Structural characteristics and Re–Os dating of quartz-pyrite veins in the Lewisian Gneiss Complex, NW Scotland: Evidence of an Early Paleoproterozoic hydrothermal regime during terrane amalgamation

Autor: Vernon, R., Holdsworth, R.E., Selby, D., Dempsey, E., Finlay, A.J., Fallick, A.E.

Publikováno v: In Precambrian Research June 2014 246:256-267

Trace element fingerprinting of ceramic building material from Carpow and York Roman fortresses manufactured by the VI Legion

Autor: Finlay, A.J., McComish, J.M., Ottley, C.J., Bates, C.R., Selby, D.

Publikováno v: In Journal of Archaeological Science July 2012 39(7):2385-2391

Silurian to Devonian magmatism, molybdenite mineralization, regional exhumation and brittle strike-slip deformation along the Loch Shin Line, NW Scotland

Autor: Holdsworth, R., Dempsey, E., Selby, D., Darling, James Richard, Feely, M., Costanzo, A., Strachan, Robin A, Waters, P., Finlay, A.J.

Publikováno v: Holdsworth, R, Dempsey, E, Selby, D, Darling, J R, Feely, M, Costanzo, A, Strachan, R A, Waters, P & Finlay, A J 2015, ' Silurian to Devonian magmatism, molybdenite mineralization, regional exhumation and brittle strike-slip deformation along the Loch Shin Line, NW Scotland ', Journal of the Geological Society, vol. 172, no. 6, pp. 748-762 . https://doi.org/10.1144/jgs2015-058

The Loch Shin Line is a geological–geophysical lineament associated with a zone of mantle-derived appinites, granites and strike-slip faulting that runs NW–SE across the Moine Nappe, northern Scotland. U–Pb zircon and Re–Os molybdenite dating

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od______3461::9c971ddf1dda52f989914d832ce3132d
https://researchportal.port.ac.uk/ws/files/2529537/Shin_submitted.pdf

Suitability of Bioapatite as Backfill Material for Nuclear Waste Isolation.

Autor: Finlay, A.J., Drewicz, A.E., Terry, D.O., Grandstaff, D.E., Ash, Richard D.

Publikováno v: MRS Online Proceedings Library; 2012, Vol. 1518 Issue 1, p191-196, 6p

Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.