The large volume press facility at ID06 beamline of the European synchrotron radiation facility as a High Pressure-High Temperature deformation apparatus

2015 ◽  
Vol 86 (8) ◽  
pp. 085112 ◽  
Author(s):  
Jeremy Guignard ◽  
Wilson A. Crichton
Keyword(s):  
High Pressure ◽  
High Temperature ◽  
Synchrotron Radiation ◽  
Large Volume ◽  
European Synchrotron Radiation Facility ◽  
High Temperature Deformation ◽  
Temperature Deformation ◽  
High Pressure High Temperature

scholarly journals Microscale and nanoscale strain mapping techniques applied to creep of rocks

Solid Earth ◽  
2017 ◽  
Vol 8 (4) ◽  
pp. 751-765 ◽  
Author(s):  
Alejandra Quintanilla-Terminel ◽  
Mark E. Zimmerman ◽  
Brian Evans ◽  
David L. Kohlstedt
Keyword(s):  
High Pressure ◽  
High Temperature ◽  
Laboratory Data ◽  
Confining Pressure ◽  
Grain Boundary Sliding ◽  
High Temperature Deformation ◽  
Temperature Deformation ◽  
Computational Techniques ◽  
Strain Partitioning ◽  
Strain Mapping

Abstract. Usually several deformation mechanisms interact to accommodate plastic deformation. Quantifying the contribution of each to the total strain is necessary to bridge the gaps from observations of microstructures, to geomechanical descriptions, to extrapolating from laboratory data to field observations. Here, we describe the experimental and computational techniques involved in microscale strain mapping (MSSM), which allows strain produced during high-pressure, high-temperature deformation experiments to be tracked with high resolution. MSSM relies on the analysis of the relative displacement of initially regularly spaced markers after deformation. We present two lithography techniques used to pattern rock substrates at different scales: photolithography and electron-beam lithography. Further, we discuss the challenges of applying the MSSM technique to samples used in high-temperature and high-pressure experiments. We applied the MSSM technique to a study of strain partitioning during creep of Carrara marble and grain boundary sliding in San Carlos olivine, synthetic forsterite, and Solnhofen limestone at a confining pressure, Pc, of 300 MPa and homologous temperatures, T∕Tm, of 0.3 to 0.6. The MSSM technique works very well up to temperatures of 700 °C. The experimental developments described here show promising results for higher-temperature applications.

scholarly journals Erratum to: High-pressure and high-temperature deformation experiments on polycrystalline wadsleyite using the rotational Drickamer apparatus

2017 ◽  
Vol 44 (3) ◽  
pp. 235-235
Author(s):  
Robert Farla ◽  
George Amulele ◽  
Jennifer Girard ◽  
Nobuyoshi Miyajima ◽  
Shun-ichiro Karato
Keyword(s):  
High Pressure ◽  
High Temperature ◽  
High Temperature Deformation ◽  
Temperature Deformation

High-pressure and high-temperature deformation experiments on polycrystalline wadsleyite using the rotational Drickamer apparatus

2015 ◽  
Vol 42 (7) ◽  
pp. 541-558 ◽  
Author(s):  
Robert Farla ◽  
George Amulele ◽  
Jennifer Girard ◽  
Nobuyoshi Miyajima ◽  
Shun-ichiro Karato
Keyword(s):  
High Pressure ◽  
High Temperature ◽  
High Temperature Deformation ◽  
Temperature Deformation
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