Výsledky vyhledávání - "P. W. G Tanner"

Caledonian and Knoydartian overprinting of a Grenvillian inlier and the enclosing Morar Group rocks: structural evolution of the Precambrian Proto-Moine Nappe, Glenelg, NW Scotland

Autor: P. W. G. Tanner, A. G. Leslie, Kathryn Goodenough, Maarten Krabbendam, J. G. Ramsay, D. Dietrich

Publikováno v: Scottish Journal of Geology. 54:13-35

The Grenville and Caledonian orogens, fundamental to building Laurentia and Baltica, intersect in northern Scotland. The Precambrian Glenelg Inlier, within the Scottish Caledonides, preserves a record of Grenvillian, Knoydartian and Caledonian orogen

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::be04460cb6eab6d2064c45bec09f89b9
https://doi.org/10.1144/sjg2017-006

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Rare earth element and La–Th–Sc analysis of cherts from the Highland Border Complex, Scotland: Geochemical determination of the sedimentary environment in greenschist facies rocks

Autor: P. W. G. Tanner, Alan W. Owen, Howard A. Armstrong

Publikováno v: Scottish Journal of Geology. 49:15-31

Synopsis New geological maps of the Highland Border Complex (HBC) at four classical localities across Scotland – Stonehaven; River North Esk; Loch Ard Forest, Aberfoyle; and North Glen Sannox, Arran – are presented as part of this study. Cherts s

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::a6405526049a474fb346c57d578a16be
https://doi.org/10.1144/sjg2012-464

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Provenance of the Highland Border Complex: constraints on Laurentian margin accretion in the Scottish Caledonides

Autor: Renaud E. Merle, Rob Strachan, Peter A. Cawood, P. W. G. Tanner

Publikováno v: Journal of the Geological Society. 169:575-586

Contrasting tectonic models for the Highland Border Complex in the Scottish Caledonides view it either as part of the rifted Laurentian margin of the Iapetus Ocean or as an oceanic terrane. Detrital zircon data from sandstones of the complex yield ag

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::c1ddf988a1e7c1a20f9b83dfd3bff151
https://doi.org/10.1144/0016-76492011-076

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Discussion of ‘The Highland Boundary Fault and the Highland Border Complex’ by B. J. Bluck, Scottish Journal of Geology , 46 , 113–124

Autor: P. W. G. Tanner

Publikováno v: Scottish Journal of Geology. 47:89-93

P.W. Geoff Tanner writes: In this paper, Bluck has failed to provide a balanced and accurate assessment of the progress that has been made over many years to find a robust, modern geological interpretation of the Highland Border. This is no trivial m

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::86e0a65f6b3e2d4d154df4d9147e6a2b
https://doi.org/10.1144/0036-9276/01-432

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The Highland Border Ophiolite of Scotland: observations from the Highland Workshop field excursion of April 2008

Autor: Rob Strachan, P. W. G. Tanner, W. G. Henderson

Publikováno v: Scottish Journal of Geology. 45:13-18

Synopsis In April 2008, 23 attendees of the Highland Workshop visited critical localities of the Scottish Highland Border Complex between Aberfoyle and the Isle of Bute. Widespread existence of fragmental ophicarbonates was confirmed, with the possib

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::a15a609489ced5e40de6d75ce4c4fa33
https://doi.org/10.1144/0036-9276/01-381

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The role of the Highland Border Ophiolite in the ∼ 470 Ma Grampian Event, Scotland

Autor: P. W. G. Tanner

Publikováno v: Geological Magazine. 144:597-602

Field and petrological studies of the Highland Border Ophiolite demonstrate that it was obducted onto the Neoproterozoic–Ordovician rocks of the Dalradian block, and not emplaced against them by post-orogenic strike-slip movement. It was welded ont

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::051c62af8decef292cd1fc80d536f4e1
https://doi.org/10.1017/s0016756807003342

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Structural setting and petrogenesis of the Ben Vuirich Granite Pluton of the Grampian Highlands: a pre-orogenic, rift-related intrusion

Autor: Martin R. Gillespie, P. W. G. Tanner, A. G. Leslie

Publikováno v: Scottish Journal of Geology. 42:113-136

Synopsis The Ben Vuirich intrusion is a small, elongate body of monzogranite that occurs in the Tummel Steep Belt, Perthshire. It was emplaced into Dalradian rocks (Appin Group) at 590 Ma, prior to the D1 phase of the Grampian Event (Caledonian Oroge

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::642416a658a7d6326fb4fc380e175bbf
https://doi.org/10.1144/sjg42020113

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Discussion on evidence for a major Neoproterozoic orogenic unconformity within the Dalradian Supergroup of NW Ireland

Autor: P. W. G. Tanner, Geoffrey Ian Alsop, D.H.W. Hutton

Publikováno v: Journal of the Geological Society. 162:221-224

Geoff Tanner writes: Firstly, I would like to congratulate the authors for presenting a very carefully documented, and splendidly illustrated, account of the origin of the Stralinchy conglomerates. The aim of this contribution is to focus on one impo

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::bd1d7a23be94dd374d03a427297b463a
https://doi.org/10.1144/0016-764904-105

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