The structural style comprised half-grabens bounded by faults whose dip and downthrow were mostly to the south. |
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We use these values to estimate the maximum downthrow of the Skinos fault as 1.12 km from basic trigonometry. |
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Kinematic indicators for main phase deformation fabrics consistently demonstrate a sinistral sense of displacement with a minor southeasterly component of downthrow. |
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The Great Pemberton Fault is a downthrow and passes Pemberton, Orrell and to the west of Shevington. |
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Downthrow on the east side of this fault places the Simpsons Field Formation in tectonic contact with the Jacquet River Formation and creates a half-graben structure. |
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