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AAPG Bulletin
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AAPG Bulletin; Year: 2022; Issue: March DOI: 10.1306/07132120084
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Figure 24.
Geological cross section and plan view geologic map showing the evidence for early Cenozoic uplift and fault reactivation in the western part of the Moray Firth rift arm (Guariguata-Rojas and Underhill, 2017). The transient nature of uplift is illustrated by the development and drowning of a dendritic drainage network that incised into easterly prograding deltaic foresets in the Outer Moray Firth. Fm = Formation; Undiff. = undifferentiated.
Figure 24. Geological cross section and plan view geologic map showing the evidence for early Cenozoic uplift and fault reactivation in the western part of the Moray Firth rift arm (Guariguata-Rojas and Underhill, 2017). The transient nature of uplift is illustrated by the development and drowning of a dendritic drainage network that incised into easterly prograding deltaic foresets in the Outer Moray Firth. Fm = Formation; Undiff. = undifferentiated.