Activity

2016

• COEVAL ULTRAMAFIC, CARBONATITIC, AND FELSIC ROCKS ARE ASSOCIATED WITH MAGNETITE DEPOSITS IN THE HUDSON HIGHLANDS OF NEW YORK: A CASE OF MULTIPLE ANATECTIC MELTS
  31 The Grenville-Age Low Ti-Fe Oxide Deposits from New York State: Igneous or Hydrothermal?
  Tuesday, 22 March 2016

  8:00 AM - 12:00 PM

  Meeting Room 3