Modern hot spring geochemistry at the Tanlu fault and Jiaoliao block in eastern China

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D,温泉的 18O 价值总是是比本地冷弹簧的那些更否定的。为 ocrurrence 的主要原因身体上在地下水的深传播过程期间是同位素分别。在 D, 18O 值和地下水的最大的传播深度之间的关系表达式被给。从地热的液体逃离的气体主要是在学习区域的导出外壳的气体。Tanlu 差错的压缩结构能延长到深外壳,并且基本上停止上升向表面的深层的气体。
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