该矿田产于中生代相山火山岩盆地古水热系统之中，是水热系统中水-岩相互作用的产物。
It occurs in the fossil hydrothermal systems within Xiangshan Mesozoic volcanic basin and is the product of water-rock interactions in the hydrothermal systems.
研究了水热合成条件及组成变化对产物物相、结构和粒度的影响。
The effects of hydrothermal conditions and compound compositions on phases, structures and grain size of the products were studied.
在KOH催化条件下，还原性气氛有利于纤维素水热液化转化率及液相产物的产率和品质的提高。
By adding KOH as catalyst, the reducing atmosphere was favorable to improve the conversion of collusion and the yield of liquid products.
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