概括
使用-和-同位素的地质年代学研究显示,加拿大盾牌的高级,奴隶和丘吉尔省在25亿至27亿年前形成,为大陆地演变提供了洞察力.
科学领域:
- 地质化学 地质化学
- 同位素地质学的同位素.
- 地质时间学 (Geochronology)
背景情况:
- 了解大陆地的形成和演变对于破译地球的地质历史至关重要.
- 同位素系统学提供了强大的工具来测定地质材料的年代和追踪它们的起源.
研究的目的:
- 为了确定大陆地特定部分的形成年龄.
- 研究加拿大盾牌的地化学演变.
主要方法:
- 使用- (Sm-Nd) 和- (Rb-Sr) 的同位素系统.
- 从加拿大盾牌的高级,奴隶和丘吉尔结构省份分析复合样本.
- 应用关于大陆地的地化学演变的可信假设.
主要成果:
- 加拿大盾牌的高级,奴隶和丘吉尔结构省份是在25亿至27亿年前 (eons) 形成的.
- 沉积岩中的-同位素系统在沉积和二代生成过程中似乎在很大程度上不受干扰,这使得可靠的来源年龄确定.
结论:
- 加拿大盾牌的主要结构性省份具有连贯的形成年龄范围.
- 沉积物的-测年是一种可行的方法来确定沉积物来源的年龄,有助于我们了解地的演化.
更多相关视频
相关概念视频
Radioactive Decay and Radiometric Dating
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.
The Fossil Record
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...
Nuclear Stability
Protons and neutrons, collectively called nucleons, are packed together tightly in a nucleus. With a radius of about 10−15 meters, a nucleus is quite small compared to the radius of the entire atom, which is about 10−10 meters. Nuclei are extremely dense compared to bulk matter, averaging 1.8 × 1014 grams per cubic centimeter. If the earth’s density were equal to the average nuclear density, the earth’s radius would be only about 200 meters.
To hold positively charged protons together in the...
To hold positively charged protons together in the...
Speciation Rates
Speciation can proceed at markedly different rates, and evolutionary biologists commonly describe these differences through the models of gradualism and punctuated equilibrium. Both patterns explain how new species arise, but they differ in the tempo and continuity of evolutionary change. In both cases, evolutionary change arises from heritable variation within populations, with natural selection often shaping traits that improve survival and reproduction under specific environmental conditions.
Conditions on Early Earth
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.
Diversity of Protists III
Rhizaria are a diverse group of unicellular protists characterized by their threadlike cytoplasmic extensions known as pseudopodia. These structures aid in both locomotion and feeding, giving Rhizaria an amoeboid appearance. Their amoeboid morphology once led to taxonomic confusion, but molecular phylogenetics has clarified their evolutionary placement and emphasized their shared use of pseudopodia despite divergent lineages.This clade comprises diverse lineages such as Chlorarachniophyta,...


