The late stage quartz-carbonate veinlets, with comb structure, are likely formed in an extensional tectonic environment.

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。

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The late stage quartz-carbonate veinlets, with comb structure, are likely formed in an extensional tectonic environment.

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。

youdao