| 11. | Seismic line showing sedimentary layers, footwall and hanging wall of a growth fault : Modified after Bjerkvik, 2012
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| 12. | It was located immediately above the 800 level, about 15 feet into the ore from the hanging wall.
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| 13. | A number of high-angle normal faults accommodating tilting and extension within the hanging wall are easily visible as well.
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| 14. | The vein carries a black gouge on the foot-wall and several feet of altered granodiorite on the hanging wall.
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| 15. | A reverse fault is the opposite of a normal fault the hanging wall moves up relative to the footwall.
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| 16. | The new added layers are thicker within the footwall than within the hanging wall ( fig . 2 ).
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| 17. | Most of the sediment will enter the half-graben down the unfaulted hanging wall side ( " e . g ."
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| 18. | Subduction occurs along a hanging wall, or overriding slab is thrust over an overridden slab, also called the subducting slab.
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| 19. | The clearly defined fault was exposed in the trench and emerged as a band of coarse gravels lining the hanging wall.
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| 20. | Graben are produced from parallel normal faults, where the displacement of the hanging wall is downward, while that of the footwall is upward.
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