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Geology of the Nicola Group in the vicinity of the Iron Mask batholith, Kamloops, British Columbia.

机译:Nicola集团的地质,位于不列颠哥伦比亚省坎卢普斯的铁面具岩床附近。

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摘要

Two regional scale deformation events are observed in the Kamloops region. A Late Triassic-Early Jurassic southwest directed compressional event and a later Tertiary extensional deformation episode, manifested in the uplift of the Nicola horst.;A pervasive metamorphic fabric, exposed in the horst and cross-cut by the 144.8 +/- 5.9 Ma LeJeune granodiorite, is interpreted to represent a broad, Middle Jurassic shear zone, formed by east-directed translation of the Nicola arc during contractional tectonics inboard of an east dipping subduction zone. Variations in orientation of the fabric suggest subsequent east-directed compression during post-Jurassic, pre-Eocene deformation.;The Nicola horst is bounded to the northeast by the Cherry Creek Tectonic Zone, a northwest striking fault zone that separates schistose footwall rocks of the Nicola horst from relatively undeformed Nicola Group rocks in the hanging wall. The fault is interpreted to have accommodated multiple episodes of movement associated with both compressional and extensional tectonics.
机译:在坎卢普斯地区观测到两个区域尺度变形事件。晚三叠世-早侏罗世西南方向的压缩事件和后来的第三纪伸展变形事件,表现在尼古拉霍斯特的隆起中;一种普遍的变质织物,在霍斯特中暴露并被144.8 +/- 5.9 Ma LeJeune横切花岗闪长岩被解释为代表着一个宽大的侏罗纪剪切带,它是由尼古拉弧的东向平移在东倾俯冲带内侧的收缩构造过程中形成的。织物取向的变化表明在侏罗纪后,始新世之前的变形过程中,随后的向东挤压作用。尼古拉霍斯特地带以樱桃溪构造带为东北边界,该带是西北走向的断裂带,分隔了片岩的片状底盘岩。来自相对未变形的Nicola Group的Nicola Horst在悬挂的墙壁上晃动。断层被解释为适应了与压缩构造和伸展构造有关的多个运动事件。

著录项

  • 作者

    White, Shawna Elizabeth.;

  • 作者单位

    University of Alberta (Canada).;

  • 授予单位 University of Alberta (Canada).;
  • 学科 Geology.
  • 学位 M.Sc.
  • 年度 2010
  • 页码 152 p.
  • 总页数 152
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 老年病学;
  • 关键词

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