概括
水热喷口将释放到海洋中,形成一个宽的羽毛,作为海底反应的标志物. 这表明,在东太平洋上升沿线广泛存在低温液体通风.
科学领域:
- 地质化学 地质化学
- 海洋学 海洋学 海洋学
- 海洋地质学 海洋地质学
背景情况:
- 海洋中山脊上的热水活动会向海洋释放化学特征.
- 了解这些签名有助于追踪地质过程和海洋化学.
研究的目的:
- 为了研究作为水热活动的标记物.
- 为了描述沿着东太平洋海拔的热水喷发的性质.
主要方法:
- 对海洋水柱地质化学的分析.
- 在东太平洋上升层上方的羽的映射.
主要成果:
- 在东南太平洋上方的水柱中观察到的缩.
- 检测到一个广泛的,扩散的羽毛,与其他标记物的尖羽毛形成鲜明对比.
- 这表明普遍存在的低温热水流体通风.
结论:
- 作为一种新的海洋标志物,用于水热变化.
- 扩散的日耳曼羽毛表明大范围的,低温的通风脱离主脊轴.
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