Construct · 1 fields · 1 citations

slip partitioning: a standalone construct

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Structural geology

the division of oblique plate convergence into near-normal thrusting on the subduction interface and margin-parallel strike-slip faulting inland.

In structural geology, slip partitioning refers to the division of oblique plate convergence into near-normal thrusting on the subduction interface and margin-parallel strike-slip faulting inland. This meaning comes from Fitch (1972) in Journal of Geophysical Research.[1]

Unit
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Measured by

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Nearby constructs

convergence4 fields · 4 citationsjingle · one word, four constructs division4 fields · 7 citationsjingle · one word, four constructs interface2 fields · 2 citationsjingle · one word, two constructs

References

Fitch, T. J. (1972). Plate convergence, transcurrent faults, and internal deformation adjacent to Southeast Asia and the western Pacific. Journal of Geophysical Research, 77(23), 4432-4460. https://doi.org/10.1029/jb077i023p04432

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