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   <subfield code="a">The Cenozoic evolution of the Lundy Pull-Apart Basin into the Lundy Rhomb Horst</subfield>
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   <subfield code="a">The NW-SE Cornubian fault zones (FZs) continue to southwest Wales, where they caused dextral offsets during the late Stephanian. A fault bounded area of Devonian-Carboniferous strata, intruded by the Tertiary Lundy Igneous Complex, forms the Lundy Rhomboid. It originated as the Lundy Rhomb Graben, created by 28-40 km of Tertiary sinistral strike-slip faulting along the left-stepping NW-SE Sticklepath-Lustleigh FZ (SLFZ). Tertiary sedimentation in the graben was accompanied by intrusion of the 2.5-4.0 km thick igneous complex into its basement. Sedimentation later spread beyond the graben to form a ‘steer's horns' basin, of which the Stanley Bank and West Lundy basins are remnants. The strata of the rhomb graben and the ‘steer's horns' basin constituted the perhaps 4 km deep Lundy Pull-Apart Basin. Subsequent relatively minor dextral faulting on the left-stepping SLFZ inverted the graben into the Lundy Rhomb Horst; the basement of the graben was uplifted &lt;̸ 1-2 km (net) and exposed by erosion of the Tertiary strata. The pull-apart basin developed at the intersection of reactivated Hercynian NW-SE transform FZs, and E-W subduction zone thrusts. Cenozoic N-S tensional and compressional reactivations of the thrusts were respectively associated with transtensional development of the pull-apart basin, transpressional of the rhomb horst.</subfield>
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