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Response to Comment on “How will induced seismicity in Oklahoma respond to decreased saltwater injection rates?”

机译:对“俄克拉何马州的地震活动将如何应对注入盐水速度下降的评论”的评论

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Goebel et al. question our forecasted response of induced seismicity to reduction of saltwater injection rates in north-central Oklahoma and raise the concern that “the probability of future damaging earthquakes may be underestimated.” We compare our prediction to earthquake data recorded in the 8 months after publication. Observed seismicity rates and magnitudes agree with the forecast of our model. Our use of a probabilistic model accounts for uncertainties and observed M ≥ 4.5 to date confirm the conservative nature of our prediction. The “realistic parameter range” suggested by Goebel et al. is based on a misunderstanding of our statistical model and disagrees with the long-term decay of seismicity in the region.
机译:Goebel等。质疑我们对俄克拉荷马州中北部诱发的地震活动对咸水注入率降低的预测响应,并引起人们的担忧,即“未来破坏性地震的可能性可能被低估了。”我们将我们的预测与发布后8个月内记录的地震数据进行了比较。观测到的地震活动率和震级与我们模型的预测一致。我们使用概率模型解决了不确定性,迄今为止,观察到的M≥4.5证实了我们预测的保守性。 Goebel等人建议的“现实参数范围”。基于对我们的统计模型的误解,不同意该地区地震活动的长期衰减。

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