https://atpase-signaling.com/i....ndex.php/your-ms-del
After the Late Permian, coal-bearing strata underwent a substantial post-depositional annealing, as indicated by the age and length of apatite fission tracks (AFTs), suggesting an unusual thermal event in the Late Mesozoic. A maximum paleotemperature of 140 degrees Celsius characterized the Meso-Cenozoic thermal event, primarily driven by Early Jurassic plutonic metamorphism
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