Timing and magnitude of Miocene eustasy derived from the mixed siliciclastic-carbonate stratigraphic record of the northeastern Australian margin
Eustasy is a key parameter to understand sedimentary sequences on continental margins and to reconstruct continental ice volume in the...
Diagenetic Implications of Stylolitization In Pelagic Carbonates, Canterbury Basin, Offshore New Zealand
Stylolites are irregular discontinuity surfaces that are thought to result from localized stress-induced dissolution during burial or tectonic compression. The...
Benthic foraminiferal biotic events related to the Paleocene–Eocene Thermal Maximum along the California margin
The faunal expression of the Paleocene-Eocene Thermal Maximum (PETM) is well documented in deep-sea sediments. However, few studies have examined...
Controls on the formation of stratabound dolostone bodies, Hammam Faraun Fault block, Gulf of Suez
Dolomitization is commonly associated with crustal‐scale faults, but tectonic rejuvenation, diagenetic overprinting and a fluid and Mg mass‐imbalance often makes...
Relationship between karstification and burial dolomitization in Permian platform carbonates (Lower Khuff—Oman)
Large breccia fabrics associated with karst constitute an important structure in massive limestone successions. The dimensions and shapes of breccia...
Determination of the spatial distribution of wetting in the pore networks of rocks
The macroscopic movement of subsurface fluids involved in CO2 storage, groundwater, and petroleum engineering applications is controlled by interfacial forces...
Clumped-isotope thermometry of magnesium carbonates in ultramafic rocks
Magnesium carbonate minerals produced by reaction of H2O–CO2 with ultramafic rocks occur in a wide range of paragenetic and tectonic...
Evidence of taxonomic non-equilibrium effects in the clumped isotope composition of modern cephalopod carbonate
The stable oxygen isotope composition (δ18O) of ammonites and belemnites is a common proxy for Jurassic and Cretaceous sea temperatures....
Effects of oxygen plasma ashing treatment on carbonate clumped isotopes
For clumped isotope analysis (Δ47), hydrocarbon and organic molecules present an important contaminant that cannot always be removed by CO2...
Burial estimates constrained by clumped isotope thermometry: example of the Lower Cretaceous Qishn Formation (Haushi-Huqf High, Oman)
Accurate determination of the thermal history of sedimentary basins is critical to constrain the timing of diagenetic processes. Here, clumped...