Výsledky vyhledávání - "Tanner, P.W.G."

Late Precambrian U-Pb titanite age for peak regional metamorphism and deformation (Knoydartian orogeny) in the western Moine, Scotland

Autor: Tanner, P.W.G., Evans, J.A.

There has been controversy over the number and timing of orogenies in the Precambrian Moine block in the Scottish Caledonides since the earliest radiometric dating in the 1960s. This work challenges a recent hypothesis, that this sector of the Lauren

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Timing of deposition, orogenesis and glaciation within the Dalradian rocks of Scotland: constraints from U-Pb zircon ages

Autor: Dempster, T.J., Rogerson, G., Tanner, P.W.G., Bluck, B.J., Muir, R.J., Redwood, S.D., Ireland, T.R., Paterson, B.A.

The stratigraphical and structural continuity of the Late Proterozoic Dalradian rocks of the Scottish Highlands is re-examined in the light of new U-Pb zircon ages on the tuffs belonging to the Tayvallich Volcanic Formation (601 ñ 4 Ma), and on the

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::af8989c0ca1a187f90787622cd52bfa2
https://eprints.gla.ac.uk/139/1/Dempster_2002.pdf

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Testing for the presence of a terrane boundary within Neoproterozoic (Dalradian) to Cambrian siliceous turbidites at Callander, Perthshire, Scotland

Autor: Tanner, P.W.G., Pringle, M.S.

The Southern Highland Group (Dalradian) and Keltie Water Grit Formation, which includes the Lower Cambrian Leny Limestone, form an inverted, 1.4 km thick, largely arenaceous, sequence at Callander. The grits have the same detrital mineralogy througho

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::48f83a7ec2a340820f8f689ae694a2f3
https://eprints.gla.ac.uk/141/1/Tanner,_P_1999.pdf

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Current controversies in the Caledonides

Autor: Tanner, P.W.G., Bluck, B.J.

No abstract available.

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::550865801a8b2b4e9c5449156686c004
https://eprints.gla.ac.uk/140/1/Tanner,P.W.G__1999.pdf

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Interstratal dewatering origin for polygonal patterns of sand-filled cracks: a case study from late Proterozoic metasediments of Islay, Scotland

Autor: Tanner, P.W.G

Sand-filled cracks from the Lower Fine-grained Quartzite of Dalradian (late Proterozoic) age on the Island of Islay, western Scotland, may be divided into two main types, both of which\ud form orthogonal and non-orthogonal closed patterns on bedding

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::bbbbc5ef7692743ed908ddfb1a45e049
https://eprints.gla.ac.uk/172/1/Tanner_Vol_45.pdf

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