协同产生的崩:从中间地的角度来看,原生态的格伦维尔或原体
概括
格伦维尔原体中发生的一大延伸断层与推进一起发展,表明由于超出了学极限而导致地的崩. 这一前生态时期的事件反映了现代喜马拉雅山脉的orogenic过程.
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
- 结构地质学 结构地质学
背景情况:
- 加拿大安大略省的格伦维尔地层提供了一个关键的窗口,可以了解中期到晚期的原生代构造活动.
- 了解包括断层和变形在内的orogenic过程对于重建地球地质历史至关重要.
研究的目的:
- 调查格伦维尔矿物质的结构,岩石学和地质年代学演变.
- 为了确定扩展断层,推进和变态在orogenesis期间之间的关系.
- 为了比较Proterozoic orogenic过程与现代的例子,如喜马拉雅山脉.
主要方法:
- 岩石形成的结构分析.
- 岩石样本的 Petrological 检查. 岩石样本的石油学检查.
- 地质年代测定用于建立时间线.
主要成果:
- 一个显著的延伸故障与格伦维尔orogen的后期推进同步启动.
- 这个断层在地内延伸到至少25公里的深度.
- 断层,变形和压缩的时间和空间分布表明地过度加厚,随后崩.
结论:
- 同源性崩是由地超过其性支能力引发的.
- 像格伦维尔这样的前生代产带在生理学高度,地厚度和强度上与现代产带系统 (如喜马拉雅山脉) 有共同之处.
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