例句與造句

1. The calcium oxide, silica, and silicates melt and are mixed into the corium.
2. He is credited for proposing that pegmatites form through the interaction of silicate melt and supercritical water.
3. Fractional crystallization in silicate melts ( magmas ) is a very complex process compared to chemical systems in the laboratory because it is affected by a wide variety of phenomena.
4. Fractional crystallization in silicate melts ( magmas ) is complex compared to crystallization in chemical systems at constant pressure and composition, because changes in pressure and composition can have dramatic effects on magma evolution.
5. The Chernobyl melt was a silicate melt which contained inclusions of U phases, molten steel and high levels of uranium zirconium silicate ( " chernobylite ", a black and yellow technogenic mineral ).
6. It's difficult to find silicate melt in a sentence. 用silicate melt造句挺難的
7. These intergrowths are typical of pegmatite and granophyre, and they have been interpreted as documenting simultaneous crystallization of the intergrown minerals in the presence of a silicate melt together with a water-rich phase.
8. The texture may commonly form in the presence of a vapor phase as well as a silicate melt, however, and vapor-rock reactions below the solidus may result in feldspar replacement and consequent compositional changes.
9. Water in silicate melts at the high temperature and pressure conditions within the crust exists as a supercritical fluid rather than in a gaseous state ( the critical point for water is at 374 癈 and 218 bar ).
10. A variant of the diamond anvil, the hydrothermal diamond anvil cell ( HDAC ) is used in experimental petrology / geochemistry for the study of aqueous fluids, silicate melts, immiscible liquids, mineral solubility and aqueous fluid speciation at geologic pressures and temperatures.
11. In association with the names of geologists grouped in this area, it was named by the UK Antarctic Place-Names Committee in 1971 after Pentti Eskola, a Finnish geologist who was an authority on the Precambrian rocks of Finland and on silicate melt systems.
12. Metasomatism is more complicated in the Earth's mantle, because the composition of peridotite at high temperatures can be changed by infiltration of carbonate and silicate melts and by carbon dioxide-rich and water-rich fluids, as discussed by Luth ( 2003 ).
13. For example, the partial pressure ( fugacity ) of water in silicate melts can be of prime importance, as in near-oxygen fugacity of melts, and separation of the oxide phases can be an important control of silica concentration in the evolving magma, and may be important in andesite genesis.