The Role of Fluids in Crustal Processes (1990)
Chapter: 5. Oxygen and Hydrogen Isotope Constraints on the Deep Circulation of Surface Waters into Zones of Hydrothermal Metamorphism and Melting
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Previous Chapter:
4. Fluid Dynamics During Progressive Regional Metamorphism
Next Chapter: 6. Hydrothermal Systems Associated with Regional Metamorphism and Crustal Anatexis: Example from the Pyrenees, France
Suggested Citation:
"5. Oxygen and Hydrogen Isotope Constraints on the Deep Circulation of Surface Waters into Zones of Hydrothermal Metamorphism and Melting." National Research Council. 1990. The Role of Fluids in Crustal Processes. Washington, DC: The National Academies Press.
doi: 10.17226/1346.
Suggested Citation:
"5. Oxygen and Hydrogen Isotope Constraints on the Deep Circulation of Surface Waters into Zones of Hydrothermal Metamorphism and Melting." National Research Council. 1990. The Role of Fluids in Crustal Processes. Washington, DC: The National Academies Press.
doi: 10.17226/1346.
Suggested Citation:
"5. Oxygen and Hydrogen Isotope Constraints on the Deep Circulation of Surface Waters into Zones of Hydrothermal Metamorphism and Melting." National Research Council. 1990. The Role of Fluids in Crustal Processes. Washington, DC: The National Academies Press.
doi: 10.17226/1346.
Suggested Citation:
"5. Oxygen and Hydrogen Isotope Constraints on the Deep Circulation of Surface Waters into Zones of Hydrothermal Metamorphism and Melting." National Research Council. 1990. The Role of Fluids in Crustal Processes. Washington, DC: The National Academies Press.
doi: 10.17226/1346.
Suggested Citation:
"5. Oxygen and Hydrogen Isotope Constraints on the Deep Circulation of Surface Waters into Zones of Hydrothermal Metamorphism and Melting." National Research Council. 1990. The Role of Fluids in Crustal Processes. Washington, DC: The National Academies Press.
doi: 10.17226/1346.
Suggested Citation:
"5. Oxygen and Hydrogen Isotope Constraints on the Deep Circulation of Surface Waters into Zones of Hydrothermal Metamorphism and Melting." National Research Council. 1990. The Role of Fluids in Crustal Processes. Washington, DC: The National Academies Press.
doi: 10.17226/1346.
Suggested Citation:
"5. Oxygen and Hydrogen Isotope Constraints on the Deep Circulation of Surface Waters into Zones of Hydrothermal Metamorphism and Melting." National Research Council. 1990. The Role of Fluids in Crustal Processes. Washington, DC: The National Academies Press.
doi: 10.17226/1346.
Suggested Citation:
"5. Oxygen and Hydrogen Isotope Constraints on the Deep Circulation of Surface Waters into Zones of Hydrothermal Metamorphism and Melting." National Research Council. 1990. The Role of Fluids in Crustal Processes. Washington, DC: The National Academies Press.
doi: 10.17226/1346.
Suggested Citation:
"5. Oxygen and Hydrogen Isotope Constraints on the Deep Circulation of Surface Waters into Zones of Hydrothermal Metamorphism and Melting." National Research Council. 1990. The Role of Fluids in Crustal Processes. Washington, DC: The National Academies Press.
doi: 10.17226/1346.
Suggested Citation:
"5. Oxygen and Hydrogen Isotope Constraints on the Deep Circulation of Surface Waters into Zones of Hydrothermal Metamorphism and Melting." National Research Council. 1990. The Role of Fluids in Crustal Processes. Washington, DC: The National Academies Press.
doi: 10.17226/1346.
Suggested Citation:
"5. Oxygen and Hydrogen Isotope Constraints on the Deep Circulation of Surface Waters into Zones of Hydrothermal Metamorphism and Melting." National Research Council. 1990. The Role of Fluids in Crustal Processes. Washington, DC: The National Academies Press.
doi: 10.17226/1346.
Suggested Citation:
"5. Oxygen and Hydrogen Isotope Constraints on the Deep Circulation of Surface Waters into Zones of Hydrothermal Metamorphism and Melting." National Research Council. 1990. The Role of Fluids in Crustal Processes. Washington, DC: The National Academies Press.
doi: 10.17226/1346.
Suggested Citation:
"5. Oxygen and Hydrogen Isotope Constraints on the Deep Circulation of Surface Waters into Zones of Hydrothermal Metamorphism and Melting." National Research Council. 1990. The Role of Fluids in Crustal Processes. Washington, DC: The National Academies Press.
doi: 10.17226/1346.
Suggested Citation:
"5. Oxygen and Hydrogen Isotope Constraints on the Deep Circulation of Surface Waters into Zones of Hydrothermal Metamorphism and Melting." National Research Council. 1990. The Role of Fluids in Crustal Processes. Washington, DC: The National Academies Press.
doi: 10.17226/1346.
Suggested Citation:
"5. Oxygen and Hydrogen Isotope Constraints on the Deep Circulation of Surface Waters into Zones of Hydrothermal Metamorphism and Melting." National Research Council. 1990. The Role of Fluids in Crustal Processes. Washington, DC: The National Academies Press.
doi: 10.17226/1346.
Suggested Citation:
"5. Oxygen and Hydrogen Isotope Constraints on the Deep Circulation of Surface Waters into Zones of Hydrothermal Metamorphism and Melting." National Research Council. 1990. The Role of Fluids in Crustal Processes. Washington, DC: The National Academies Press.
doi: 10.17226/1346.
Suggested Citation:
"5. Oxygen and Hydrogen Isotope Constraints on the Deep Circulation of Surface Waters into Zones of Hydrothermal Metamorphism and Melting." National Research Council. 1990. The Role of Fluids in Crustal Processes. Washington, DC: The National Academies Press.
doi: 10.17226/1346.
Suggested Citation:
"5. Oxygen and Hydrogen Isotope Constraints on the Deep Circulation of Surface Waters into Zones of Hydrothermal Metamorphism and Melting." National Research Council. 1990. The Role of Fluids in Crustal Processes. Washington, DC: The National Academies Press.
doi: 10.17226/1346.
Suggested Citation:
"5. Oxygen and Hydrogen Isotope Constraints on the Deep Circulation of Surface Waters into Zones of Hydrothermal Metamorphism and Melting." National Research Council. 1990. The Role of Fluids in Crustal Processes. Washington, DC: The National Academies Press.
doi: 10.17226/1346.
Suggested Citation:
"5. Oxygen and Hydrogen Isotope Constraints on the Deep Circulation of Surface Waters into Zones of Hydrothermal Metamorphism and Melting." National Research Council. 1990. The Role of Fluids in Crustal Processes. Washington, DC: The National Academies Press.
doi: 10.17226/1346.
Suggested Citation:
"5. Oxygen and Hydrogen Isotope Constraints on the Deep Circulation of Surface Waters into Zones of Hydrothermal Metamorphism and Melting." National Research Council. 1990. The Role of Fluids in Crustal Processes. Washington, DC: The National Academies Press.
doi: 10.17226/1346.
Suggested Citation:
"5. Oxygen and Hydrogen Isotope Constraints on the Deep Circulation of Surface Waters into Zones of Hydrothermal Metamorphism and Melting." National Research Council. 1990. The Role of Fluids in Crustal Processes. Washington, DC: The National Academies Press.
doi: 10.17226/1346.
Suggested Citation:
"5. Oxygen and Hydrogen Isotope Constraints on the Deep Circulation of Surface Waters into Zones of Hydrothermal Metamorphism and Melting." National Research Council. 1990. The Role of Fluids in Crustal Processes. Washington, DC: The National Academies Press.
doi: 10.17226/1346.
Suggested Citation:
"5. Oxygen and Hydrogen Isotope Constraints on the Deep Circulation of Surface Waters into Zones of Hydrothermal Metamorphism and Melting." National Research Council. 1990. The Role of Fluids in Crustal Processes. Washington, DC: The National Academies Press.
doi: 10.17226/1346.
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