Add to ORKGWe report new K-Ar isochron data for two approximately 380 million-years-old basaltic rocks, using an updated version of the Potassium-Argon Laser Experiment (KArLE), which is being developed for future in situ dating of planetary materials. These basalts have K contents comparable with those of lunar KREEP basalts or igneous lithologies found by Mars rovers, whereas previous proof-of-concept studies focused primarily on more K-rich rocks. We aim to measure these analogous samples to show the advancing capability of in situ K-Ar geochronology
Sur Mars, la datation par comptage de densité de cratères est actuellement la seule méthode utilisée...
Absolute age determination is necessary to check and calibrate the relative Martian chronology prese...
Laser-inducedbreakdownspectroscopy is explored for the development of an in-situ K–Ar geochronology ...
We report new K-Ar isochron data for two approximately 380 Ma basaltic rocks, using an updated versi...
Absolute dating of planetary samples is an essential tool to establish the chronology of geological ...
Geochronology is a fundamental measurement for planetary samples, providing the ability to establish...
The instrument 'Potassium (K) Argon Laser Experiment' (KArLE) is developed and designed for in situ ...
The Potassium (K) - Argon (Ar) Laser Experiment (KArLE) will make in situ noble-gas geochronology me...
In planetary exploration, in situ absolute geochronology is one of the main important measurements t...
If extinct and/or extant life is discovered on Mars, knowledge of the chronology of the biosphere wi...
The Potassium-Argon Laser Experiment( KArLE), is composed of two main instruments: a spectrometer as...
The development of an in-situ geochronology capability for Mars and other planetary surfaces has t...
The absolute chronology of Mars is poorly known and as a consequence a key science aim is to perform...
International audienceAbsolute dating is needed to check and calibrate the relative Martian chronolo...
Radiometric age dating of Martian rocks and surfaces at known locations for which crater densities c...
Sur Mars, la datation par comptage de densité de cratères est actuellement la seule méthode utilisée...
Absolute age determination is necessary to check and calibrate the relative Martian chronology prese...
Laser-inducedbreakdownspectroscopy is explored for the development of an in-situ K–Ar geochronology ...
We report new K-Ar isochron data for two approximately 380 Ma basaltic rocks, using an updated versi...
Absolute dating of planetary samples is an essential tool to establish the chronology of geological ...
Geochronology is a fundamental measurement for planetary samples, providing the ability to establish...
The instrument 'Potassium (K) Argon Laser Experiment' (KArLE) is developed and designed for in situ ...
The Potassium (K) - Argon (Ar) Laser Experiment (KArLE) will make in situ noble-gas geochronology me...
In planetary exploration, in situ absolute geochronology is one of the main important measurements t...
If extinct and/or extant life is discovered on Mars, knowledge of the chronology of the biosphere wi...
The Potassium-Argon Laser Experiment( KArLE), is composed of two main instruments: a spectrometer as...
The development of an in-situ geochronology capability for Mars and other planetary surfaces has t...
The absolute chronology of Mars is poorly known and as a consequence a key science aim is to perform...
International audienceAbsolute dating is needed to check and calibrate the relative Martian chronolo...
Radiometric age dating of Martian rocks and surfaces at known locations for which crater densities c...
Sur Mars, la datation par comptage de densité de cratères est actuellement la seule méthode utilisée...
Absolute age determination is necessary to check and calibrate the relative Martian chronology prese...
Laser-inducedbreakdownspectroscopy is explored for the development of an in-situ K–Ar geochronology ...