Zobrazeno 1 - 8 of 8 pro vyhledávání: '"J. R. Mendum"'
2
A regional geochemical assessment of some terrane relationships in the British Caledonides
Autor: P. M. Green, J. A. Plant, Philip Stone, J. R. Mendum
Publikováno v: Scottish Journal of Geology. 35:145-156
Synopsis Regional geochemical data have been systematically collected across the British Caledonides and interpreted, using single and multielement image analysis, to provide geochemical constraints on terrane relationships. In the Hebridean Terrane,
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::4d2fd07b324e71c71592d1da7b40f440
https://doi.org/10.1144/sjg35020145
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5
The Tay nappe and associated folding in the Ben Ledi–Loch Lomond area
Autor: J. R. Mendum, D. J. Fettes
Publikováno v: Scottish Journal of Geology. 21:41-56
Synopsis Recent mapping in the Ben Ledi—Loch Lomond area has shown the southern closure of the Tay nappe to consist of three major folds, the Aberfoyle anticline, Ben Ledi antiform and Benvane synform. The D 1 age of these folds is clearly demonstr
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::1867ba7ca4beaa00a570efd84ae908eb
https://doi.org/10.1144/sjg21010041
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6
Aspects of the post-depositional evolution of Dalradian and Highland Border Complex rocks in the Southern Highlands of Scotland
Autor: D. J. Fettes, B. Harte, D. Watts, Tim J. Dempster, J. E. Booth, J. R. Mendum
Publikováno v: Transactions of the Royal Society of Edinburgh: Earth Sciences. 75:151-163
Palaeomagnetic data define a polar wander path for the Dalradian tectonic block of the Scottish Highlands but resolve no relative motion between the Dalradian and Midland Valley blocks from early Ordo vician onwards. The history of structural episode
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::56e2821b359556f4b5e47eb7effa82ca
https://doi.org/10.1017/s0263593300013791
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7
A strain study of the Strathan Conglomerate, North Sutherland
Autor: J. R. Mendum
Publikováno v: Scottish Journal of Geology. 12:135-146
Synopsis The Strathan Conglomerate lies in the Lower Moinian of Sutherland and has been strongly deformed by two events, f 1 and f 2 . Minimum finite strain values X:Y:Z, calculated from deformed pebbles, range from 51:44.5:1 to 32:25:1 respectively.
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::8c40a7c5892075e6ecd334346d7bdfc0
https://doi.org/10.1144/sjg12020135
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