来自循环平流图的地球-月球动态揭示了在中原生态时代可能发生的海洋潮共振
Maoyang Zhou1,2,3,4, Huaichun Wu1,2,3, Linda A Hinnov4
1State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences (Beijing), Beijing, China.
Science advances
|August 2, 2024
概括
来自中国古老岩层的新循环平面图学数据为地球月球演变提供了洞察力. 这项研究对中原生态时期的地球与月球的分离和潮消散提供了微弱的限制.
科学领域:
- 地质科学 地质科学
- 古气候学 古气候学
- 地球和月球之间的动态.
背景情况:
- 循环轨道图谱为理解地球月球系统历史提供了关键数据.
- 中原生态时代 (1.01.6亿年前) 的循环平流图记录有限,阻碍了地球和月亮的分离和潮消散的精确约束.
研究的目的:
- 为了研究地球-月球系统在中原生态时代的演变.
- 分析来自中国形成的循环平面图形数据,以限制潮消散历史.
主要方法:
- 从中国的Yemahe,Wumishan和Chuanlinggou形成的循环平面图分析.
- 应用贝叶斯反转方法来解释循环平面图段.
- 将新数据与以前的发现整合起来,以更新地球-月球演化模型.
主要成果:
- 分析了来自约12亿至16亿年中国形成的新循环平面图形数据.
- 构建了25亿年前后的最新地球月球系统演化和潮消散历史.
- 观察到与模型预测一致的潮消散峰值,以及潜在的中原生态共振波动.
结论:
- 这项研究增强了对中新生代地球月球动态的理解.
- 这些发现在关键地质时期改善了潮消散和地球月球分离的限制.
- 在Mesoproterozoic中潜在的共振波动需要进一步调查.
相关概念视频
Tidal Forces
2.5K
The origin of Earth's ocean tides has been a subject of continuous investigation for over 2000 years. However, the work of Newton is considered to be the beginning of the proper understanding of the phenomenon. Ocean tides are the result of gravitational tidal forces. These same tidal forces are present in any astronomical body; they are responsible for the internal heat that creates the volcanic activity on Io, one of Jupiter's moons, and the breakup of stars that get too close to...
2.5K
Simple Harmonic Motion and Uniform Circular Motion
4.2K
While simple harmonic motion and uniform circular motion may be two separate concepts, they correlate and interlink with each other. Simple harmonic motion is an oscillatory motion in a system where the net force can be described by Hooke's law, while uniform circular motion is the motion of an object in a circular path at constant speed.
There is an easy way to produce simple harmonic motion by using uniform circular motion. For instance, consider a ball attached to a uniformly rotating...
There is an easy way to produce simple harmonic motion by using uniform circular motion. For instance, consider a ball attached to a uniformly rotating...
4.2K
Gravitation
6.4K
In the years before Newton, a general belief prevailed that different laws governed objects in the sky than objects on Earth. When Kepler wrote down the three laws of planetary motion, explaining in detail the geometrical properties of the planetary orbits around the Sun, there was no immediate idea to discern their connection with more fundamental laws. It was Isaac Newton who, in 1665–66, figured out the connection between planetary motion, the motion of the moon around the Earth, and...
6.4K
Atomic Nuclei: Larmor Precession Frequency
1.2K
The earth's gravitational field produces a 'twisting force' perpendicular to the angular momentum of a spinning mass (such as a spinning top) that causes the mass to 'wobble' around the gravitational field axis in a phenomenon called precession. Similarly, the magnetic moment (μ) of a spinning nucleus precesses due to an external magnetic field directed along the z-axis. The precession of the magnetic moment vector about the magnetic field is called Larmor precession,...
1.2K
Global Climate Change
24.3K
Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
24.3K
Influence of Earth's Curvature and Atmospheric Refraction on Leveling
89
During leveling, the Earth's curvature and atmospheric refraction introduce deviations in the line of sight from a true horizontal reference. When the line of sight is leveled, it remains perpendicular to the plumb line only at a single point. Beyond this, it deviates due to the Earth’s curvature, represented by the correction C. For a sight distance D, the deviation can be derived using the relationship:This relationship shows that the deviation increases quadratically with distance.
89


