geochronometry的音標是[?d?i???kr??n??me?t?]或[?d?i???kr??n??me?t?]，意思是利用放射性測定地質年代的方法。

基本翻譯為“地質年代測定法”。

速記技巧可以結合其英文名稱記憶，可以嘗試將其想象成中文的“給年代測量”，這樣可以幫助快速記住其發音和含義。

Geochronometry（地層年代測定法）這個詞的英文詞源是geology（地質學）和chronology（年代學）的結合。它是一種通過測量和分析地質材料中的放射性衰變過程，來確定地層形成年代的方法。

變化形式：復數形式是geochronometry，過去式是geochronized，現在分詞是geochronizing。

相關單詞：

1. Geochronology - 地層年代學：這是geochronometry的一個分支，專門研究如何通過地層年代測定法來確定地層的形成年代。

2. Isotope geochronology - 同位素地層年代學：這是一種特殊的地層年代測定法，利用放射性同位素衰變來確定地層的年代。

3. Uranium-lead geochronology - 鈾鉛地層年代學：這是一種常用的同位素地層年代測定法，利用鈾和鉛的放射性衰變來確定地層的年代。

4. Argon-argon geochronology - 氬氬地層年代學：這也是一種常用的同位素地層年代測定法，利用氬的放射性衰變來確定地層的年代。

5. Radiocarbon geochronology - 放射性碳定年法：這是專門用來測定有機物質（如木材、紙張、骨頭等）的年代的方法，因為這些物質中的碳有放射性衰變。

6. Chronometer - 年代計：這是一個專門用來表示地層年代測定的單位，通常用于表示經過測定后的地層形成時間。

7. Chronostratigraphy - 年代地層學：這是地質學的一個分支，專門研究地層和年代之間的關系，以及如何利用地層和年代信息來解釋地質歷史。

8. Chronozone - 年代界線：這是指兩個具有不同年代的地質界線，通常用于表示地層的形成和變化。

9. Chronostratigraphic - 年代地層特征的：這是一個形容詞，用來描述具有年代地層意義的地質特征或現象。

10. Geochronological dating - 地層年代測定：這是一個專業術語，用來表示使用geochronometry方法來確定地層的形成年代。

常用短語：

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.