“熔融”造句

岩石圈之下是由部分熔融的橄榄岩所组成的软流圈.
Below the lithosphere is the rheosphere comprising partly fused peridotite.

熔融氧化物的流化度增大,纤维直径增大.
The fibre diameter increases with increasing fluidity of the molten oxide.

低速层是由于空隙自由挥发和初期的熔融作用造成的.
The LV zone is due to interstitial free volatiles and incipient melting.

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