中洋山脊的地震性揭示了极端类型的海洋岩层
Vera Schlindwein1, Florian Schmid1
1Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Am Alten Hafen 26, 27568 Bremerhaven, Germany.
Nature
|July 1, 2016
概括
地震数据显示,超慢扩散的山脊具有寒冷,厚厚的石化层,深度地震表明了广泛的蛇形化. 这就解释了地的不连续生成和深层流体循环.
科学领域:
- 地质学
- 构造学
- 海洋学
背景情况:
- 超慢扩散的山脊表现出不连续的融化和可变的岩层组成,结构和构造活动.
- 由于有限的地震数据,这些山脊的岩层结构不明.
研究的目的:
- 研究极慢扩散的岩层结构和积累方式.
- 了解岩层结构对融化和流体循环的影响.
主要方法:
- 沿着390公里的超慢扩散脊轴进行了详细的地震调查.
- 对地震分布进行分析,以推断岩层属性.
主要成果:
- 亚马格的部分缺乏浅层地震,但地震深度低至35公里,这意味着冰冷,厚厚的石化层有蛇形化.
- 岩石层在火山中心下面变薄,这表明岩石层-岩石层边界地形在沿轴融化流中的作用.
- 海底变形和流体循环的影响.
结论:
- 超慢扩散的山脊的特点是寒冷,厚厚的石化层与深层变化区域.
- 石化层-石化层边界地形影响了融化分布和地产量.
- 深层流体的循环和变化是海洋岩层形成的重要过程.
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