Abstract
Geometric analysis shows that motion of sets of strike-slip faults should cause block rotation. The predictions of the geometric model can be independently tested by palaeomagnetic measurements. The model was tested in N Israel. The results are in agreement with the prediction of the geometric analysis of the structure and demonstrate large block rotations, in different senses, in domains of strike-slip faults. The independent structural and palaeomagnetic data can be interpreted within the framework of a simple geometric model. Northern Israel is considered to be a good model for this efficient mechanism of intraplate deformation, which is expected to occur in similar tectonic settings elsewhere.-from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 6256-6270 |
| Number of pages | 15 |
| Journal | Journal of Geophysical Research |
| Volume | 89 |
| Issue number | B7 |
| DOIs | |
| State | Published - 1984 |
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