Downward hydrocarbon migration predicted from numerical modeling of fluid overpressure in the Paleozoic Anticosti Basin, eastern Canada.

It can be divided into 3 system tracts: (1) Transgressive System Tract, which corresponds to flooding of the paleo-topography with formation of a lake system

This approach further highlighted the contrast between two types of weathering regimes present in the central Congo Basin: one in which formed clays remain stable, light Si

Each of the components consumes electricity, and can be grouped into three categories - power delivery, IT equipment, and heat removal (or cooling equipment). Additionally,

the potential generated by the stimulating sites by placing two needle electrodes (as well as a third, reference electrode) into the saline solution and measuring the voltage

Nous avons proposé dans cet article une approche originale de formalisation des arguments via le modèle AIPA, basée sur l’argumentation abstraite de Dung, pour analyser les

The average values of the various parameters of the river SPOM (Ertel et al., 1986; Hedges et al., 1986), wetland soils, “terra firme” soils and the potential biological OM

The raining season (RW season), when increases the soil runo ff and the receding of waters (FW season), when the organic matter is transported from the flooded soils to the

Excitation of plasma waves by unstable photoelectron and thermal electron populations on closed magnetic field lines in the Martian ionosphere.. It is argued that anisotropic