Hydrothermal sedimentary silicalite studies are important for ore deposits. 熱水沉積硅質(zhì)巖對于礦床研究具有重要意義。
The deposit was produced by superimposition of the hot-water sedimentary mineralization and magmatic hydatogenesis. 該礦床是熱水沉積成礦作用與巖漿熱液成礦作用疊加成礦的產(chǎn)物。
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