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相关概念视频

Conditions on Early Earth02:06

Conditions on Early Earth

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Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
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Global Climate Change01:50

Global Climate Change

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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.
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Isothermal Processes01:21

Isothermal Processes

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A thermodynamic process that occurs at constant temperature is called an isothermal process. Heat slowly flows into the system or out of the system to maintain thermal equilibrium. Processes involving phase changes like water evaporation into steam or freezing water into ice at a constant temperature are examples of Isothermal Processes.
An ideal gas can also undergo isothermal expansion or compression.
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Magnetostatic Boundary Conditions01:28

Magnetostatic Boundary Conditions

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An electric field suffers a discontinuity at a surface charge. Similarly, a magnetic field is discontinuous at a surface current. The perpendicular component of a magnetic field is continuous across the interface of two magnetic mediums. In contrast, its parallel component, perpendicular to the current, is discontinuous by the amount equal to the product of the vacuum permeability and the surface current. Like the scalar potential in electrostatics, the vector potential is also continuous...
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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. Over a...
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Atomic Nuclei: Nuclear Relaxation Processes01:23

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In the absence of an external magnetic field, nuclear spin states are degenerate and randomly oriented. When a magnetic field is applied, the spins begin to precess and orient themselves along (lower energy) or against (higher energy) the direction of the field. At equilibrium, a slight excess population of spins exists in the lower energy state. Because the direction of the magnetic field is fixed as the z-axis,  the precessing magnetic moments are randomly oriented around the z-axis.
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相关实验视频

Updated: Nov 17, 2025

Isolation of Quartz Grains for Optically Stimulated Luminescence OSL Dating of Quaternary Sediments for Paleoenvironmental Research
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在地球的中年时代产生的静止

Ming Tang1, Xu Chu2, Jihua Hao3,4

  • 1Key Laboratory of Orogenic Belt and Crustal Evolution, MOE; School of Earth and Space Science, Peking University, Beijing 100871, China. mingtang@pku.edu.cn.

Science (New York, N.Y.)
|February 12, 2021
PubMed
概括

地球山脉形成的历史显示,在古世和世时代,地的厚度最高. 由于超级大陆的存在,原生态时期的山脉活动有所减少,这可能阻碍了生命的进化.

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科学领域:

  • 地质学
  • 地质化学
  • 古生物学

背景情况:

  • 山地带对于营养循环至关重要,影响排泄和水文.
  • 了解长期的山脉形成过程是地球表面演变的关键.

研究的目的:

  • 用地化学代理来重建山脉形成的历史.
  • 研究大陆地的厚度与地质时间上的活动之间的关系.

主要方法:

  • 作为追踪山脉形成的替代物,
  • 分析了地质时代的活跃大陆地厚度的变化.

主要成果:

  • 大陆地的厚度在阿纪和法内罗纪时期达到顶峰.
  • 原生态时代表现出地厚度的持续下降,与最小的orogenesis.
  • 长期的原生态静止与Nuna-Rodinia超大陆有关.

结论:

  • 超大陆周期对地幔的热结构和岩层强度产生重大影响,影响了山脉的形成.
  • 在前世时期缺乏重要的山脉形成可能导致海洋营养物质的限制和进化进程的停滞.