W. Jack Rink Jereon Thompson Michael A. Cosca 2014 <p>Definition: ⁴⁰Ar/³⁹Ar geochronology of structural fabrics: The application of ⁴⁰Ar/³⁹Ar methods to date development of structural fabrics in geologic samples.</p> <br/> <p>Introduction: Structural fabrics develop during rock deformation at variable pressures (P), temperatures (T), fluid compositions (X), and time (t). Structural fabrics are represented in rocks by features such as foliations and shear zones developed at the mm to km scale. In ideal cases, the P-T-X history of a given structural fabric can be constrained using stable isotope, cation exchange, and/or mineral equilibria thermobarometry (Essene 1989). The timing of structural fabric development can be assessed qualitatively using geologic field observations or quantitatively using isotope-based geochronology. High-precision geochronology of the thermal and fluid flow histories associated with structural fabric development can answer fundamental geologic questions including (1) when hydrothermal fluids transported and deposited ore minerals, ...</p> application/pdf 10.1007/978-94-007-6326-5_124-1 en Springer Potassium-argon (argon-argon), structural fabrics chapter