To calculate this boundary parameter , mohorovicic discontinuity palaeo - heat flow value during basin evolution process is identified through geotectonic background analogy method based on " peeling " method model , and the basin basement palaeo - heat flow is calculated through inversion from today to antiquity with current tectonic structure as constraint condition for palaeo - crustal architecture analogy 为了求取这个边界参数，以“剥层”法模型为基础，通过大地构造背景类比法确定盆地演化过程中莫霍面古热流值，以现今地壳结构为约束条件类比古地壳结构，从今至古反演求取了盆地基底的古热流。
