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      Comment on “The magmatic-hydrothermal transition—evidence from quartz porphyritic textures and endoskarn abundance in Cu–Zn skarns at the Empire Mine, Idaho, USA” by Z. Chang and L.D. Meinert, Chem. Geol. (2004) 210, 149–171

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      Chemical Geology
      Elsevier BV

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          Journal
          Chemical Geology
          Chemical Geology
          Elsevier BV
          00092541
          April 2006
          April 2006
          : 228
          : 4
          : 286-288
          Article
          10.1016/j.chemgeo.2005.11.013
          b2d532c6-1aee-4364-bb59-8da523df22d6
          © 2006

          https://www.elsevier.com/tdm/userlicense/1.0/

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