Determination of geological sample ages using nuclear analysis methods Article Swipe
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· 2025
· Open Access
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· DOI: https://doi.org/10.29227/im-2025-01-02-029
The determination of geological sample ages is a fundamental aspect of geoscience, offering insights into the history and development of Earth's crust. This study employs the Uranium - Thorium - Lead (U - Th - Pb) method to accurately date sediment samples from the Viet Phuong 2 quarry in Loc Thanh, Binh Phuoc province, Vietnam. Using Total Reflection X - Ray Fluorescence (T - XRF) and gamma spectrometry, the study measured lead, uranium, and thorium concentrations in the samples. The analysis revealed that the ages of the samples ranged from approximately 228 million to 435 million years, consistent with the geological history of the area. Specifically, the U - Pb dating method provided a more accurate and consistent age range, while the Th - Pb method showed slightly higher variability. These results confirm the reliability of the U - Th - Pb dating method and suggest its broader application in geological studies.
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- Type
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- OA Status
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Raw OpenAlex JSON
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https://doi.org/10.29227/im-2025-01-02-029Digital Object Identifier
- Title
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Determination of geological sample ages using nuclear analysis methodsWork title
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articleOpenAlex work type
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2025Year of publication
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2025-09-01Full publication date if available
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Pham Duy Hoai, Cao Thi Kieu Oanh, Truong Huu Ngan Thy, Hanpyo Hong, Đinh Quoc Tuan, Nguyen Thi Minh Sang, Lei HaoList of authors in order
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https://doi.org/10.29227/im-2025-01-02-029Publisher landing page
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https://inz-min.online/index.php/im/article/download/1717/3287Direct link to full text PDF
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YesWhether a free full text is available
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diamondOpen access status per OpenAlex
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0Total citation count in OpenAlex
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