Similarly the CO 2 was partially lost from the fluid phase by precipitation of late diagenetic calcite.

同样地,部分CO2因成岩晚期方解石的沉淀而不再以流体相存在.

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Activation of these two pathways was unexpectedly linked and dependent on fluid - phase activation of factor XII.

激活这两个通路意外地联系并依赖与液相XII因子激活.

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