0Ar/39Ar ages of lunar impact glasses: Relationships among Ar diffusivity, chemical composition, shape, and size

· by · in

N.E.B. Zellner, J.W. Delano

Geochimica et Cosmochimica Acta
available online 16 April 2015
doi:10.1016/j.gca.2015.04.013

LINK

Related posts (automatically generated):

  1. Constraining the formation and transport of lunar impact glasses using the ages and chemical compositions of Chang’e-5 glass beadsOPEN ACCESS 
  2. U-Pb isotope systematics and impact ages recorded by a chemically diverse population of glasses from an Apollo 14 lunar soilOPEN ACCESS 
  3. Ages of lunar impact breccias: limits for timing of the Imbrium impact
  4. Pb‐Pb ages and initial Pb isotopic composition of lunar meteorites: NWA 773 clan, NWA 4734, and Dhofar 287OPEN ACCESS 
  5. Absence of a long-lived lunar paleomagnetosphereOPEN ACCESS 
  6. Evidence of extensive lunar crust formation in impact melt sheets 4,330 Myr ago
  7. Large sulfur isotope fractionation in lunar volcanic glasses reveals the magmatic differentiation and degassing of the MoonOPEN ACCESS 
  8. The lunar Dhofar 1436 meteorite: 40Ar‐39Ar chronology and volatiles, revealed by stepwise combustion and crushing methodsOPEN ACCESS 
  9. A review of lunar chronology revealing a preponderance of 4.34–4.37 Ga ages
  10. Evidence of chemical heterogeneity within lunar anorthosite parental magmasOPEN ACCESS 
Tags: , , , , ,