概括
中大西洋山脊裂纹区域的超级巨型物体揭示了浅水石灰岩. 这些地质形成表明,在随后的大西洋开放之前,这些岩石在一个狭窄的原大西洋中沉积.
科学领域:
- 地质地质地质地质地质地
- 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:
- 由上层地幔超大质体组成的横脊,发生在中大西洋脊交于赤道断裂区域的地方.
- 这些位于偏移区域的超级物体在分离的地板之间起到防扩散的作用.
研究的目的:
- 调查中大西洋山脊横向超级巨型天体的地质组成和起源.
- 为了解释这些超级巨型结构上浅水石灰岩的存在.
主要方法:
- 在Vema断裂区的横向超岩体的地质检查.
- 石灰岩组成的分析,包括破碎颗粒 (石英,微克林,正方体).
主要成果:
- 在Vema断裂区的超大质体上发现了直径高达1毫米的破碎粒的浅水石灰岩.
- 超体在扩散的地板中充当不扩散的块.
结论:
- 石灰石很可能沉积在一个狭窄,浅的原大西洋.
- 这些沉积物随后随着大西洋的扩大而留在后面.
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