The fluid was so hot that it made upper Ordovician palaeotemperature go up 50 ℃, and increased the hydrocarbon-generating rate of carbonate rock in Ordovician 32 times at least.
流体携带了大量深部热能，使奥陶系上部古地温升
50℃，
将其中的碳酸盐岩生烃速度
了至少32倍。
The fluid was so hot that it made upper Ordovician palaeotemperature go up 50 ℃, and increased the hydrocarbon-generating rate of carbonate rock in Ordovician 32 times at least.
流体携带了大量深部热能，使奥陶系上部古地温升50℃，将其中的碳酸盐岩生烃速度了至少32倍。
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