The Stanley unconformity in Lake Huron basin: evidence for a climate-driven closed lowstand about 7900 14C BP, with similar implications for the Chippewa lowstand in Lake Michigan basin

C. F. M. Lewis; C. W. Heil Jr.; J. B. Hubeny; J. W. King; T. C. Moore Jr.; D. K. Rea

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The Stanley unconformity in Lake Huron basin: evidence for a climate-driven closed lowstand about 7900 14C BP, with similar implications for the Chippewa lowstand in Lake Michigan basin

机译：休伦湖盆地的斯坦利不整合面：证据表明气候驱动的封闭低位约7900 14 C BP，与密歇根湖盆地奇珀瓦低位相似

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J.L. Hough in 1962 recognized an erosional unconformity in the upper section of early postglacial lake sediments in northwestern Lake Huron. Low-level Lake Stanley was defined at 70 m below present water surface on the basis of this observation, and was inferred to follow the Main Algonquin highstand and Post-Algonquin lake phases about 10 14C ka, a seminal contribution to the understanding of Great Lakes history. Lake Stanley was thought to have overflowed from the Huron basin through the Georgian Bay basin and the glacio-isostatically depressed North Bay outlet to Ottawa and St. Lawrence rivers. For this overflow to have occurred, Hough assumed that post-Algonquin glacial rebound was delayed until after the Lake Stanley phase.

机译：霍夫（J.L. Hough）于1962年认识到休伦湖西北部早期冰川后湖泊沉积物的上部存在侵蚀不整合。根据这一观察，将低水位的斯坦利湖定义为当前水面以下70 m，并推断其遵循的主要Algonquin高水位相和后Algonquin湖相约为10 14 C ka，这对对大湖区历史的了解。人们认为，斯坦利湖已经从休伦盆地溢出，流经乔治亚湾流域，以及北冰洋的冰川等静压出口流向渥太华河和圣劳伦斯河。对于这种溢出的发生，霍夫认为阿冈昆后的冰川回弹被推迟到斯坦利湖阶段之后。

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来源
《Journal of Paleolimnology》 |2007年第3期|435-452|共18页
作者
C. F. M. Lewis; C. W. Heil Jr.; J. B. Hubeny; J. W. King; T. C. Moore Jr.; D. K. Rea;
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作者单位

Geological Survey of Canada Atlantic Natural Resources Canada Bedford Institute of Oceanography P.O. Box 1006 Dartmouth NS B2Y 4A2 Canada;

Graduate School of Oceanography University of Rhode Island Narragansett RI 02882-1197 USA;

Graduate School of Oceanography University of Rhode Island Narragansett RI 02882-1197 USA;

Graduate School of Oceanography University of Rhode Island Narragansett RI 02882-1197 USA;

Department of Geological Sciences University of Michigan Ann Arbor MI 48019-1063 USA;

Department of Geological Sciences University of Michigan Ann Arbor MI 48019-1063 USA;

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原文格式 PDF
正文语种 eng
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关键词
Great Lakes; Holocene lake levels; Stratigraphy; Sediment physical properties; Glacial rebound; Closed lakes;

机译：大湖;全新世湖水位;地层;沉积物物性;冰川回弹;封闭湖泊;

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外文文献

1. The Stanley unconformity in Lake Huron basin: evidence for a climate-driven closed lowstand about 7900 C-14 BP, with similar implications for the Chippewa lowstand in Lake Michigan basin [J] . Lewis CFM, Heil CW, Hubeny JB, Journal of paleolimnology . 2007,第3期

机译：休伦湖盆地的斯坦利不整合面：证据表明气候驱动的封闭低层约7900 C-14 BP，与密歇根湖盆地奇珀瓦低层相似
2. A new water-level history for Lake Ontario basin: Evidence for a climate-driven early Holocene lowstand [J] . Anderson T.W., Lewis C.F.M. Journal of paleolimnology . 2012,第3期

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3. A new water-level history for Lake Ontario basin: evidence for a climate-driven early Holocene lowstand [J] . T. W. Anderson, C. F. M. Lewis Journal of Paleolimnology . 2012,第3期

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8. Pilot Study Program, Great Lakes Shoreland Damage Study. Apendix III. Part 1. Great Lakes Shoreland Damage Survey; Muskegon, Manistee, Schoolcraft, Chippewa, Alcona, and Huron Counties, Michigan. [R] . Armstong, J. M., McGill, M. R., Kubeck, A. M., 1976

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The Stanley unconformity in Lake Huron basin: evidence for a climate-driven closed lowstand about 7900 14C BP, with similar implications for the Chippewa lowstand in Lake Michigan basin

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