王世成, 荆贵茹, 康铁生
Abstract
Apatite fission tracks have become an important and unique geothermometer for investigating a variety of processes that affect the thermal structure of the upper crust as a result of their sensitivity to temperatures between 20℃ and 150℃ for most geologically reasonable time scales. Inverse mode...
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Apatite fission tracks have become an important and unique geothermometer for investigating a variety of processes that affect the thermal structure of the upper crust as a result of their sensitivity to temperatures between 20℃ and 150℃ for most geologically reasonable time scales. Inverse mode...
Key concepts: Fission track dating, Apatite, Fission, Upper crust, Geology, Thermal, Inverse, Crust