Linking process, dimension, texture, and geochemistry in dolomite geobodies: A case study from Wadi Mistal (northern Oman)
Understanding the distribution and geometry of reservoir geobodies is crucial for net-to-gross estimates and to model subsurface flow. This article...
Crestal graben fluid evolution during growth of the Puig-reig anticline (South Pyrenean fold and thrust belt)
The Puig-reig anticline, located in the South Pyrenean fold and thrust belt, developed during the Alpine compression, which affected the...
The magnesium isotope (δ26Mg) signature of dolomites
Dolomite precipitation models and kinetics are debated and complicated due to the complex and temporally fluctuating fluid chemistry and different...
From hydroplastic to brittle deformation: controls on fluid flow in fold and thrust belts. Insights from the Lower Pedraforca thrust sheet (SE Pyrenees)
We present a multidisciplinary study to decipher the controls of deformation on fluid flow regime in fold and thrust belts...
Fluid surface coverage showing the controls of rock mineralogy on the wetting state
The wetting state is an important control on flow in subsurface multi‐fluid phase systems, for example, carbon storage and oil...
Eustatic variations during the Paleocene‐Eocene greenhouse world
We reconstruct eustatic variations during the latest Paleocene and earliest Eocene (∼58–52 Ma). Dinoflagellate cysts, grain size fractions, and organic...
Phosphogenesis and organic-carbon preservation in the Miocene Monterey Formation at Naples Beach, California—The Monterey hypothesis revisited
The middle part of the Miocene Monterey Formation at Naples Beach, west of Santa Barbara, California, is predominantly composed of...
Chemostratigraphy in Miocene heterozoan carbonate settings: applications, limitations and perspectives
The temporal variability of geochemical proxies can be used in time intervals characterized by global changes in marine chemistry to...
Impact of dynamic sedimentation on facies heterogeneities in Lower Cretaceous peritidal deposits of central east Oman
This study, based in the Haushi‐Huqf area of central east Oman, aims to characterize the controls on facies distribution and...
Exploring the geological features and processes that control the shape and internal fabrics of late diagenetic dolomite bodies (Lower Khuff equivalent–Central Oman Mountains)
The Lower Permian carbonate rock succession of the Oman Mountains represents a stratigraphical surface analogue for Middle Eastern Lower Khuff...