Geochemistry of Vein Calcites Hosted in the Troodos Pillow Lavas and Their Implications for the Timing and Physicochemical Environment of Fracturing, Fluid Circulation, and Vein Mineral Growth-Reference-Cited by-同舟云学术

Geochemistry of Vein Calcites Hosted in the Troodos Pillow Lavas and Their Implications for the Timing and Physicochemical Environment of Fracturing, Fluid Circulation, and Vein Mineral Growth

Published:2019-12 Issue:12 Volume:20 Page:5913-5938
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Quandt D.¹^ORCID,Micheuz P.¹^ORCID,Kurz W.¹^ORCID,Kluge T.²^ORCID,Boch R.³,Hippler D.³^ORCID,Krenn K.¹^ORCID,Hauzenberger C.A.¹

Affiliation:

1. Institute of Earth Sciences, NAWI Graz GeocenterUniversity of Graz Graz Austria

2. Institute of Environmental PhysicsUniversity of Heidelberg Heidelberg Germany

3. Institute of Applied Geosciences, NAWI Graz GeocenterGraz University of Technology Graz Austria

Funder

Heidelberg Graduate School of Fundamental Physics

Austrian Science Fund

Deutsche Forschungsgemeinschaft

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GC008369

Reference163 articles.

1. Evidence from gabbro of the Troodos ophiolite for lateral magma transport along a slow-spreading mid-ocean ridge

2. REE controls in ultramafic hosted MOR hydrothermal systems: An experimental study at elevated temperature and pressure

3. Spreading evolution of the Troodos ophiolite, Cyprus

4. Subseafloor Processes in Mid-Ocean Ridge Hydrothennal Systems

5. Hydrothermal alteration and fluid fluxes in ophiolites and oceanic crust

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