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超大陆的周期和计算绝对的古长度在深时间
Ross N Mitchell1, Taylor M Kilian, David A D Evans
1Yale University, 210 Whitney Avenue, New Haven, Connecticut 06511, USA. ross.mitchell@yale.edu
Nature
|February 10, 2012
概括
一个新的正向性模型预测未来的超级大陆与过去的超级大陆形成90°,挑战了内向性和外向性理论. 这种超大陆周期模型得到了来自努纳,罗丁尼亚和潘盖亚的真极流浪数据的支持.
科学领域:
- 地质物理学 地质物理学
- 板块构造学是一种板块构造学.
- 地球科学 地球科学 地球科学
背景情况:
- 超大陆周期模型传统上通过内向或外向预测未来超大陆的形成.
- 现有的模型不能完全解释连续的超级大陆之间的空间关系.
研究的目的:
- 提出和验证超大陆形成的新"正向"模型.
- 为了研究过去超级大陆的空间分布,使用真正的极地漫游数据.
主要方法:
- 开发了orthoversion模型,假定超大陆形成与前身相距90°.
- 根据地球的非水静态形状和最小惯性瞬间计算真极流浪.
- 在超大陆上安装大圆,以确定弧距.
主要成果:
- 正向转变模型预测超大陆中心形成大约90°的距离.
- 对努纳,罗丁尼亚和潘盖亚的分析表明,连续的中心相隔88°和87°,支持正向模式.
- 已识别的超大陆中心为计算绝对古长度提供了固定点.
结论:
- 正向转变模型为理解超大陆周期提供了一个新的框架.
- 真极流浪分析验证了 orthoversion 模型的预测.
- 改进的古长度限制将增强古代板块运动和生物地理学的重建.
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