The answer is peridotite.
Olivine is the mineral present in much greater quantities in peridotite than gabbro. Peridotite is rich in olivine, while gabbro contains less olivine and more plagioclase feldspar.
Olivine is the mineral that is present in much greater quantities in peridotite compared to gabbro. Peridotite is rich in olivine, which gives it its characteristic green color, while gabbro contains less olivine and more dark minerals like pyroxene.
Mineral compositions of a basalt can be determined using techniques such as X-ray diffraction, petrographic microscopy, and electron microprobe analysis. X-ray diffraction can identify crystalline minerals present, petrographic microscopy can provide qualitative mineral identification, and electron microprobe analysis can quantify the mineral compositions by measuring the elemental composition of minerals present in the basalt.
Isotopic ratios of elements such as oxygen, hydrogen, and carbon are present in small quantities and can be used to determine the origin of materials such as food or drugs. These ratios vary depending on factors such as geographical location, climate, and production processes, allowing scientists to track the origin of a substance.
Gold is not found in large quantities in Earth's mantle. While it is present in the Earth's crust and in small amounts in the mantle, it is not one of the major elements that make up the mantle's composition.
Olivine is the mineral present in much greater quantities in peridotite than gabbro. Peridotite is rich in olivine, while gabbro contains less olivine and more plagioclase feldspar.
Olivine is the mineral that is present in much greater quantities in peridotite compared to gabbro. Peridotite is rich in olivine, which gives it its characteristic green color, while gabbro contains less olivine and more dark minerals like pyroxene.
The substance that is in the greater amount in a solution is called the solvent. It is typically the dissolving medium that is present in larger quantities compared to the solute.
The scum on the surface of boiling hard water is usually a buildup of mineral deposits, such as calcium and magnesium. These minerals are present in high quantities in hard water and can form a layer of scum when the water is boiled, especially if there are impurities present.
evaporation
The name of the common mineral salt present in seat is
iron
An accessory mineral is a mineral present in small amounts in a rock, but not considered to be characteristic of the rock.
calcium
Lipid is a countable noun. Testing will identify the types and the quantities of lipids present; types and quantities can be counted.
The common mineral salt present in sweat is sodium chloride, also known as table salt.
The most abundant is nitrogen.