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Differential scanning calorimetry (DSC) measurements were performed using the Thermal Analyst system 2000 (DSC 2910, TA Instument Ltd ,Newcastle, UK).
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All thermal scans were acquired using the thermal functions of two Insight Subluxation Stations® software version 7.05.
Cantilever elastic constants were obtained using the thermal noise method.
Thermogravimetric analysis (TG) was carried out using Thermal Analyst (Setaram Set Sys 16/18) with temperatures ranging from 25 to 800 °C and heating increments of 5 °C per minute in the presence of air.
The slope map is derived from the DEM using the Spatial Analyst tool available in ArcGIS.
The slope map (Fig. 3) was derived from the DEM using the Spatial Analyst tool.
Slope values are then calculated from this map using the spatial analyst tools in ArcGIS 10.2.
Data-mining was performed using the Genedata Analyst 4.1 package (Genedata, Basel, Switzerland).
Analyses of the data were performed using the Raindrop analyst software as previously described [ 20, 21].
Data was assessed using the Analyst® QS software (PE Sciex Instruments, Toronto, Canada).
The weights are obtained by a random process and are hierarchically adjusted using the analyst preferences.
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