Data for: New magnetobiostratigraphic results from the Ladinian of the Dolomites and implications for the Triassic geomagnetic polarity timescale

Published: 18 December 2018| Version 1 | DOI: 10.17632/n95skz67t6.1
Matteo Maron, Manuel Rigo, Piero Gianolla, Dennis V. Kent, Giovanni Muttoni


Supplementary Table S1: ChRM components from Rio Nigra and Rio Frommer stratigraphic sections. Data are in core, in situ, and tilt-corrected coordinates. Legend of the header is at the end of the table. Supplementary Table S2: Ages and durations of the chrons of the GPTS. The name of the chrons refers to the name of the magnetozones of origin. The mean polarity reversal rates for Early, Middle and Late Triassic (reversal/Myr) have been obtained through linear regression. Figure S1: Anisotropy of Magnetic Susceptibility carried out on the samples from Rio Nigra and Rio Frommer sections. Figure S2: Detail of the Middle Triassic interval of the GPTS/Age plot showing the error bars of the U-Pb zircon ages from Seceda (Wotzlaw et al., 2018) and Rio Nigra (Mietto et al., 2012).



Paleomagnetism, Geochronology, Magnetostratigraphy