High salinity fluids: The result of retrograde metamorphism in thrust zones
- 1 January 1992
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 56 (1) , 81-95
- https://doi.org/10.1016/0016-7037(92)90118-3
Abstract
No abstract availableKeywords
This publication has 24 references indexed in Scilit:
- P-V-T properties of fluids in the system H2O ± CO2 ± NaCl: New graphical presentations and implications for fluid inclusion studiesPublished by Elsevier ,2003
- Chemistry, source, and behavior of fluids involved in alpine thrusting of the Central PyreneesJournal of Geophysical Research, 1990
- Fluid and enthalpy production during regional metamorphismContributions to Mineralogy and Petrology, 1989
- Synthetic fluid inclusions ‐ VI. Quantitative evaluation of the decrepitation behaviour of fluid inclusions in quartz at one atmosphere confining pressureJournal of Metamorphic Geology, 1989
- Cation site occupancy in chlorites and illites as a function of temperatureClay Minerals, 1988
- Internally-Consistent Thermodynamic Data for Minerals in the System Na2O-K2O-CaO-MgO-FeO-Fe2O3-Al2O3-SiO2-TiO2-H2O-CO2Journal of Petrology, 1988
- Communication. Oxide and doubly charged ion response of a commercial inductively coupled plasma mass spectrometry instrumentJournal of Analytical Atomic Spectrometry, 1987
- Deformation partitioning and porphyroblast rotation in meta‐morphic rocks: a radical reinterpretationJournal of Metamorphic Geology, 1985
- Pressure--Temperature--Time Paths of Regional Metamorphism I. Heat Transfer during the Evolution of Regions of Thickened Continental CrustJournal of Petrology, 1984
- The role of the fluid phase during regional metamorphism and deformationJournal of Metamorphic Geology, 1983