These first results demonstrate that LIBS spectra can be an interesting tool to estimate the ablated volume. When the ablated volume is bigger than 9.10(exp 6) cubic micrometers, this method has less than 10% of uncertainties. Far enough to be directly implemented in the KArLE experiment protocol. Nevertheless, depending on the samples and their mean grain size, the difficulty to have homogeneous spectra will increase with the ablated volume. Several K-Ar dating studies based on this approach will be implemented. After that, the results will be shown and discussed
Sur Mars, la datation par comptage de densité de cratères est actuellement la seule méthode utilisée...
Absolute dating of planetary samples is an essential tool to establish the chronology of geological ...
We have measured 87Rb–87Sr isochron ages for two granites, using the breadboard version of our Chemi...
In planetary exploration, in situ absolute geochronology is an important measurement. Thus far, on M...
In planetary exploration, in situ absolute geochronology is one of the main important measurements t...
The instrument 'Potassium (K) Argon Laser Experiment' (KArLE) is developed and designed for in situ ...
The Potassium-Argon Laser Experiment( KArLE), is composed of two main instruments: a spectrometer as...
Geochronology is a fundamental measurement for planetary samples, providing the ability to establish...
Crater counting is the only method used on Mars to give relative geochronological information but it...
We report new K-Ar isochron data for two approximately 380 Ma basaltic rocks, using an updated versi...
Absolute age determination is necessary to check and calibrate the relative Martian chronology prese...
abstract: Radiometric dating estimates the age of rocks by comparing the concentration of a decaying...
International audienceAbsolute dating is needed to check and calibrate the relative Martian chronolo...
The development of an in-situ geochronology capability for Mars and other planetary surfaces has t...
Techniques enabling in situ elemental and mineralogical analysis on extraterrestrial planets are str...
Sur Mars, la datation par comptage de densité de cratères est actuellement la seule méthode utilisée...
Absolute dating of planetary samples is an essential tool to establish the chronology of geological ...
We have measured 87Rb–87Sr isochron ages for two granites, using the breadboard version of our Chemi...
In planetary exploration, in situ absolute geochronology is an important measurement. Thus far, on M...
In planetary exploration, in situ absolute geochronology is one of the main important measurements t...
The instrument 'Potassium (K) Argon Laser Experiment' (KArLE) is developed and designed for in situ ...
The Potassium-Argon Laser Experiment( KArLE), is composed of two main instruments: a spectrometer as...
Geochronology is a fundamental measurement for planetary samples, providing the ability to establish...
Crater counting is the only method used on Mars to give relative geochronological information but it...
We report new K-Ar isochron data for two approximately 380 Ma basaltic rocks, using an updated versi...
Absolute age determination is necessary to check and calibrate the relative Martian chronology prese...
abstract: Radiometric dating estimates the age of rocks by comparing the concentration of a decaying...
International audienceAbsolute dating is needed to check and calibrate the relative Martian chronolo...
The development of an in-situ geochronology capability for Mars and other planetary surfaces has t...
Techniques enabling in situ elemental and mineralogical analysis on extraterrestrial planets are str...
Sur Mars, la datation par comptage de densité de cratères est actuellement la seule méthode utilisée...
Absolute dating of planetary samples is an essential tool to establish the chronology of geological ...
We have measured 87Rb–87Sr isochron ages for two granites, using the breadboard version of our Chemi...