晚阶段具梳状构造的石英-碳酸盐细脉形成于伸展引张环境。
The late stage quartz-carbonate veinlets, with comb structure, are likely formed in an extensional tectonic environment.
分析了“引细入汤”工程水权转让的必然性和可行性、初始水权的确定、水权转让及“引细入汤”工程的兴建等问题。
The inevitability and feasibility of the transfer of water right and the initial water right of the project are analyzed.
分析了“引细入汤”工程水权转让的必然性和可行性、初始水权的确定、水权转让及“引细入汤”工程的兴建等问题。
The inevitability and feasibility of the transfer of water right and the initial water right of the project are ana.
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