Paleogene Strata, Seymour Island, Antarctic Peninsula

南极半岛西摩岛古近纪地层

• 批准号: 9508089
• 负责人: David Elliot
• 金额: $ 2.9万
• 依托单位: Ohio State University Research Foundation -DO NOT USE
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 1995
• 资助国家: 美国
• 起止时间: 1995-02-15 至 1997-01-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=9508089&HistoricalAwards=false
• 关键词: Paleogene; Strata; Seymour; Island; Antarctic

9508089 Elliot Abstract This award supports a geologic research project that will take advantage of an opportunity to participate in the 1994-95 geology field program of the Argentine Antarctic Institute. Participation will provide the opportunity to address important problems in the stratigraphic relations and dating of the Paleogene strata on Seymour Island and to field check the new 1:20,000 topographic map that is being prepared by the USGS. The sedimentary strata on Seymour Island are part of the only exposed Upper Cretaceous to Lower Tertiary marine sequence in Antarctica. The Cretaceous-Tertiary succession was deposited in an ensialic back-arc basin related to the development of the mid-Mesozoic to mid-Cenozoic active plate margin of the Antarctic Peninsula. Seymour Island strata range in age between Late Campanian and middle(?) Eocene to earliest(?) Oligocene. These poorly consolidated sedimentary rocks contain a diverse and exceptionally preserved invertebrate fauna, a diverse microflora, and a variety of vertebrates, including marsupials. Fieldwork (to be supported by the Argentine Antarctic Institute in the 1994-95 season) will be directed toward: resolving the complex stratigraphic relations of the Paleogene units on Seymour Island; collection of tuff beds for radiometric dating, and petrologic and geochemical analysis; and sequence analysis of the Paleogene succession. This award is to support travel to Buenos Aires to join the Argentine Antarctic Institute's geology project, travel to confer with the USGS about the results of field checking of the topographic map, and laboratory studies on samples collected in the course of the field season. Specifically, the lab objectives are to: 1) date the ash beds in order to provide absolute age control for sequences that lack calcareous and siliceous microfossil assemblages; and 2) establish the geochemistry of the ash beds to assess contemporaneous volcanic activity and magmatic evol ution of the source region. The results will provide the stratigraphic framework for on-going paleontological projects on Paleogene strata, radiometric data in support of paleontological ages and sequence analysis, and characteristics of the magmatic activity in the source region of the sediments.

小行星9508089 摘要 该奖项支持一个地质研究项目，该项目将利用参加阿根廷南极研究所1994- 1995年地质实地方案的机会。 参加会议将提供机会，解决西摩岛古近纪地层关系和年代测定方面的重要问题，并实地检查美国地质勘探局正在编制的新的1：20，000地形图。 西摩岛上的沉积地层是南极洲唯一出露的上白垩纪-下第三纪海相层序的一部分。 第三纪-第三纪沉积序列形成于与中、新生代南极半岛活动板块边缘发育有关的硅铝质弧后盆地。 西摩岛地层的时代介于晚坎帕尼亚期和中坎帕尼亚期之间。始新世至最早期（？） 渐新世。 这些不牢固的沉积岩包含了多种多样且保存异常完好的无脊椎动物群，多种多样的微生物区系和各种脊椎动物，包括有袋动物。 实地工作（将在1994- 1995年季节得到阿根廷南极研究所的支助）的方向是：解决西摩岛上古近纪各单位的复杂地层关系;收集凝灰岩床，用于放射性测年、岩石学和地球化学分析;以及古近纪序列分析。 该奖项是为了支持前往布宜诺斯艾利斯参加阿根廷南极研究所的地质项目，旅行与美国地质勘探局讨论地形图的实地检查结果，以及对野外季节收集的样本进行实验室研究。 具体而言，实验室的目标是：1）确定灰层的年代，以便为缺乏钙质和硅质微体化石组合的序列提供绝对的年龄控制; 2）建立灰层的地球化学，以评估源区同期的火山活动和岩浆演化。 研究结果将为正在进行的古近纪地层古生物学研究提供地层格架，为古生物时代和层序分析提供放射性数据，并为沉积物源区的岩浆活动特征提供依据。