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Stable Isotopic Information on Calcareous Pelitic Rocks in the Tizapa Volcanogenic Massive Sulfide Deposit Area, the United Mexican States |
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| Authors: | Haruhisa Morozumi Hideya Metsugi Yoshiyuki Kita Toru Suzuki |
| Institution: | Japan Mining Engineering Center for International Cooperation, 14F, No. 17 Mori Building, 1–26–5 Toranomon, Minato–ku, Tokyo 105–0001, Japan [e-mail: ];Metal Mining Agency of Japan, Tokiwa Building, 1–24–14 Toranomon, Minato–ku, Tokyo 105–0001, Japan |
| Abstract: | Abstract: Tizapa volcanogenic massive sulfide (VMS) deposit is hosted in greenschist facies metamorphic rocks; footwall is green schist of felsic to mafic metavolcanic rocks and hanging wall is graphite schist of metasedmentary pelitic rock. Pb-Pb dating of ore samples indicates 103. 4Ma to 156. 3Ma for the age of mineralization (JICA/MMAJ, 1991). |
| Keywords: | Tizapa mine volcanogenic massive sulfide (VMS) stable isotope calcareous pelitic rock |