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176 pic characterization of marginal basins with constraints to geotectonic setting and provenance. Tectonophysics, 352, 33Ȃ64. LINNEMANN, U., MCNAUGHTON, N.J., ROMER, R.L., GEHMLICH, M., DROST, K., TONK, C. (2004). West African provenance for Saxo-Thuringia (Bohemian Massif): did Armorica ever leave pre-Pangean Gond- wana?—U/Pb-SHRIMP zircon evidence and the Nd isotopic record. Internatio- nal Journal of Earth Sciences, 93, 683Ȃ 705. LINNEMANN, U., GERDES, A., DROST, K., BUSǧ CHMANN, B. (2007). The continuum be- tween Cadomian orogenesis and ope- ning of the Rheic Ocean: constraints from LA-ICP-MS UȂPb zircon dating and analysis of plate-tectonic setting (Sa- xo-Thuringian zone, northeastern Bohe- mian Massif, Germany). In: Linnemann, U., Nance, R.D., Kraft, P., Zulauf, G. (Eds.), The evolution of the Rheic Ocean: From AvalonianȂCadomian Active Margin to AlleghenianȂVariscan collision: Geolo- gical Society of America, Special Paper, 423, 61Ȃ96. LINNEMANN, U., PEREIRA, M.F., JEFFRIES, T., DROST, K., GERDES, A. (2008). Cado- mian Orogeny and the opening of the Rheic Ocean: new insights in the dia- crony of geotectonic processes constra- ined by LAȂICPȂMS U-Pb zircon dating (OssaȂMorena and Saxo-Thuringian Zones, Iberian and Bohemian Massifs). Tectonophysics, 461, 21Ȃ43. LINNEMANN, U., GERDES, A., HOFMANN, M., MARKO, L. (2014). The Cadomian Oro- gen: Neoproterozoic to Early Cambrian crustal growth and orogenic zoning along the periphery of the West African Craton — Constraints from UȂPb zircon ages and Hf isotopes (Schwarzburg Anti- form, Germany). Precambrian Research, 244, 236Ȃ278. LLANAǧFUÑEZ, S. (2001). La estructura de la Unidad de Malpica-Tui (Cordillera Varis- ca en Iberia). Serie Tesis Doctorales, 1, IGME, Madrid, 295 pp. LÓPEZ CARMONA, A. (2015). Blueschist-fa- cies rocks from the Malpica-Tui Com- plex (NW Iberian Massif). Nova Terra, 47, 299 pp. LÓPEZǧGUIJARRO, R., ARMENDARIZ, M., QUEǧ SADA, C., FERNÁNDEZǧSUÁREZ, J., MURǧ PHY, J.B., PIN, C., BELLIDO, F. (2008). Ediacaran-Palaeozoic tectonic evolution of the Ossa Morena and Central Iberian zones (SW Iberia) as revealed by SmȂ Nd isotope systematics. Tectonophysics, 461, 202Ȃ214. LOTZE, F. (1945). Zur gliederung der variszi- den der Iberischen Meseta. Geotektonis- che Forschungen, 6, 78-92. LUGMAIR, G.W., CARLSON, R.W. (1978). The Sm-Nd History of KREEP. Lunar and Pla- netary Science Conference, 9th. Hous- ton, Tex. Proceedings. Vol. 1. New York, Pergamon Press, Inc., 689-704. LUGMAIR, G.W., MARTI, K. (1978). Lunar Ini- tial 143 Nd/ 144 Nd: Differential evolution of the lunar crust and mantle. Earth and Planetary Science Letters, 39, 349-357. MAAS, R., MCCULLOCH, M.T. (1991). The pro- venance of Archean clastic metasedi- ments in the Narryer Geniss Complex, Western Australia: trace element geo- chemistry, Nd isotopes, and U-Pb ages for detrital zircons. Geochimica et Cos-