geochronometry

geochronometry的音标是[ˌdʒiːəʊkrəʊnəˈmeɪtɪ]或[ˌdʒiːəʊkrəʊnɪˈmeɪtɪ]，意思是利用放射性测定地质年代的方法。

基本翻译为“地质年代测定法”。

速记技巧可以结合其英文名称记忆，可以尝试将其想象成中文的“给年代测量”，这样可以帮助快速记住其发音和含义。

Geochronometry（地层年代测定法）这个词的英文词源是geology（地质学）和chronology（年代学）的结合。它是一种通过测量和分析地质材料中的放射性衰变过程，来确定地层形成年代的方法。

变化形式：复数形式是geochronometry，过去式是geochronized，现在分词是geochronizing。

相关单词：

1. Geochronology - 地层年代学：这是geochronometry的一个分支，专门研究如何通过地层年代测定法来确定地层的形成年代。

2. Isotope geochronology - 同位素地层年代学：这是一种特殊的地层年代测定法，利用放射性同位素衰变来确定地层的年代。

3. Uranium-lead geochronology - 铀铅地层年代学：这是一种常用的同位素地层年代测定法，利用铀和铅的放射性衰变来确定地层的年代。

4. Argon-argon geochronology - 氩氩地层年代学：这也是一种常用的同位素地层年代测定法，利用氩的放射性衰变来确定地层的年代。

5. Radiocarbon geochronology - 放射性碳定年法：这是专门用来测定有机物质（如木材、纸张、骨头等）的年代的方法，因为这些物质中的碳有放射性衰变。

6. Chronometer - 年代计：这是一个专门用来表示地层年代测定的单位，通常用于表示经过测定后的地层形成时间。

7. Chronostratigraphy - 年代地层学：这是地质学的一个分支，专门研究地层和年代之间的关系，以及如何利用地层和年代信息来解释地质历史。

8. Chronozone - 年代界线：这是指两个具有不同年代的地质界线，通常用于表示地层的形成和变化。

9. Chronostratigraphic - 年代地层特征的：这是一个形容词，用来描述具有年代地层意义的地质特征或现象。

10. Geochronological dating - 地层年代测定：这是一个专业术语，用来表示使用geochronometry方法来确定地层的形成年代。

常用短语：

1. geochronometry analysis

2. age determination using geochronometry

3. uranium-lead dating

4. argon-argon dating

5. radiocarbon dating

6. isotope geochronometry

7. zircon geochronometry

例句：

1. The geochronometry analysis of the fossil bones has provided valuable information about the age of the species.

2. The use of uranium-lead dating has revolutionized the study of ancient human remains.

3. The argon-argon dating method has been used to determine the age of rocks and minerals.

4. The radiocarbon dating method has been used to determine the age of organic materials that have decayed since about 1950.

5. The isotope geochronometry approach has been used to study the movement of water and other substances in the Earth"s crust.

6. Zircon geochronometry has been used to determine the age of rocks and to study the movement of tectonic plates.

英文小作文：

Geochronometry is a powerful tool for studying the history of the Earth and its resources. It allows us to determine the age of rocks, minerals, and even ancient biological remains with precision and accuracy. Uranium-lead dating, argon-argon dating, radiocarbon dating, isotope geochronmetry, and zircon geochronmetry are just some of the techniques that are used in geochronometry. These methods have provided us with a better understanding of our planet"s history and have contributed to our knowledge of geological processes and environmental changes. Through geochronometry, we can also investigate the movement of water and other substances in the Earth"s crust, which is essential for understanding the dynamics of our planet"s environment. In conclusion, geochronometry is a crucial tool for studying the Earth"s past and present, and it continues to provide valuable insights into our planet"s history and evolution.