Persisting Rock-Buffered Conditions in the Upper Triassic and Lower Jurassic Dolomites of the Central Apennines (Italy) During Diagenesis, Burial, and Thrusting

Persisting Rock-Buffered Conditions in the Upper Triassic and Lower Jurassic Dolomites of the Central Apennines (Italy) During Diagenesis, Burial, and Thrusting

Basin-scale dolomitization of carbonate sequences occurs over long time spans and results from diagenesis, burial, and tectonically driven fluid fluxes. Depicting the different geological processes producing dolomitized carbonate sequences requires combining accurate field, petrographic, and geochem...

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Bibliographic Details
Main Authors: Alessio Lucca, Silvia Mittempergher, Fabrizio Balsamo, Anna Cipriani, Antonino Cilona, Fabrizio Storti
Format: Article
Language:English
Published: MDPI AG 2025-01-01
Series:Geosciences
Subjects:
dolomitization
clumped isotopes
rock-buffered conditions
seawater dolomitization
periadriatic platform
Online Access:https://www.mdpi.com/2076-3263/15/2/35
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