PLANT DIVERSITY IN A MESOTHERMAL CLIMATE: INSIGHTS FROM THE RIO SAN PEDRO FORMATION (LATE EOCENE, SOUTH-CENTRAL CHILE, 39°S).
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Analytical Method for U-Pb Geochronology and Geochronological Data We conducted U-Pb geochronology on two samples. To determine the depositional ages of a volcanic rock and maximum depositional age, as well as the zircon provenance of a sedimentary rock, we analyzed more than 50 and over 100 zircon crystals per sample, respectively.
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2025-10-02
