Create piezometric_database_ver2.yaml

grain_size_tools/piezometric_database_ver2.yaml

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+# =================================================================== #
+# Save this file in the same directory as GrainSizeTools              #
+# =================================================================== #
+
+---
+database_version: 2024.05.21
+
+metadata:
+  author: Marco A. Lopez-Sanchez
+  contact_email: marcoalopez (at) outlook.com
+  description: Piezometric database from GrainSizeTools script
+  created_at: 2024-05-21
+  license: Open Database License (ODbL) - version 1.0
+  usage_terms: https://opendatacommons.org/licenses/odbl/summary/
+  contributors:
+
+data:
+## quartz piezometers ######################################################################
+  quartz:
+    Stipp_Tullis:
+      year: 2003
+      reference: https://doi.org/10.1029/2003GL018444
+      B: 669.0
+      m: 0.79
+      warn: Please ensure that you have entered the apparent grain size as the root mean square (RMS).
+      linear_intercepts: false
+      correction_factor: false
+      notes: Only applies to recrystallization regimes 2 and 3 (SGR, GBM)
+
+    Stipp_Tullis_BLG:
+      year: 2003
+      reference: https://doi.org/10.1029/2003GL018444
+      B: 1264.1
+      m: 1.64
+      warn: Please ensure that you have entered the apparent grain size as the root mean square (RMS).
+      linear_intercepts: false
+      correction_factor: false
+      notes: Only applies to recrystallization regime 1 (BLG)      
+
+    Holyoke:
+      year: 2010
+      reference: https://doi.org/10.1016/j.tecto.2010.08.001
+      B: 490.3
+      m: 0.79
+      warn: Please ensure that you have entered the apparent grain size as the root mean square (RMS).
+      linear_intercepts: false
+      correction_factor: false
+      notes: Only applies to recrystallization regimes 2 and 3 (SGR, GBM)
+
+    Holyoke_BLG:
+      year: 2010
+      reference: https://doi.org/10.1016/j.tecto.2010.08.001
+      B: 883.9
+      m: 1.85
+      warn: Please ensure that you have entered the apparent grain size as the root mean square (RMS).
+      linear_intercepts: false
+      correction_factor: false
+      notes: Only applies to recrystallization regimes 2 and 3 (SGR, GBM)
+
+    Cross:
+      year: 2017
+      reference: https://doi.org/10.1002/2017GL073836
+      B: 593.0
+      m: 0.71
+      warn: Please ensure that you have entered the apparent grain size as the root mean square (RMS).
+      linear_intercepts: false
+      correction_factor: false
+      notes: None
+
+    Cross_HR:
+      year: 2017
+      reference: https://doi.org/10.1002/2017GL073836
+      B: 450.9
+      m: 0.63
+      warn: Please ensure that you have entered the apparent grain size as the root mean square (RMS).
+      linear_intercepts: false
+      correction_factor: false
+      notes: None
+
+    Shimizu:
+      year: 2008
+      reference: https://doi.org/10.1016/j.jsg.2008.03.004
+      B: 352.0
+      m: 0.8
+      warn: Please ensure that you have entered the apparent grain size as the median in log (base e) scale.
+      linear_intercepts: false
+      correction_factor: false
+      notes: |
+        The Shimizu (2008) piezometer requires entering the grain size as the
+        logarithm of the median apparent grain size calculated using equivalent
+        circular diameters with no stereological correction. It uses a different
+        piezometer model to the Twiss model in which the stress estimation is
+        temperature-dependent.
+  
+    Twiss:
+      year: 1977
+      reference: https://www.doi.org/10.1007/BF01637105
+      B: 550.0
+      m: 0.68
+      warn: Please ensure that you have entered the apparent grain size as the arithmetic mean grain size.
+      linear_intercepts: false
+      correction_factor: 1.5
+      notes: |
+        Twiss (1977) piezometer was calibrated using the linear intercepts (LI) multiplied
+        by 1.5 (correction factor). Equivalent circular diameters (ECD) without stereological
+        correction must be converted to LIs using the empirical equation of De Hoff and
+        Rhines (1968) as follows LI = (1.5 / sqrt(4/pi)) * ECD
+
+## olivine piezometers ######################################################################
+  olivine:
+    VanderWal_wet:
+      year: 1993
+      reference: https://doi.org/10.1029/93GL01382
+      B: 1355.4
+      m: 0.75
+      warn: Please ensure that you have entered the apparent grain size as the arithmetic mean in linear scale.
+      linear_intercepts: true
+      correction_factor: 1.5
+      notes: |
+        The Van der Wal (1993) piezometer was calibrated using the linear intercept (LI) grain size
+        multiplied by 1.5 (correction factor). ECDs without stereological correction will be converted
+        to LIs using the empirical equation of De Hoff and Rhines (1968) LI = (1.5 / sqrt(4/pi)) * ECD
+
+    Jung_Karato:
+      year: 2001
+      reference: https://doi.org/10.1016/S0191-8141(01)00005-0
+      B: 5461.03
+      m: 0.85
+      warn: Please ensure that you have entered the apparent grain size as the arithmetic mean in linear scale.
+      linear_intercepts: true
+      correction_factor: 1.5 
+      notes: |
+        The Jung & Karato (2001) piezometer was calibrated using the linear intercept (LI) grain size
+        multiplied by 1.5 (correction factor). ECDs without stereological correction will be converted
+        to LIs using the empirical equation of De Hoff and Rhines (1968) LI = (1.5 / sqrt(4/pi)) * ECD
+
+## calcite piezometers ######################################################################
+  calcite:
+    Rutter_SGR:
+      year: 1995
+      reference: https://doi.org/10.1029/95JB02500
+      B: 812.83
+      m: 0.88
+      warn: Please ensure that you have entered the apparent grain size as the arithmetic mean in linear scale.
+      linear_intercepts: false
+      correction_factor: false
+      notes: Only applies to subgrain rotation recrystallization
+
+    Rutter_GBM:    
+      year: 1995
+      reference: https://doi.org/10.1029/95JB02500
+      B: 2691.53
+      m: 0.89
+      warn: Please ensure that you have entered the apparent grain size as the arithmetic mean in linear scale.
+      linear_intercepts: false
+      correction_factor: false
+      notes: Only applies to grain boundary migration recrystallization
+
+    Barnhoorn:
+      year: 2003
+      reference: https://doi.org/10.1016/j.jsg.2003.11.024
+      B: 537.03
+      m: 0.82
+      warn: Please ensure that you have entered the apparent grain size as the arithmetic mean in linear scale.
+      linear_intercepts: false
+      correction_factor: false
+      notes: None
+
+    Platt_Bresser:
+      year: 2017
+      reference: https://doi.org/10.1016/j.jsg.2017.10.012
+      B: 538.40
+      m: 0.82
+      warn: Please ensure that you have entered the apparent grain size as the root mean square (RMS) in linear scale.
+      linear_intercepts: false
+      correction_factor: false
+      notes: |
+        Contrary to other calcite piezometers, this one was calibrated using the RMS mean
+        instead of the arithmetic mean.
+  
+    Valcke:
+      year: 2015
+      reference: https://doi.org/10.1144/SP409.4
+      B: 1467.92
+      m: 1.67
+      warn: Please ensure that you have entered the apparent grain size the arithmetic mean in linear scale.
+      linear_intercepts: false
+      correction_factor: false
+      notes: None
+
+## feldspar piezometers #####################################################################
+  feldspar:  # feldspar piezometers
+    Post_Tullis_BLG:
+      year: 1999
+      reference: https://doi.org/10.1016/S0040-1951(98)00260-1
+      B: 433.4
+      m: 1.52
+      warn: Please ensure that you have entered the apparent grain size as the median in linear scale.
+      linear_intercepts: true
+      correction_factor: false
+      notes: |
+        The Post and Tullis (1999) piezometer was calibrated using the median of the
+        equivalent circular diameters (ECD) grain size with no stereological correction.
+
+## End of file ##############################################################################