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                             11 gevonden resultaten
nr titel auteur tijdschrift jaar jaarg. afl. pagina('s) type
1 Andalusite and Na- and Li-rich cordierite in the La Costa pluton, Sierras Pampeanas, Argentina: textural and chemical evidence for a magmatic origin Alasino, Pablo H.
2009
99 5 p. 1051-1065
artikel
2 Deformation mechanisms of deeply buried and surface-piercing Late Pre-Cambrian to Early Cambrian Ara Salt from interior Oman Schoenherr, Johannes
2009
99 5 p. 1007-1025
artikel
3 Factors controlling present-day tufa dynamics in the Monasterio de Piedra Natural Park (Iberian Range, Spain): depositional environmental settings, sedimentation rates and hydrochemistry Vázquez-Urbez, M.
2009
99 5 p. 1027-1049
artikel
4 From ductile to brittle deformation: structural development and strain distribution along a crustal-scale shear zone in SW Finland Torvela, Taija
2009
99 5 p. 1133-1152
artikel
5 Geomagnetic field anomalies over the Lombok Island region: an attempt to understand the local tectonic changes Zubaidah, Teti
2009
99 5 p. 1123-1132
artikel
6 Higher Himalayan Shear Zone, Zanskar Indian Himalaya: microstructural studies and extrusion mechanism by a combination of simple shear and channel flow Mukherjee, Soumyajit
2009
99 5 p. 1083-1110
artikel
7 Internal structural geometry of the Paleozoic of Graz Gasser, Deta
2009
99 5 p. 1067-1081
artikel
8 Late Palaeozoic deformation of post-Variscan lower crust: shear zone widening due to strain localization during retrograde shearing Zibra, Ivan
2009
99 5 p. 973-991
artikel
9 Shear-wave velocity structure of the western part of the Mediterranean Sea from Rayleigh-wave analysis Corchete, Victor
2009
99 5 p. 955-972
artikel
10 Transpressional tectonics and nappe stacking along the Southern Variscan Front of Morocco Cerrina Feroni, Andrea
2009
99 5 p. 1111-1122
artikel
11 Zircon Hf isotope perspective on the origin of granitic rocks from eastern Bavaria, SW Bohemian Massif Siebel, Wolfgang
2009
99 5 p. 993-1005
artikel
                             11 gevonden resultaten
 
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