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- W1993573767 abstract "Documentation of new and existing sites in the Middle Lias shows that the MarlstoneRock Bed has a greater stratigraphic range than previously thought, extending down into the margaritatus Zone (late- subnodosus Subzone). From the relationship of earlier Middle Lias marker bands to the Marlstone Rock Bed it is concluded that uplift occurred during the late- subnodosus Subzone about a WNW-ESE axis, located near Gloucester. The Marlstone Rock Bed rests unconformably upon the planed-off surface of these tilted strata. Other episodes of uplift about this axis occurred in the Aalenian ( concavum Zone) and Bajocian ( garantiana Zone). The active block was bounded to the east by the southward continuation of the Inkberrow-Haselor Hill Fault, beyond which the sediments remained unaffected. Movement of the block was presumably due to reactivation of a fault in the underlying basement." @default.
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- W1993573767 date "1990-01-01" @default.
- W1993573767 modified "2023-09-26" @default.
- W1993573767 title "Upper Pliensbachian stratigraphy in the Severn Basin area: evidencefor anomalous structural controls in the Lower and Middle Jurassic" @default.
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- W1993573767 doi "https://doi.org/10.1016/s0016-7878(08)80249-0" @default.
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