most likely Mg rich pyroxenen since Fe starts melting earlier from a melt and also mantle rocks that are highly melt depleted contain very high mg rich pyroxenes
Magnesium oxide is non-flammable, but magnesium can burn. Magnesium oxide Melting Point: 2852 °C, 3125 K, 5166 °F Boiling Point: 3600 °C, 3873 K, 6512 °F Magnesium Melting Point: 923 K, 650 °C, 1202 °F Boiling Point: 1363 K, 1091 °C, 1994 °F
higher melting temperature
Because the temperature is higher hence make the boiling and melting point higher.
The outer core is liquid. Its pressure is low enough and its temperature high enough for it to melt. The inner core is solid. Both its pressure and temperature are higher than the outer core, but the increased pressure overwhelms the increased temperature, keeping the inner core from melting.
the melting point of it is higher, if u increase the temperature in a furnace u'll see
most likely Mg rich pyroxenen since Fe starts melting earlier from a melt and also mantle rocks that are highly melt depleted contain very high mg rich pyroxenes
Magnesium Oxide Strontium Sulphate has a melting point of 1606°C while Magnesium Oxide has a melting point of 2852°C
Magnesium has a higher melting point.
a more dense metal
Primers with more GC content will affect the melting temperature. Higher GC content will have a higher melting temperature.
Magnesium oxide is non-flammable, but magnesium can burn. Magnesium oxide Melting Point: 2852 °C, 3125 K, 5166 °F Boiling Point: 3600 °C, 3873 K, 6512 °F Magnesium Melting Point: 923 K, 650 °C, 1202 °F Boiling Point: 1363 K, 1091 °C, 1994 °F
sodium oxide: 1132oC magnesium oxide: 2852oC
higher
higher
higher
higher melting temperature
G-C rich DNA has a higher melting point that A-T rich DNA.