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从太平洋到大西洋的上层地幔流通过德雷克通道的地化学追踪
J A Pearce1, P T Leat, P F Barker
1Department of Earth Sciences, Cardiff University, Cardiff, CF10 3YE, UK. PearceJA@cardiff.ac.uk
Nature
|March 22, 2001
概括
地化学数据显示,太平洋地幔流出到德雷克海峡,这是由区域构造学驱动的,而不是全球质量平衡. 一个地幔域边界存在于德雷克海峡和东苏格兰海之间.
科学领域:
- 地质物理学 地质物理学
- 地质化学 地质化学
- 地球科学 地球科学 地球科学
背景情况:
- 地球上层地幔包括三个主要的水库:太平洋,大西洋和印度洋.
- 太平洋水库正在收缩,而大西洋和印度水库正在扩大,这是由于山脊和俯冲区的动态.
- 从太平洋到大西洋和印度水库的地幔流被提议用于质量平衡,可能通过特定的"门户".
研究的目的:
- 通过德雷克海峡调查太平洋地幔外流的地化学证据.
- 确定这种地幔流动背后的驱动力 (区域构造学与全球质量平衡).
- 为了确定南大洋的地幔领域边界.
主要方法:
- 从德雷克海峡地区的地化学数据分析.
- 对地质化学特征进行比较,以了解地幔水库相互作用.
- 地力学建模以评估地幔流动力学.
主要成果:
- 地化学数据证实太平洋地幔流出到德雷克海峡.
- 外流似乎主要受到区域构造约束的影响.
- 一个地幔域边界,类似于澳大利亚-南极不一致,在德雷克海峡和东斯科提亚海之间被确定.
结论:
- 太平洋地幔流入德雷克海峡的情况已得到证实,但是由当地构造学驱动的.
- 全球质量平衡不是这种特定地幔流动的主要驱动因素.
- 南大洋表现出明显的地幔领域,由显著的边界分开.
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