在平坦化切割区域中进行应变分区:对环岛风格隔离区的重新评估
T A Ducharme1,2, D A Schneider1, B Grasemann3
1Department of Earth and Environmental Science University of Ottawa Ottawa ON Canada.
概括
阿尔米罗波塔莫斯的构造窗口揭示了爱琴海的两种不同的变形事件,柔性稀释塑造了埃维亚切割区. 这项研究记录了Oligocene早期的高压/低温变形和后来的绿皮石面表面覆盖印记.
科学领域:
- 地质地质地质地质地质地
- 构造学 构造学 构造学 构造学
- 变形主义的变形主义
背景情况:
- 埃维亚岛上的阿尔米罗波塔莫斯 (Almyropotamos) 构造窗口与两个不同的希腊推力板相对应:基底单位和环岛蓝岩单位.
- 沿埃维亚切割区的管稀释使这些单元密切接触,大理石-飞沙序列结构上低于斯特拉大理石.
研究的目的:
- 为了研究Almyropotamos构造窗口的结构和变形演变.
- 用地质年代学来确定变形事件的时间.
- 了解埃维亚切割区在爱琴海挖掘过程中的作用.
主要方法:
- 在flysch和相关单元中对不同石型的结构分析.
- 微结构分析包括石英c轴分布.
- 在现场40Ar/39Ar和87Rb/87Sr地质年代学.
主要成果:
- 确定了两种不同的变形事件:一个早期的奥利古森高压/低温 (HP-LT) 事件和一个晚期的奥利古森-早期的米奥森绿皮石面膜重印.
- 埃维亚切割区表现出柔性稀释和应变分区,变形织物在皮质矩阵和分散块之间变化.
- 地质年代学证实了这两个构造变态事件的时间.
结论:
- 阿尔米罗波塔莫斯的构造窗口记录了复杂的变形和变形历史,包括一个不寻常的扩散和不连续的剪切区域风格.
- 这种风格可能代表了混合主机剪切区域的模型,可以在俯冲和挖掘过程中适应渐进式应变.
- 这项研究为爱琴海地区的构造演变提供了新的地质年代学约束.
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