Applicability of low-temperature thermochronology to the evolution of young (< ~ 5 Ma) orogenic systems: a case study from the Japanese Islands
Abstract Low-temperature thermochronology, including fission track (FT) and (U–Th–Sm)/He thermochronometry, has been widely used to constrain the exhumation history of orogenic systems over timescales of 106–108 years. This research employed simple numerical modeling to evaluate the applicability of...
محفوظ في:
| المؤلفون الرئيسيون: | , |
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| التنسيق: | Artigo |
| اللغة: | Inglês |
| منشور في: |
SpringerOpen
2025-07-01
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| سلاسل: | Progress in Earth and Planetary Science |
| الموضوعات: | |
| الوصول للمادة أونلاين: | https://doi.org/10.1186/s40645-025-00735-1 |
| الوسوم: |
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