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首页> 外文期刊>Rocky Mountain geology >Heart Mountain and South Fork fault systems: Architecture and evolution of the collapse of an Eocene volcanic system, northwest Wyoming: COMMENT
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Heart Mountain and South Fork fault systems: Architecture and evolution of the collapse of an Eocene volcanic system, northwest Wyoming: COMMENT

机译:心山和南福克断层系统:怀俄明州西北部始新世火山系统坍塌的构造和演化:评论

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We would like to begin by paying tribute to Ed Beutner who passed away in 2008. Ed made significant contributions to the continuing debate over one of the most enigmatic features on the surface of the Earth, the Heart Mountain slide block. Ed will be greatly missed and we wish that he were here to respond to our discussion of his most recent paper—we are certain his comments would have been insightful and of interest to all working on the Heart Mountain problem. In lieu of having Ed’s response, we are confident that Tom Hauge will provide a vigorous defense picking up the mantle so aptly held by Ed. We have a number of concerns about the slow/fast model presented by Beutner and Hauge (2009). In our view, many of their arguments supporting slow or incremental movement of the Heart Mountain slide block are not supported by the evidence. In addition, we wish to correct certain erroneous statements and omissions about previous work.
机译:首先,我们要向2008年去世的Ed Beutner致敬。Ed为持续辩论做出了重要贡献,该辩论是地球表面最神秘的特征之一,Heart Mountain滑块。埃德将无比怀念,我们希望他能在这里回应我们对他的最新论文的讨论-我们确信他的评论将是有见地的,并且对所有解决“心山”问题的人都感兴趣。我们相信汤姆·海格(Tom Hauge)将提供强有力的防御,以弥补艾德(Ed)的反应,以捡拾艾德(Ed)如此恰当的举动。我们对Beutner和Hauge(2009)提出的慢/快模型有很多担忧。我们认为,他们的许多论据都没有支持心山滑块缓慢或增量运动的论据。此外,我们希望纠正关于先前工作的某些错误陈述和遗漏。

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