在完好无损的海洋地中钻探gabbro
Douglas S Wilson1, Damon A H Teagle, Jeffrey C Alt
1Department of Earth Science and Marine Science Institute, University of California, Santa Barbara, CA 93106, USA. dwilson@geol.ucsb.edu
概括
科学家在东太平洋钻探了海洋地,证实融化镜头以更快的传播速度形成更浅的层次. 这提供了对中海脊地形成的关键见解.
科学领域:
- 地质地质地质地质地质地
- 海洋学 海洋学 海洋学
- 石化学 石化学是一门学科.
背景情况:
- 了解中海山脊上的海洋地形成需要采样完整的岩,堤和布的序列.
- 通过科学海洋钻探进入这些深层地的部分一直是一个长期的挑战.
研究的目的:
- 为了研究海洋地以超快速传播速度的形成和演变.
- 为了取样gabbroic岩石,代表水晶化融化镜片下一个中海山脊.
主要方法:
- 在太平洋东部的洞1256D进行科学海洋钻探.
- 地质采样和回收岩核的分析,包括gabbros,堤和岩.
主要成果:
- 在海洋地的第2层地震层内,Gabbro在1157米深处被到达.
- 加布罗的深度证实,在更浅的位置,在更快的传播条件下,融化镜片形成.
- 回收的加布罗斯侵入了变形的板状堤,并且与覆盖的岩有着共同的组成相似之处.
结论:
- 这些发现支持地震预测,关于在超快速扩散的山脊上发生浅层融化镜片的地震预测.
- 采样的gabbros可能代表了结晶的融化透镜,直接位于轴下方.
- 这项研究表明,透的融化透镜可能不是累积下层海洋地的主要来源.
相关概念视频
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