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A robust code, called Low-T Thermo, has been developed to combine low-Tthermochronological data arbitrarily to model thermal history. After apatitefission-track age and confined length are decoupled into two completelyindependent data to inverse thermal history and thermal history inversion usingmica Ar-Ar age or bedrock quartz optically stimulated luminescence age aredeveloped, there are eight kinds of low-T thermochronological data used toinverse thermal history including apatite fission-track age, apatitefission-track confined length, zircon fission-track age, apatite (U-Th)/He age,zircon (U-Th)/He age, mica Ar-Ar, bedrock quartz optically stimulatedluminescence age and vitrinite reflectance. A total of 247 kinds of combinationmodes can be used to jointly inverse thermal history in theory (except theeight single methods modelling). These arbitrary combinations are helpful tomodel thermal history with the "incomplete" low-T thermochronological data setregarded to be unuseful for thermal history modelling and reduce experimentalcost. For arbitrary combination of different low-T thermochronological data,each low-T thermochronological method is independent incompletely and theequivalent p-value is used to be the identical evaluation indicator in theinverse process. The usefulness of the code is demonstrated by modellingthermal history of existing low-T thermochronological data in the areas ofDabie Mountain, Ahimanawa Range and Southern Alps.

Low-T Thermo: a new program for arbitrarily combining low-T thermochronological data to model thermal history