Examples
- Paleoflow patterns of dolomitizing fluids and paleohydrogeology of the southern Canadian Rocky Mountains: Evidence from dolomite geometry and Fluid-inclusion data indicated that the primary dolomitizing fluids were warm to hot (100 to 200 °C) saline. — “Paleoflow patterns of dolomitizing fluids and”,
- The Watt Mountain shale was also a regional aquiclude that prevented upward circulation of dolomitizing fluids in areas behind the Slave Point shelf edge. Flow of dolomitizing NaCl-CaCl2-MgCl2-H2O brine solutions began in the shallow subsurface. — “The Gas-Bearing Devonian Presqu'ile Dolomite of the Cordova”,
- The Energy Citations Database (ECD) provides access to historical and current research (1948 to the present) from the Department of Energy (DOE) and predecessor agencies. Rocks proximal to the source of dolomitizing fluids exhibit a greater amount of porosity occlusion than more. — “Energy Citations Database (ECD) - - Document #7068157”, osti.gov
- The distribution pattern may be controlled by either the availability of a dolomitizing water or the physical-chemical character of the rock. the greater reactivity to dolomitizing water of fine-grained sediment. — “Cause and Control of Dolomite Distribution by Rock”,
- These data suggest that the dolomitizing fluid is ***ogous to modern diffuse effluent at mid-ocean ridges, and was a mixture of mass balance using the spatial extent of dolomitization in the field and the Ca/Mg of the dolomitizing fluid. — “FORMATION OF REPLACEMENT DOLOMITE BY INFILTRATION OF DIFFUSE”, jscholarship.library.jhu.edu
- The oxygen and strontium isotope compositions reflect equilibration with dolomitizing fluid and provide a chemical fingerprint of the fluid. If the flux of dolomitizing fluid was similar to that of modern diffuse effluent, 0.02 cm3/cm2 · s, the duration of fluid flow and mineral-fluid. — “Formation of replacement dolomite in the Latemar carbonate”,
- Cantabrian Zone (NW Spain): origin of the dolomitizing fluid and relation to the geodynamic setting Crush-leach ***yses reveal that the dolomitizing fluids are highly evaporated seawater which has been. — “HeiDOK - Late burial, hydrothermal dolomitization of the”, archiv.ub.uni-
- temperature of dolomitization, (2) the origin of the dolomitizing fluid, (3) the amount The dolomitizing fluid therefore must have had elevated concentrations. — “American Journal of Science”, appstate.edu
- The dolomitizing fluids rose parallel to major faults to diffuse laterally through the with each stage reflecting several changes in the character of dolomitizing solutions. — “IngentaConnect The geometry and petrogenesis of hydrothermal”,
- Our study addresses questions about the flow geometry, dolomitizing fluid, and flow mechanism involved in one instance of dolomitization. On the basis of these data, we suggest a dolomitizing fluid, ***ogous to diffuse effluent (DE) at mid-ocean. — “DOLOMITIZATION OF A TRIASSIC ATOLL IN A NOVEL SEAFLOOR FLUID”,
- Dolomitizing definition, to convert (limestone) into dolomite. See more. — “Dolomitizing | Define Dolomitizing at ”,
- Isotopic and inclusion data indicate that the most likely dolomitizing fluid was dominated by Neogene seawater (for dolomites, 18OV-PDB = 5.9 to Dolomitizing fluids used faults and fractures as conduits to move. — “AAPG/Datapages, Inc. DOI Citation”,
- Definition of word from the Merriam-Webster Online Dictionary with audio pronunciations, thesaurus, Word of the Day, and word games. — “Dolomitizing - Definition and More from the Free Merriam”, merriam-
- Magnesium-rich fluids moved along faults and fractures through the Trenton and Black River interval, dolomitizing adjacent limestone. Finally, interpreting the source of dolomitizing fluids and migration pathways will help to define the geographic limits of the play. — “Trenton-Black River: Exploration Model and Remaining Problems”, uky.edu
- The distribution of porous and permeable carbonate facies undoubtedly influenced the subsurface fairways traveled by dolomitizing fluids; in many instances these fluids initially entered the Trenton and Black River rocks along vertical fractures. — “Pennsylvania Geological Survey: Trenton Black River”, dcnr.state.pa.us
- carbon isotopes between dolomite crystals and the dolomitizing fluid also The use of fluid inclusions for a direct ***ysis of dolomitizing. — “CHARACTERIZATION OF DOLOMITIZING FLUIDS IN THE CARBONIFEROUS”, fluids.unileoben.ac.at
- However, the nature of the dolomitizing and ore-forming fluids remains unresolved. It appears that a large volume of dolomitized rock (87Sr/86Sr = 0.7095-0.7150, 30-50 ppm Sr, δ18O ~ -8‰ PDB) was affected by similar Late dolomitizing fluids at nearly constant temperatures (~120°C). — “Kevin L. Shelton - Geological Sciences, University of”, rcp.missouri.edu
- The Watt Mountain shale was also a regional aquiclude that prevented upward circulation of dolomitizing fluids in areas behind the Slave Point shelf edge. Flow of dolomitizing NaCl-CaCl2-MgCl2-H2O brine solutions began in the shallow subsurface. — “The gas-bearing Devonian Presqu'ile Dolomite of the Cordova”, cat.inist.fr
- 261-12 From Outcrop to Numerical Modeling of Dolomitizing Fluids, Permian San Andres Fm, Guadalupe Mountains and Algerita Escarpment The source of dolomitizing fluids migrates across the platform top in response to relative sea-level fluctuations and feeds brine plumes within the underlying sediments. — “Paper: From Outcrop to Numerical Modeling of Dolomitizing”, a-c-