一个长段的蛇形化枯竭地
C Johan Lissenberg1, Andrew M McCaig2, Susan Q Lang3
1School of Earth and Environmental Sciences, Cardiff University, Cardiff, UK.
概括
研究人员研究了深层地幔岩石,揭示了岩石和元素循环的洞察力. 这些发现显示了地幔的组成和倾斜的融化运输,挑战了关于地幔结构的先前假设.
科学领域:
- * 地球科学
- * 地质化学
- * 石化学
背景情况:
- * 地球的上层地幔对于理解岩,地形成和元素循环至关重要.
- 之前对地幔构成和演变的了解主要依赖于间接方法和表面采样.
- * 蛇形深层地幔石提供了对地球深层过程的独特视角.
研究的目的:
- * 为了分析一段恢复的蛇形化深地幔石.
- * 调查地幔的组成,矿物学,以及融化流动的影响.
- 了解水热流体与岩石的相互作用及其对地幔变化的影响.
主要方法:
- * 1268米长的蛇形化深海地幔石的回收和分析.
- * 检查矿物学和化学组成以推断地幔过程.
- * 对变化模式和流体岩石相互作用区域的绘制.
主要成果:
- 经过回收的矿石呈现出被耗尽的组成,其矿物质变化由流控制.
- * 砂岩区域显示中间的陷,表明斜的融化运输而不是原来的织物.
- 整个部分都明显出现了广泛的热水变化,氧化集中在上200米.
- * 变化模式与附近的迷失城水热场所观察到的风口液体组成相关.
结论:
- 这项研究直接证实了地幔的组成和复杂的融化流动.
- *斜运输对地幔结构和矿物学产生重大影响.
- 水热过程在上层地幔岩石的变化中起着重要作用,对元素循环有影响.
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