Clumped isotope record of individual limestone fabrics: A potential method to constrain the timing of oil migration
This study applied clumped isotope analyses to investigate how different limestone components (larger skeletal grains and enclosing matrix) and cements...
Disentangling the Impact of Global and Regional Climate Changes During the Middle Eocene in the Hampshire Basin: New Insights From Carbonate Clumped Isotopes and Ostracod Assemblages
We present a novel multiproxy data set (bulk and clumped isotopes on gastropod shells and variations in ostracod assemblages) of...
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...
Influence of climate and dolomite composition on dedolomitization: insights from a multi-proxy study in the central Oman Mountains
Dedolomitization is an important diagenetic process that can yield information on the history of paleo-fluids in a given aquifer or...
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...
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...
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...
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...
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...