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期刊界 All Journals 搜尽天下杂志传播学术成果专业期刊搜索期刊信息化学术搜索

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

Authors:	Michael J. Nicholl Thomas Williams

Affiliation:	^a Geoscience Department, University of Nevada, Las Vegas, Las Vegas, NV 89122-4010, United States ^b College of Science, University of Idaho, Moscow, ID 83844, United States

Abstract:

Keywords:	Discussion Quartz dissolution Igneous Vermicular Embayments
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