The Significance of Heat Transport by Shallow Fluid Flow at an Active Plate Boundary: The Southern Alps, New Zealand.
- Published in:
- Geophysical Research Letters, 2018, v. 45, n. 19, p. 10,323, doi. 10.1029/2018GL078692
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- Publication type:
- Article
Works by Menzies, Catriona D.
Results: 4
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Fluid–rock interactions in the shallow Mariana forearc: carbon cycling and redox conditions.
- Published in:
- Solid Earth, 2019, v. 10, n. 3, p. 907, doi. 10.5194/se-10-907-2019
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- Publication type:
- Article
3
Geochemical and microstructural evidence for interseismic changes in fault zone permeability and strength, Alpine Fault, New Zealand.
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- Geochemistry, Geophysics, Geosystems: G3, 2017, v. 18, n. 1, p. 238, doi. 10.1002/2016GC006588
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- Article
4
Serpentine alteration as source of high dissolved silicon and elevated δ<sup>30</sup>Si values to the marine Si cycle.
- Published in:
- Nature Communications, 2020, v. 11, n. 1, p. N.PAG, doi. 10.1038/s41467-020-18804-y
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- Publication type:
- Article