地球地中浅层断层的年代测定
B A van der Pluijm1, C M Hall, P J Vrolijk
1Department of Geological Sciences, University of Michigan, Ann Arbor, Michigan 48109, USA. vdpluijm@umich.edu
Nature
|July 13, 2001
概括
浅层断层的放射测年是具有挑战性的,因为矿物质年龄混合. 这项研究引入了一种使用X射线建模的新方法,可靠地测定近地表面断层活动的日期,揭示了北美西部显著的压力体制转变.
科学领域:
- 地质地质地质地质地质地
- 地质时间学 (Geochronology)
- 构造学 构造学 构造学 构造学
背景情况:
- 浅层地断层的放射测年是困难的,因为低温阻止矿物质再结晶.
- 浅浅的断层区域保留了碎和异性菌的混合种群,使年龄的确定复杂化.
- 在辐射期间的阿贡-39 (39Ar) 损失可以导致错误的年龄在约会粘土矿物质时.
研究的目的:
- 开发和介绍一种可靠的方法来测定近地表面断层活动的年代.
- 用X射线建模和样本封装来描述断层沟中的粘土种群.
- 为了确定加拿大洛基山脉的易斯推力断层的年龄,并推断构造历史.
主要方法:
- 使用X射线建模来描述断层沟中的粘土矿物种群.
- 采用样品封装技术来提高约会准确度.
- 从易斯推力断层的断层口样本中应用放射测年法.
主要成果:
- 位于加拿大南部洛基山脉的易斯推力断层约有5200万年前.
- 这个年龄表明,北美西部的压力体制在伊欧纪期间从收缩到延伸的快速转变.
- 岩石的提升/挖掘年龄和沉积源估计大约有1.72亿年.
结论:
- 这种方法可靠地确定了近地表面断层活动的日期.
- 易斯推力断层的伊纪时代为北美西部的构造进化提供了关键的见解.
- 这项研究强调了矿物种群的特征化对于在脆弱断层区域进行准确的地球时间学研究的重要性.
相关概念视频
The Fossil Record
23.0K
The fossil record documents only a small fraction of all organisms that have ever inhabited Earth. Fossilization is a rare process, and most organisms never become fossils. Moreover, the fossil record only exhibits fossils that have been discovered. Nevertheless, sedimentary rock fossils of long-lived, abundant, hard-bodied organisms dominate the fossil record. These fossils offer valuable information, such as an organism's physical form, behavior, and age. Studying the fossil record helps...
23.0K
Radioactive Decay and Radiometric Dating
34.6K
Radioactivity is a spontaneous disintegration of an unstable nuclide and is a random process, as all the nuclei in the sample do not decay simultaneously. The number of disintegrations per unit time is called the activity (A), which is directly proportional to the number of nuclei in the sample. The decay constant (λ) is an average probability of decay per nucleus in unit time.
34.6K
Imperfections in Crystal Structure: Point, Line and Plane Defects
150
A perfect crystal, in theory, has a uniform structure with the same unit cell and lattice points throughout. However, any deviation from this periodic arrangement is known as an imperfection or defect. These defects can be categorized into three types: point, line, and plane defects.Point defects occur when there is a deviation from the ideal due to missing atoms, displaced atoms, or additional atoms. These imperfections might occur due to imperfect packing during crystallization or because of...
150
Imperfections in Crystal Structure: Stoichiometric Point Defects
143
Schottky defects arise when some lattice points in a crystal, such as those in NaCl, remain unoccupied, creating lattice vacancies without disturbing the overall electrical neutrality of the crystal. This defect is common in ionic crystals where the positive and negative ions are similar in size, as seen in sodium chloride and cesium chloride. The presence of Schottky defects enables the crystal to conduct electricity to a small extent through an ionic mechanism. Electric fields cause nearby...
143
Fault Types
601
When analyzing a single line-to-ground fault from phase A to ground at a three-phase bus, it is important to consider the fault impedance. This impedance is zero for a bolted fault, equal to the arc impedance for an arcing fault, and represents the total fault impedance for a transmission-line insulator flashover. To derive sequence and phase currents, fault conditions are translated from the phase domain to the sequence domain.
For line-to-line faults occurring between phases B and C, the...
For line-to-line faults occurring between phases B and C, the...
601
Microcracking in Concrete
614
Microcracking in concrete refers to the tiny cracks that can form within the material even before any external load is applied. These microcracks typically occur at the interface between the coarse aggregate and the hydrated cement paste, often as a result of differential volume changes prompted by variations in stress-strain behavior, as well as thermal and moisture movement. Initially, these microcracks remain stable and do not grow substantially until the concrete is stressed to about 30...
614


