Review of low salinity waterflooding in carbonate rocks: mechanisms, investigation techniques, and future directions
This review analyses the fundamental thermodynamic theory of the crude oil-brine-rock
(COBR) interface and the underlying rock-brine and oil-brine interactions. The available …
(COBR) interface and the underlying rock-brine and oil-brine interactions. The available …
An evaluation of reactive fluid flow and trace element mobility in subducting slabs
Permeabilities in the subducting slab appear to be too low and dihedral angles between
fluid and relevant minerals too high to allow for porous flow, hence fluid channelization is …
fluid and relevant minerals too high to allow for porous flow, hence fluid channelization is …
Variation of crystal dissolution rate based on a dissolution stepwave model
AC Lasaga, A Luttge - Science, 2001 - science.org
A formulation based on defect-generated dissolution stepwaves of the variation of
dissolution rate with the degree of undersaturation is validated by near-atomic-scale …
dissolution rate with the degree of undersaturation is validated by near-atomic-scale …
Chemical geodynamics of continental subduction-zone metamorphism: insights from studies of the Chinese Continental Scientific Drilling (CCSD) core samples
The Dabie–Sulu orogenic belt of east-central China has long been a type location for the
study of geodynamic processes associated with ultrahigh-pressure (UHP) tectonics. Much of …
study of geodynamic processes associated with ultrahigh-pressure (UHP) tectonics. Much of …
Instantaneous rock transformations in the deep crust driven by reactive fluid flow
A Beinlich, T John, JC Vrijmoed, M Tominaga… - Nature …, 2020 - nature.com
Fluid–rock interactions are a fundamental component of geodynamic processes. They link
mass and energy transfer with large-scale tectonic deformation and drive mineral deposit …
mass and energy transfer with large-scale tectonic deformation and drive mineral deposit …
Fluid flow in the deep crust
JJ Ague, RL Rudnick - The crust, 2003 - books.google.com
The heating and burial of rock masses during mountain building drives chemical reactions
that liberate volatile fluid species (Figure 1). These volatiles, including H2O, CO₂, and CH4 …
that liberate volatile fluid species (Figure 1). These volatiles, including H2O, CO₂, and CH4 …
Coupling of anatectic reactions and dissolution of accessory phases and the Sr and Nd isotope systematics of anatectic melts from a metasedimentary source
L Zeng, PD Asimow, JB Saleeby - Geochimica et Cosmochimica Acta, 2005 - Elsevier
Advances in field observations and experimental petrology on anatectic products have
motivated us to investigate the geochemical consequences of accessory mineral dissolution …
motivated us to investigate the geochemical consequences of accessory mineral dissolution …
Density distribution of the India plate beneath the Tibetan plateau: Geophysical and petrological constraints on the kinetics of lower-crustal eclogitization
We combine seismological and Bouguer anomaly data with thermo-kinematic and
petrological modelling to constrain the extent and kinetics of the eclogitization process in the …
petrological modelling to constrain the extent and kinetics of the eclogitization process in the …
Brief thermal pulses during mountain building recorded by Sr diffusion in apatite and multicomponent diffusion in garnet
We use the records of Sr diffusion preserved in apatite and corroborating multicomponent Fe-
Mg–Ca–Mn diffusion preserved in garnet from the classic Barrovian metamorphic zones …
Mg–Ca–Mn diffusion preserved in garnet from the classic Barrovian metamorphic zones …
Prograde temperature–time evolution in the Barrovian type–locality constrained by Sm/Nd garnet ages from Glen Clova, Scotland
The timing of garnet growth during metamorphism associated with the Grampian Orogeny in
the sillimanite zone of the Barrovian type-locality in Glen Clova, Scotland, was determined …
the sillimanite zone of the Barrovian type-locality in Glen Clova, Scotland, was determined …