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Deep Time Reconstructions of Internal Earth Structure with the Adjoint Method

Deep Time Reconstructions of Internal Earth Structure with the Adjoint Method
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摘要 The adjoint method is a powerful tool to obtain gradient information in a computational model relative to unknown model parameters,allowing one to solve inverse problems where analytical solutions are not available or the cost to determine prohibitive.
出处 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2019年第S01期3-4,共2页 地质学报(英文版)
基金 funding through the infrastructure program of the German Science Foundation(DFG)for geophysical capacity computing DFG funding through the SPP 1375(SAMPLE)as well as generous computing support through the Leibniz Rechenzentrum(LRZ)of the Bavarian Academy of Sciences.
关键词 ADJOINT method inverse problems paleo MANTLE CONVECTION flow RESTORATIONS dynamic TOPOGRAPHY adjoint method inverse problems paleo mantle convection flow restorations dynamic topography
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