Potassium-argon and related 40Ar/39Ar dating methods are widely recognized as highly accurate and essential geochronological tools for dating geological, archaeological, and planetary events, though proper sample selection is necessary to mitigate challenges like excess argon.
The vast majority of the provided literature confirms that potassium-argon (K-Ar and 40Ar/39Ar) dating is a cornerstone of modern geochronology, yielding high-precision absolute ages that align well with other dating frameworks such as astrochronology. While one paper (11) discusses analytical complications arising from extraneous argon in specific mineral phases (metamorphosed amphiboles), this represents a known challenge in sample selection rather than a fundamental refutation of the method's overall accuracy when properly applied.