Multiple fluid flow events from salt‐related rifting to basin inversion (Upper Pedraforca thrust sheet, SE Pyrenees)
The field of clumped isotope paleothermometry is over a decade old, but the influence of precipitation rate on the fractionation...
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...
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...
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...