NUCM2 Monte Carlo results - wet crust and dry mantle rheology

Monte Carlo results for NUCM2 simulations (Figure 9b)Rheology = dry mantle and wet crust, diffusion creep Files:Each line of the files (scores, thickness, enrichment factor and crustal radioelement content) corresponds to a model with given crustal parameters (crustal thickness in meters and enrichment factor) and the results obtained for this model. Gaussian scores for the three constraints on elastic thickness are given in the files "score". To compute scores between 0 and 1, these scores have to be divided by the maximum of the corresponding gaussian (given in "Gaussian_maximum.csv": in order for the Noachian, the Southern polar cap and the Northern polar cap) The file "MeltFormation" gives the difference in meters between the depth of the stagnant lid and the depth of melt formation in the Southern hemisphere. Models with present-day formation in the South are those where this difference is lower than 100 km. The percentage of radioelement contained in the Northern and Southern crusts are given in files "RadioelementContents".

NUCM2模拟的蒙特卡洛（Monte Carlo）结果（图9b）：流变学参数设置为干地幔与湿地壳，采用扩散蠕变机制。相关文件说明如下：各文件中的每一行数据分别对应得分、厚度、富集因子与地壳放射元素含量，每一行代表一组给定地壳参数（以米为单位的地壳厚度与富集因子）的模型，以及该模型对应的计算结果。针对弹性厚度三项约束条件的高斯得分存储于名为"score"的文件中。为将得分归一化至0至1区间，需将这些得分除以对应高斯分布的最大值，该最大值存储于"Gaussian_maximum.csv"，对应诺亚纪、南极大极冠与北极大极冠三项约束。文件"MeltFormation"记录了南半球停滞盖层深度与熔体形成深度之间的差值（单位：米）。南半球现今存在熔体形成过程的模型，其上述差值小于100千米。南北地壳所含放射元素的百分比存储于"RadioelementContents"文件中。