“…[12][13][14][15][16][17][18][19][20][21][22][23][24][25][26][27][28][29][30] Geochronology: Because natural monazites are often U and Th enriched minerals, radiogenic Pb accumulates quickly through the ␣,  decay sequences in the three natural radioactive families, and reaches, in about 100 Ma, a level where its analysis becomes possible by electron probe microanalysis (EPMA). 31 Assuming that common Pb is negligible, and that radiogenic Pb is kept in the structure all along the time excluding lead loss when ageing, 32,33 the simultaneous measurement of U, Th, and Pb allows to reach the geologically meaningful age from a single electron probe analysis.…”