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Cooling and inferred uplift/erosion history of the Grenville Orogen, Ontario: Constraints from argon-40/argon-39 thermochronology.

机译:安大略省格伦维尔造山带的降温和推断隆升/侵蚀历史:氩40 /氩39热年代学的限制。

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摘要

In this thesis field observations and laboratory data are related to the regional cooling and uplift/erosion history of the Grenville Province in Ontario. The conclusions reached during this investigation provide important constraints for tectonic models of the evolution of this ancient mountain belt. Equally important, these results provide a quantitative measure of the time involved in mountain building processes, thus yielding fundamental insights into phenomena that continually act to reshape the face of our planet.;Thermochronological (;Regional uplift/erosion rates for the Grenville Orogen of Ontario have been estimated from the ;Different terranes within the CMB preserve hornblende ;Twenty-two of the hornblendes used for thermochronology have been quantitatively analyzed for major elements by microprobe, Fe;Water activities (aH
机译:在本文中,野外观测和实验室数据与安大略省格伦维尔省的区域降温和隆升/侵蚀历史有关。在这项调查过程中得出的结论为这一古老山区带的演化构造模型提供了重要的限制。同样重要的是,这些结果提供了对山区建造过程中所用时间的定量度量,从而得出了对现象的基本见解,这些现象不断作用于重塑我们星球的表面。;热年代学(;安大略省Grenville Orogen的区域隆升/侵蚀速率通过以下方法进行估算:; CMB保护区角闪石中的不同地形;通过热探针,Fe,水活度(aH

著录项

  • 作者

    Cosca, Michael Anthony.;

  • 作者单位

    University of Michigan.;

  • 授予单位 University of Michigan.;
  • 学科 Geology.;Geochemistry.
  • 学位 Ph.D.
  • 年度 1989
  • 页码 235 p.
  • 总页数 235
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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