概括
由于地厚度的变化,中大西洋山脊的扩散部分表现出负重力异常. 细分中心较厚的地和端端较薄的地,由第三层变异驱动,解释了这些发现.
科学领域:
- 地质物理学 地质物理学
- 海洋地质学海洋地质学
- 板块构造学是一种板块构造学.
背景情况:
- 中大西洋山脊的扩展部分在地幔Bouguer重力场的负牛眼异常的特点.
- 了解这些重力异常的来源对于解释地结构和中洋山脊上的积累过程至关重要.
研究的目的:
- 为了调查在中大西洋山脊的一段地区出现负重力异常的原因.
- 用地震折射数据确定地厚度变化和重力异常之间的关系.
主要方法:
- 在中大西洋山脊33度南方的地震折射数据采集和分析.
- 基于地厚度和第三层变化的重力异常的建模.
主要成果:
- 负牛眼引力异常是由沿着扩散段的地厚度变化解释的.
- 地的厚度在细分中心较大,在细分末端下降.
- 这些厚度变化主要归因于第三层厚度的变化.
结论:
- 地的积累集中在这个缓慢扩散的脊段.
- 轴谷的深度与底层地的厚度直接相关.
- 在解释来自中洋山脊的重力数据时,必须考虑沿轴密度变化.
相关概念视频
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