Abstract
The results of recent magnetic measurements in the southern part of the Sea of Galilee, Israel and in the land area south of it, indicate the presence in the subsurface of elongated intrusive bodies of basic composition. These bodies are thought to be associated with faults which formed a rhomb shaped graben during movement along the main Jordan Rift Valley shear system and may mark the southern boundary of that graben. If that is the case, the Sea of Galilee may be considerably shorter in the N-S direction than previously thought. The proposed new dimensions of the graben as outlined in this study are more readily explained by the accepted mechanisms for the formation of rhomb shaped grabens.
Original language | English |
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Pages (from-to) | 153-164 |
Number of pages | 12 |
Journal | Tectonophysics |
Volume | 126 |
Issue number | 2-4 |
DOIs | |
State | Published - 15 Jun 1986 |