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

Autor: Maron M.[1], Muttoni G.[1], Rigo M.[2, Gianolla P.[4], Kent D.V.[5

Publikováno v: Palaeogeography, palaeoclimatology, palaeoecology 517 (2019): 52–73. doi:10.1016/j.palaeo.2018.11.024
info:cnr-pdr/source/autori:Maron M.[1], Muttoni G.[1], Rigo M.[2,3], Gianolla P.[4], Kent D.V.[5,6]/titolo:New magnetobiostratigraphic results from the Ladinian of the Dolomites and implications for the Triassic geomagnetic polarity timescale/doi:10.1016%2Fj.palaeo.2018.11.024/rivista:Palaeogeography, palaeoclimatology, palaeoecology/anno:2019/pagina_da:52/pagina_a:73/intervallo_pagine:52–73/volume:517

We investigated for magnetostratigraphy the Rio Nigra and Rio Frommer stratigraphic sections from Alpe di Siusi/Seiser Alm (Dolomites, northern Italy) in order to improve the calibration of the Triassic time scale. Both sections are characterized by

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http://hdl.handle.net/11392/2397643