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A crust and basin study of the Nova Scotia margin and its ocean transition based on densely spaced ocean bottom seismic observations

[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

Injection of Tibetan crust beneath the south Qaidam Basin: Evidence from INDEPTH IV wide-angle seismic data

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

Developing mental toughness: from research to practice

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

When the Continental Crust Melts

[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 ...

Flow of partially molten crust and the internal dynamics of a migmatite dome, Naxos, Greece

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

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