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- W2365021999 abstract "Strain partitioning is the phenomenon that the oblique strain in the lower crust and lithospheric mantle is partitioned into near pure tangential and normal strain in the middle upper crust, strain partitioning is expressed as an active thrust parallel strike slip faulting. There′re 4 or 5 parameters influencing strain partitioning: dip of faults, convergence obliquity, coupling condition or stress field, strength of overriding block etc. Being a main model on fault interaction, strain partitioning model is directly supported by seismic data, such as focal mechanism, focal depth and their zonation. On the other hand, a reasonable strain partitioning model will be helpful to evaluate the independence and potentiality of earthquake source, to determine seismic sequence and seismic tendency." @default.
- W2365021999 created "2016-06-24" @default.
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- W2365021999 date "2000-01-01" @default.
- W2365021999 modified "2023-09-25" @default.
- W2365021999 title "Strain partitioning model in the middle-upper crust and its application to seismic research" @default.
- W2365021999 hasPublicationYear "2000" @default.
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