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Add example and doc for new parameters
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doc/input_description.md

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@@ -276,13 +276,19 @@ Phase changes are activated and will take place among certain of the defined pha
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| Parameters | Types | Description |
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|:------------|:-----:|:--------------|
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|**ny-inject, nelem-serp, arc-extrusion-rate**|2 int, dbl| See below.|
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|**itype-melting, nelem-serp, arc-extrusion-rate**|2 int, dbl| See below.|
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|**width-mzone, chamber-max, ratio-crust-mzone, ratio-mantle-mzone**|4 dbl| See below.|
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|**lambda-freeze, lambda-freeze-tdep**|2 dbl| See below.|
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|**weaken-ratio-plastic, weaken-ratio-viscous**|2 dbl| See below.|
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* **ny-inject**: not used.
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* **itype-melting**: 0 for no melting. 1 for arc-type melting.
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* **nelem-serp**: the thickness (# elements) of serpentinization zone above subducted oceanic crust.
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* **arc-extrusion-rate**: the rate of arc magma extrusion
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* **arc-extrusion-rate**: the rate of arc magma extrusion (how fast arc crust is generated)
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* **width-mzone**: width (in meter) of the magma zone at Moho
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* **chamber-max**: max volume ratio of magma
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* **ratio-crust-mzone, ratio-mantle-mzone**: ratios of melt migrating to the crust and mantle
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* **lambda-freeze, lambda-freeze-tdep**: temperature-dependent decaying constant of magma (ie. freezing) M(dt)=M(0)*(1-lambda*dt), where lambda = **lambda-freeze** x exp(-**lambda-freeze-tdep** x (T - **t_top**))
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* **weaken-ratio-plastic, weaken-ratio-viscous**: Magma induced weakening for yield stress (plastic) and viscosity. Saturated at **chamber-max**.
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## REMESHING
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examples/subduction.inp

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@@ -211,8 +211,8 @@ phasedat.inp ; file with distribution of phase on the 2D grid (phasedat)
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;Magma:
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; itype_melting, nelem_serp, arc_extrusion_rate
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0, 2, 4e-13
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; width_mzone, ratio_crust_mzone, ratio_mantle_mzone
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50e3, 4e-7, 4e-7
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; width_mzone, chamber_max, ratio_crust_mzone, ratio_mantle_mzone
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50e3, 0.1, 4e-7, 4e-7
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; lambda_freeze, lambda_freeze_tdep
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1e-12, 2e-3
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; weaken_ratio_plastic, weaken_ratio_viscous

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