一个新的新生代地质和冰川历史范式如何解释美国俄克拉何马州蓬托托克县及其附近的阿肯色-红河流域分水岭地形图证据

E. Clausen
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引用次数: 0

摘要

一个新的新生代地质和冰川史范式(新范式),从根本上不同于公认的新生代地质和冰川史范式(公认范式),描述了一个厚厚的北美大陆冰盖(位于大陆冰盖通常被报道的地方),它通过周围地区的深度侵蚀和隆起创造并占据了一个深“洞”(公认范式没有看到这个厚冰盖或深“洞”)。俄克拉何马州东南部蓬托托克县地区不寻常的侵蚀地貌特征包括不对称的加拿大-加拿大-红河流域分水岭,一个巨大的悬崖环绕的盆地,大多数向南的Clear Boggy Creek源头始于此,以及一个巨大的悬崖环绕的高地,向南的蓝河开始于此。用于测试新范式的能力,利用大规模和长期的南向融水洪水来解释以前无法解释或解释不清的详细地形图、排水系统和侵蚀地貌证据。众多的低点(被称为分水岭交叉点)表明,大规模且长期的南向融水洪水确实流经了现在的加拿大-红河流域分水岭(这种解释也与Clear Boggy Creek悬崖环绕的盆地和蓝河悬崖环绕的高地形状一致)。新的范式描述了大规模和长期的融水洪水,也解释了以前未被认识到的深层区域侵蚀(这可以从详细的地形图证据中确定)。东向的加拿大河谷的上游侵蚀(来自阿肯色河谷)将长期存在的南向融水洪水转移到阿肯色河谷,并最终成为深“洞”唯一的南部出口。先前俄克拉何马州东南部的排水历史解释(基于落基山脉冰川融水流向东向河流的公认范式观点)没有提供足够的水量或水流方向来解释详细的地形图排水系统和侵蚀地貌证据,而新范式的大规模和长期的南向融水洪水确实解释了这一点。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
How a New Cenozoic Geology and Glacial History Paradigm Explains Arkansas-Red River Drainage Divide Area Topographic Map Evidence in and near Pontotoc County, Oklahoma, USA
A new Cenozoic geology and glacial history paradigm (new paradigm), fundamentally different from the accepted Cenozoic geology and glacial history paradigm (accepted paradigm), describes a thick North American continental icesheet (located where continental icesheets are usually reported to have been) which by deep erosion and uplift of surrounding regions created and occupied a deep “hole” (the accepted paradigm does not see this thick ice sheet or the deep “hole”). Unusual erosional landform features in the southeast Oklahoma Pontotoc County region including the asymmetric Cana-dian-Red River drainage divide, a large escarpment-surrounded basin in which most south-oriented Clear Boggy Creek headwaters begin, and a large escarpment-surrounded upland on which the south-oriented Blue River be-gins, are used to test the new paradigm’s ability to use large and prolonged south-oriented melt water floods to explain previously unexplained or poorly explained detailed topographic map drainage system and erosional landform evidence. Numerous low points (referred to as divide crossings) indicate large and prolonged south-oriented melt water floods did flow across what is now the Canadian-Red River drainage divide (an interpretation also consistent with Clear Boggy Creek escarpment-surrounded basin and Blue River es-carpment-surrounded upland shapes). The new paradigm described massive and prolonged melt water floods also account for previously unrecognized deep regional erosion (which is determinable from detailed topographic map evidence). East-oriented Canadian River valley headward erosion (from the Arkansas River valley) diverted the long-lived south-oriented meltwater floods to the Arkansas River valley and to what ultimately became the deep “hole’s” only southern exit. Previous southeast Oklahoma drainage history interpretations (made from the accepted paradigm perspective in which Rocky Mountain glacier melt water flowed to east-oriented rivers) do not provide adequate water volumes or flow directions to explain the detailed topographic map drainage system and erosional landform evidence, which the new paradigm’s massive and prolonged south-oriented melt water floods do explain.
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