Mechanisms of near‐normal sea water dolomitisation: Mesohaline‐reflux or syn‐depositional?

Abstract The Eocene Epoch is characterised by multiple hyperthermals, which promoted extensive carbonate sediment deposition and dolomitisation, particularly across the Arabian Plate. The Dammam Formation, a key Eocene aquifer and hydrocarbon‐bearing unit in the Arabian platform, is extensively dolo...

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Autors principals:	Misbahu Abdullahi, Adhipa Herlambang, Khalid Al‐Ramadan, Ardiansyah Koeshidayatullah
Format:	Artigo
Idioma:	Inglês
Publicat:	Wiley 2026-02-01
Col·lecció:	The Depositional Record
Matèries:	Dammam Formation Eocene mesohaline reflux sea water dolomitisation syn‐depositional dolomitisation
Accés en línia:	https://doi.org/10.1002/dep2.70039
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