Hyperspectral mapping of alteration assemblages within a hydrothermal vug at the Haughton impact structure, Canada.

· by · in

Greenberger, R. N., Mustard, J. F., Osinski, G. R., Tornabene, L. L., Pontefract, A. J., Marion, C. L., Flemming, R. L., Wilson, J. H. and Cloutis, E. A.

Meteoritics & Planetary Science. doi: 10.1111/maps.12716

LINK

Related posts (automatically generated):

  1. Hydrothermally enhanced magnetization at the center of the Haughton impact structure?
  2. Evidence for a spatially extensive hydrothermal system at the Ries impact structure, Germany.
  3. Frictional melting processes and the generation of shock veins in terrestrial impact structures: evidence from the Steen River impact structure, Alberta, Canada
  4. Origin of the degassing pipes at the Ries impact structure and implications for impact‐induced alteration on Mars and other planetary bodies
  5. Opaque assemblages in CR2 Graves Nunataks (GRA) 06100 as indicators of shock-driven hydrothermal alteration in the CR chondrite parent body
  6. Shock effects in plagioclase feldspar from the Mistastin Lake impact structure, Canada
  7. In situ U–Pb analysis of shocked zircon from the Charlevoix impact structure, Québec, Canada
  8. Metal microspherules in breccias of the Onaping Formation, Sudbury impact structure, Ontario, Canada
  9. A previously unrecognized high-temperature impactite from the Steen River impact structure, Alberta, Canada
  10. 40Ar/39Ar systematics of melt lithologies and target rocks from the Gow Lake impact structure, Canada
Tags: