Andere Kunden interessierten sich auch für
![Evolution géotectonique des formations de Rapale]( "Evolution géotectonique des formations de Rapale")
Evolution géotectonique des formations de Rapale26,99 €![Evolução Geotectónica das Formações de Rapale]( "Evolução Geotectónica das Formações de Rapale")
Evolução Geotectónica das Formações de Rapale26,99 €![Self-organized structures in the systems of different nature]( "Self-organized structures in the systems of different nature")
Self-organized structures in the systems of different nature29,99 €![The Coherently Radiating Periodic Structures]( "The Coherently Radiating Periodic Structures")
The Coherently Radiating Periodic Structures44,99 €![Designing of Buildings and Structures]( "Designing of Buildings and Structures")
Designing of Buildings and Structures55,99 €![Materiality, Structures and Ideology]( "Materiality, Structures and Ideology")
Materiality, Structures and Ideology32,99 €![Structural Reliability Analysis of Offshore Structures]( "Structural Reliability Analysis of Offshore Structures")
Structural Reliability Analysis of Offshore Structures51,99 €
The work deals with the "Geotectonic evolution of the Rapale formations". The geological and tectonic evolution of Rapale is the result of the influence of various East Pan African Rift events, Grevilian Orogenies, being outcropped by Rapale Gneiss. Rapale is filled with fragile regime structures such as faults, diaclases, veins, fractures, ductile regime structures such as Boudins, some lineations; high grain metamorphic structures such as migmatites (neosomes and palaeosomes), Grabens-type fault systems. These formations have a spatial orientation of between 179N and 250N (Nairuco, T'tchotcho and Nanahe formations), while in the case of Muhitho they extend up to 360N. These latter formations have undergone East African Rift events, and events that have yet to be identified are responsible for modelling the relief and spatial orientation of the formations.