大陆积累的动态 大陆积累的动态
L Moresi1, P G Betts2, M S Miller3
11] School of Geosciences, Monash University, Clayton, Victoria 3800, Australia [2] School of Mathematical Sciences, Monash University, Clayton, Victoria 3800, Australia [3] School of Earth Sciences, University of Melbourne, Parkville, Victoria 3010, Australia.
Nature
|March 28, 2014
概括
积累性山脉带在聚合板块边缘形成. 三维模型揭示了俯冲区是如何演变的,形成曲的气系统,并使沟迁移导致后方弧度逃逸.
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
- 地力学是什么?地力学是什么?
背景情况:
- 积累性orogen,大陆生长的场所,在聚合板边缘形成,在那里,俯冲区消耗浮动地.
- 例如包括北美 Cordilleras,西南太平洋的降温区,塔斯马尼德和Altaïdes.
- 长寿命的积累性orogens经历地延伸和背弧盆地发展,与探回滚有关.
研究的目的:
- 模拟从初始碰撞到稳定的收边缘的演变.
- 为了调查orogenic曲率和后方弧形构造逃逸的发展.
- 了解沟迁移在复杂的矿产系统中的作用.
主要方法:
- 盘边缘演变的三维动态建模.
- 对地质和地物理证据的分析.
主要成果:
- 模型显示保证金不稳定,随后重新建立稳定的收率.
- 显著的orogenic系统曲率和后方弧度逃逸机制被插图.
- 侧面沟回滚,与板边界平行迁移,推动了系统的复杂性.
结论:
- 被浮动地所造成的降温区拥堵导致了增积性或原体的形成和大陆的生长.
- 沟回滚和迁移是开发复杂,曲的矿产系统的关键机制,并促进后方弧度逃逸.
- 这个过程是一个反复发生的全球现象,在塔斯马尼德群岛中得到了证据.
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