18O/16O Evidence for Contrasting Hydrothermal Regimes Involving Magmatic and Meteoric-Hydrothermal Waters at the Valhalla Metamorphic Core Complex, British Columbia-Reference-Cited by-同舟云学术

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18O/16O Evidence for Contrasting Hydrothermal Regimes Involving Magmatic and Meteoric-Hydrothermal Waters at the Valhalla Metamorphic Core Complex, British Columbia

Published:2007-09-01 Issue:6 Volume:102 Page:1063-1078
ISSN:0361-0128
Container-title:Economic Geology
language:en
Short-container-title:Economic Geology

Author:

Holk G. J.,Taylor H. P.

Publisher

Society of Economic Geologists

Subject

Economic Geology,Geochemistry and Petrology,Geology,Geophysics

Cited by 32 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Model constraints on infiltration of surface-derived fluids deep into the brittle crust;Geophysical Journal International;2024-08-06

2. Were oxygen isotopes of hydrothermally altered minerals just elevated by the 18O-enriched water? Theoretical inversion with thermodynamics and kinetics;Mineralogy and Petrology;2024-05-13

3. Theoretical inversion of the fossil hydrothermal systems with oxygen isotopes of constituent minerals partially re-equilibrated with externally infiltrated fluids;Earth and Environmental Science Transactions of the Royal Society of Edinburgh;2021-06

4. The Garies wollastonite deposit, Namaqualand, South Africa: High-Temperature metamorphism of a low-δ18O skarn?;The Canadian Mineralogist;2021-05-01

5. Deep infiltration of surface water during deformation? Evidence from a low- δ18O shear zone at Koegel Fontein, Namaqualand, South Africa;Lithos;2020-08

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