X-ray small angle scattering experiments are used to study the latent tracks produced by Fe and Ar ions (energy range : 1-7 MeV/a.m.u.) in olivine and muscovite mica. In both cases, zones of disordered material are formed which we have characterized by their size and interzone distance. This later distance appears to be the relevant parameter for the chemical etching of the latent track : the track registration process does not seem to imply the existence of an energy threshold mechanism.On étudie, par diffusion des rayons X aux petits angles, la nature de la trace latente des ions Fe et Ar (énergie comprise entre 1 et 7 MeV/nucléon) dans l'olivine et le mica muscovite. Dans les deux cas, il se forme des zones endommagées qu'on caractérise ...
The annealing behaviour of swift heavy-ion tracks in apatite from different origins is studied as a ...
When heavy ions with energies in the range of hundreds of MeV to GeV penetrate a solid, they lose th...
Ion tracks were created in olivine from San Carlos, Arizona (95% Mg2SiO4), apatite (Ca5(PO4)3(F,Cl,O...
X-ray small angle scattering experiments are used to study the latent tracks produced by Fe and Ar i...
The structure of the defects which comprise the latent track of heavy ions in muscovite mica is stud...
We present here, an optical microscope study of the recorded trajectories of fission fragments slowe...
A one-step, three-component aqueous etchant was developed for revealing the tracks of charged partic...
The geometry and composition of deformation-related low-angle boundaries in naturally deformed olivi...
We have studied the morphology and annealing kinetics of ion tracks in Durango apatite using synchro...
In minerals exhibiting cation disorder, the variation in crystal structure environments can be studi...
The aim of this project is to study the atomic surface structure of a natural muscovite crystal than...
A new dating technique uses alpha-recoil tracks (ART), formed by the natural alpha-decay of U, Th an...
Detailed analysis of the morphology of latent tracks created by swift heavy ions from the surface en...
On its way through a solid, an energetic heavy ion deposits an enormous amount of kinetic energy per...
Abstract-Previous studies of the line profiles of the basal reflections of microcrystalline muscovit...
The annealing behaviour of swift heavy-ion tracks in apatite from different origins is studied as a ...
When heavy ions with energies in the range of hundreds of MeV to GeV penetrate a solid, they lose th...
Ion tracks were created in olivine from San Carlos, Arizona (95% Mg2SiO4), apatite (Ca5(PO4)3(F,Cl,O...
X-ray small angle scattering experiments are used to study the latent tracks produced by Fe and Ar i...
The structure of the defects which comprise the latent track of heavy ions in muscovite mica is stud...
We present here, an optical microscope study of the recorded trajectories of fission fragments slowe...
A one-step, three-component aqueous etchant was developed for revealing the tracks of charged partic...
The geometry and composition of deformation-related low-angle boundaries in naturally deformed olivi...
We have studied the morphology and annealing kinetics of ion tracks in Durango apatite using synchro...
In minerals exhibiting cation disorder, the variation in crystal structure environments can be studi...
The aim of this project is to study the atomic surface structure of a natural muscovite crystal than...
A new dating technique uses alpha-recoil tracks (ART), formed by the natural alpha-decay of U, Th an...
Detailed analysis of the morphology of latent tracks created by swift heavy ions from the surface en...
On its way through a solid, an energetic heavy ion deposits an enormous amount of kinetic energy per...
Abstract-Previous studies of the line profiles of the basal reflections of microcrystalline muscovit...
The annealing behaviour of swift heavy-ion tracks in apatite from different origins is studied as a ...
When heavy ions with energies in the range of hundreds of MeV to GeV penetrate a solid, they lose th...
Ion tracks were created in olivine from San Carlos, Arizona (95% Mg2SiO4), apatite (Ca5(PO4)3(F,Cl,O...