概括
海底火山喷发的托莱伊特基岩石创造了独特的状石沉积物. 高岩水含量驱动爆炸性的海底火山活动,形成火岩沉积物.
科学领域:
- 地质地质地质地质地质地
- 火山学 火山学是一门学科.
- 海洋地质学海洋地质学
背景情况:
- 海底火山喷发可以产生类似于空中火山的沉积物.
- 背弧裂是火山活动较大的地点.
研究的目的:
- 描述一个独特的海底火岩沉积物.
- 为了研究深海海底托莱伊特基岩的喷发过程.
主要方法:
- 对135米厚的火岩沉积物的分析.
- 沉积物的古磁分析.
主要成果:
- 该沉积物是由100万年前的托莱伊特基岩岩在>1800米深处形成的,是一种状岩.
- 有证据表明,泡聚酸盐在海底喷发柱或海底上接.
- 古磁性倾向在小于2.5米的尺度上是随机的.
- 岩中的水含量 (重量为1.3%) 显著增加了爆炸性.
结论:
- 深海喷发可以产生爆炸性活动,并聚集沉积物,类似于空中喷发.
- 高岩水含量是推动爆炸性海底火山活动的关键因素.
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