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Economic Geology; April 1987; v. 82; no. 2; p. 471-481
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Stable isotope studies of the Dae Hwa tungsten-molybdenum mine, Republic of Korea; evidence of progressive meteoric water interaction in a tungsten-bearing hydrothermal system

Kevin L. Shelton, Richard P. Taylor, and Chil-Sup So

Univ. Mo., Dep. Geol., Columbia, MO, United States
Carleton Univ., Canada
Korea Univ., South Korea

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This article has been cited by other articles:


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P.-S. Ross, P.-S. Ross, M. Jebrak, and B. M. Walker
Discharge of Hydrothermal Fluids from a Magma Chamber and Concomitant Formation of a Stratified Breccia Zone at the Questa Porphyry Molybdenum Deposit, New Mexico
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S. A. Wood, S. A. Wood, and I. M. Samson
The Hydrothermal Geochemistry of Tungsten in Granitoid Environments: I. Relative Solubilities of Ferberite and Scheelite as a Function of T, P, pH, and mNaCl
Economic Geology, January 1, 2000; 95(1): 143 - 182.
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