Assessment of Factors Controlling Clumped Isotopes and δ18O Values of Hydrothermal Vent Calcites
The clumped isotope composition of CaCO3 (Δ47) is a geochemical proxy that can provide mineral formation temperatures and, together with...
Origin and distribution of calcite cements in a folded fluvial succession: The Puig‐reig anticline (south‐eastern Pyrenees)
As one of the predominant diagenetic products in clastic rocks, calcite cements are typical fingerprints of cement-forming fluids and are...
Constraining stratal architecture and pressure barriers in the subsalt Karachaganak Carboniferous carbonate platforms using forward stratigraphic modelling
Predicting reservoir quality and pressure barriers is a challenging task in carbonate systems. In this paper, we present new model...
Evolution of hot fluids in the Chingshui geothermal field inferred from crystal morphology and geochemical vein data
The Chingshui geothermal field once hosted the first geothermal power plant in Taiwan from 1981 to 1993. After a long...
Interplay between depositional facies, diagenesis and early fractures in the Early Cretaceous Habshan Formation, Jebel Madar, Oman
Diagenesis and fracturing can significantly alter petrophysical properties of subsurface carbonate reservoirs, but the impacts of these processes at the...
Evaluating climatic response to external radiative forcing during the late Miocene to early Pliocene: New perspectives from eastern equatorial Pacific (IODP U1338) and North Atlantic (ODP 982)
Orbital‐scale climate variability during the latest Miocene‐early Pliocene is poorly understood due to a lack of high‐resolution records spanning 8.0–3.5 Ma,...
Geostatistical modelling of cyclic and rhythmic facies architectures
A Pluri-Gaussian method is developed for facies variables in three dimensions to model vertical cyclicity related to facies ordering and...
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...
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...
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...