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DOLOMITE FORMATION BY NANOCRYSTAL AGGREGATION IN THE DOLOMIA PRINCIPALE OF THE BRENTA DOLOMITES (NORTHERN ITALY)

Upper intra- to supratidal laminites in the Norian Dolomia Principale of the Brenta Dolomites (Northern Italy) commonly consist of aphanitic and partially peloidal dolomite previously interpreted as very early diagenetic or penecontemporaneous. Re-examination of a sample prepared by focused ion beam...

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Hlavní autoři: PATRICK MEISTER, SILVIA FRISIA
Médium: Artigo
Jazyk:Inglês
Vydáno: Milano University Press 2018-12-01
Edice:Rivista Italiana di Paleontologia e Stratigrafia
Témata:
carbonate factory
dolomia principale
dolomite
mudstone
nanocrystals
non-classical pathway of nucleation.
On-line přístup:https://riviste.unimi.it/index.php/RIPS/article/view/11297
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