A contribution of airborne magnetic, gamma ray spectrometric data in understanding the structure of the Central Jebilet Hercynian massif and implications for mining

Comme la structure de nos échantillons nous est suffisamment connue (ce sont des graphites synthétiques qui cristallisent dans le système hexagonal), nous ne nous

In recent years more attention has been paid to the models called Local Thermal Non-Equilibrium (LTNE), its use has increased in theoretical and numerical research for convection

Developing local socio- economic scenarios through a participatory process can con- tribute, at a later stage, to modelling exercises based on the evolution of nutrient emissions

The poor correlation between pseudogravity fields for induced magnetization and observed gravity fields strongly suggests that the causative structure has a

Stratigraphic studies have shown that the Jebilet massif was an area of marine sedimentation from Late Devonian to Early Carboniferous, linked to the opening of an

were regressed in Figure 5 to give a least-square line describing the general trend between the two lead-isotope ratios. As many authors interpret the scatter of lead-isotope

In contrast, the presence of a magnetic field perpendicular to the shell collision axis (mhd1r) flattens the shock expansion law to about 0.4.. A test simulation similar to mhd1t,

The final parameters are listed in Table II and the observed and calculated profile is found in figure 1. The