Dynamics of sedimentary basins and underlying lithosphere at plate boundaries: The Eastern Mediterranean
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Fig. 5

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Range of stress magnitude for the main faulting regimes in an offshore field: (a) in normal faulting the critical Shmin is highlighted, (b) in strike-slipping the critical SHmax is highlighted and (c) in reverse faulting the SHmax is highlighted. Modified after Zoback (2010).

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