“热液的”造句

成矿热液的水主要来自大气降水.
Mineralized hydrothermal water mainly originated from the atmospheric rainfall.

次火山岩是岩浆体系分熔侵入-喷发过程中最后集中成矿热液的载体,具有直接的找矿意义.
Subvocanics is the final carrier of hydrothermal fluid of magmatism thus is the prospecting target.