface.
Both minerals have a vitreous luster, a white streak, and contain oxygen.
The minerals that form diorite include plagioclase feldspar, biotite, and hornblende. Andesite is primarily composed of plagioclase feldspar, pyroxene, and hornblende. Both rocks are intermediate in composition between granite and basalt.
Gabbro is a type of intrusive igneous rock that is rich in iron and magnesium minerals, with a coarse-grained texture. Peridotite is an ultramafic rock composed mainly of the minerals olivine and pyroxene, and is commonly found in the Earth's mantle. Both rocks are important components of the Earth's crust and play a key role in the formation of other rocks through processes like metamorphism and melting.
Oxygen (O) and hydrogen (H) are the only two that are found in both.
it is because the both elements are natural and they cannot be destroyed.
Quartz is a common mineral found on Earth that is also found on the moon and Mars. It is a hard and durable mineral that can withstand environmental conditions found on both celestial bodies.
Olivene is a mineral, not a rock. It can be found in both intrusive and extrusive igneous rocks. The appearance of olivene is mainly controlled by the composition of the magma
Because both crystallize at similar temperatures and pressures according to Bowen's Reaction Series.
Because both crystallize at similar temperatures and pressures according to Bowen's Reaction Series.
i think its amio acids.
Olivine and calcium-rich plagioclase are often found together in igneous rocks because they have similar crystallization temperatures and are both common minerals in mafic igneous rocks. They are compatible minerals that can crystallize simultaneously from a cooling magma, leading to their coexistence in the same rock.