Slip rate determined from cosmogenic nuclides on normal-fault facets

Cinq types de représentations des descripteurs audio à partir de « Eros noir 1 » extrait de Toupie Dans Le Ciel de François Bayle (de haut en bas) : corrélation hiérarchique, nuage

Finally, using the experimental observations of Stebbings (1963), we propose an empirical criterion for the stability of an active channel in non-cohesive sediment and compare it

For the densest cases, B4 and T2, statistical wind profiles exhibit the same main characteristics as profiles usually observed in continuous vegetated canopies: a strong vertical shear

It has been established that this defects is related to the change in mineralization form from hexagonal aragonite to orthorhombic vaterite.. SEM picture of pearl surface at

Chapters 1 - 2 discuss some basics: some mathematical foundations as well as real numbers and arithmetic operations.. Chapter 6 surveys some basics from analytic geometry in

(D) and (E) show close-ups of the base of the fault free-plane (location shown in A, B, and C), showing a ribbon of slip surface exposed during the 2004 seismic event (coseismic

Slip rate of trench-parallel normal faulting along the Mejillones Fault (Atacama Fault System): Relationships with the northern Chile subduction and implications for seismic

This apparent discrepancy in slip-rates may have various explanations: 1) the long-term slip-rate may not be uniform over the different time intervals of terrace formation