Sentence examples for melting at higher from inspiring English sources

The Hadean mantle potential temperature (MPT) is assumed to have been sufficiently high (1500 to 1700 °C) to initiate partial melting at higher pressure.

The first model suggests that the high degree of melting at higher pressure produced the high Mg# and intermediate amount of orthopyroxene (about 25 vol.%) residue.

Also results indicate that increasing inclination angle leads to faster pace of melting at higher attitudes that results in shorter total melting time.

The formation of a porous coating by local bonding at relatively low velocity and of a very dense coating accompanied by interfacial melting at higher velocity resulted from deformation localization at high strain rates due to the relatively higher adiabacity as compared with other materials, which is one of the unique bonding mechanisms in CP-Ti.

An endotherm at approx. 95°C was seen for the SBE RNAi4.1 starch when melting at higher temperatures (data not shown).

The unique feature of 1b and 1c is melting at high temperatures.

In combination with CO2-laser heating, containerless melting at high temperature of oxides and silicates is possible.

Risk factors of different rotor cores (for example, melting at high temperature and demagnetization effect) are assumed for motor function, but we plan to work as future research subjects based on the results of this research (Ono 2013).

While high α melting trend and data trends may not be an exact match, it is possible that these subvertical alignments result from melting at high fluid content, with a strong fractionation of Cl compared to F. This suggests that (1) the natural highly variable Cl trends we observe probably represent melting trends and (2) those magmas were produced by high degree of metasomatism.

This was attributed to the formation of less perfect crystallites formed during the cooling of melt at higher degree of supercooling.

It is indicated that a fast crystallization in the nematic phase forms relatively more ordered crystals, which melt at higher temperature, and a slow crystallization in the isotropic phase or in the biphasic melt produces poor crystals, which melt at lower temperature.