概括
红海热区的热区.
科学领域:
- 地质化学 地质化学
- 海洋地质学海洋地质学
背景情况:
- 红海热区含有富含重金属的沉积物.
- 以前的理论认为巴布·曼德布海峡是盐水的来源.
研究的目的:
- 为了调查红海热区正在进行的过程.
- 为了确定盐水的来源及其沉积物.
主要方法:
- 1971年前往红海热区的探险队.
- 对盐水的温度进行测量.
- 分析水量和温度的增加.
- 断裂区的地质评估. 断裂区的地质评估.
主要成果:
- 盐水温度升高,表明重金属沉积物正在活跃形成.
- 在52个月内增加了大约0.346立方公里的水 (最低温度为104°C).
- 计算表明一个浅的,当地的盐水源,而不是巴布·埃尔·曼德布海峡.
结论:
- 红海热区形成重金属沉积物的地质过程仍然活跃.
- 一个局部的,浅浅的来源是盐水的可能来源,由断裂区域证明.
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