[PDF] from metododirecto.ptJ Makris, K Nunn, D Roberts… - CM 2010-Abstracts, 2011 - metododirecto.pt ... A crust and basin study of the Nova Scotia margin and its ocean transition based on densely spaced ocean bottom seismic observations ... The next 100 Km consist of a stretched continental crust of 27 to 19 km, including 9 km of sediments. ... Cited by 1 - Related articles - All 2 versions
MS Karplus, W Zhao, SL Klemperer, Z Wu… - Journal of Geophysical …, 2011 - agu.org The International Deep Profiling of Tibet and the Himalaya Phase IV (INDEPTH IV) active source seismic profile in northeast Tibet extends 270 km roughly north-south across the Songpan-Ganzi terrane, the predominantly strike-slip North Kunlun Fault (along the Kunlun suture), the ... All 2 versions
L Crust… - Journal of Sport Psychology in Action, 2011 - eprints.lincoln.ac.uk This article reviews recent evidence concerning the development of mental toughness in young athletes, from first involvement in sport through to early adulthood. The role and importance of genetics, environmental factors, and psychological-skills training in the development of ... Related articles - Cached - All 2 versions
[HTML] from 171.66.125.216EW Sawyer, B Cesare… - Elements, 2011 - 171.66.125.216 Partial melting of the continental crust has long been of interest to petrologists as a small-scale phenomenon. Mineral assemblages in the cores of old, eroded mountain chains that formed where continents collided show that the continental crust was buried deeply enough to ...
SC Kruckenberg, O Vanderhaeghe, EC Ferré… - Tectonics, 2011 - agu.org Migmatite domes are common in metamorphic core complexes. Dome migmatites deform in the partially molten or magmatic state and commonly record complex form surfaces, folds, and fabrics while units mantling the dome display a simpler geometry, typically formed by ... Cited by 2 - Related articles - All 2 versions