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Pentire Succession

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Journal Article
Published: 01 March 1972
Journal of the Geological Society (1972) 128 (2): 151–172.
...GARRY ALLAN GAUSS; MICHAEL ROBERT HOUSE Abstract Two different successions of Middle and early Upper Devonian rocks are described from the north coast of Cornwall around Padstow. These have been named the Trevone and Pentire successions. The former is seen especially south and west of Camel Estuary...
Journal Article
Published: 01 September 1988
Journal of the Geological Society (1988) 145 (5): 801–807.
... to be widely accepted as an important feature of the Hercynian structure of 0 Pentire Succession m Trevone Succession 2hm , Padstow Confrontation' Overturned base, Padstow Confrontatlon P o l z e a t h S l a t e South-west England (e.g. Shackleton et al. 1982; Coward & Smallwood 1984). Gauss (1973) however...
Journal Article
Published: 01 April 1990
Journal of the Geological Society (1990) 147 (2): 408–410.
... within the confrontation zone. North of Polzeath, Andrews et al. (1988, p. 780, fig. 6) have constructed a south-facing anticline with a long right-way up limb between Tresunger's Point and Pentire Point and a short overturned limb from Pentire to Gravel Caverns. We question the existence...
Journal Article
Published: 01 September 1988
Journal of the Geological Society (1988) 145 (5): 777–787.
.... Drag in the overlying grey slates clearly demonstrates the sense of movement. The stratigraphy southwards to Boobys Bay comprises the well-established Pentire and Trevone successions (Gauss & House 1972) of contrasting Middle to Upper Devonian facies. South-west of Tresungers Point the coast turns more...
Journal Article
Published: 01 September 1988
Journal of the Geological Society (1988) 145 (5): 787–788.
... overfold reported between Pentire and Polzeath; the succession quoted by Gauss & House (1972) was regarded by them as tentative, and most of the contacts between the largely unfossiliferous formations are faulted. The stratigraphic evidence is too tenuous to be the principal support of the overfold...
Journal Article
Published: 01 January 1986
Journal of the Geological Society (1986) 143 (1): 75–82.
... lsaac Nappe-North Nappe -Pentire Tintagel Volcanic Fm. ~ Transi t ion Group ~ Conglomerate l - Pent i re Pi l low Lava Group Trevose Slate X including Woolgarden and Delabole Slates Fig. 2. Successions of Tredorn and Port Isaac Nappes. 78 E . B . S E L W O O D & J . M . T H O M A S Fig. 3. Minor F1...
Series: Geological Society, London, Geology of Series
Published: 01 January 2006
DOI: 10.1144/GOEWP.10
EISBN: 9781862393882
... of alkali basaltic lavas, pillowed in parts, hyaloclastites, and tuffs. Major developments are about the mid-basin high ( Leveridge et al . 2002 ) and the northern margin of the basin (e.g. Pentire Volcanic Formation: Frasnian; Selwood et al . 1998 ). Completing the basinal succession about Landulph...
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