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 GrowthDennis Quandt, Christoph Hauzenberger, Peter Micheuz et al.|Geochemistry Geophysics Geosystems|2019Cited by 16
Geochemistry and Microtextures of Vein Calcites Pervading the Izu‐Bonin Forearc and Rear Arc Crust: New Insights From IODP Expeditions 352 and 351Dennis Quandt, Christoph Hauzenberger, Peter Micheuz et al.|Geochemistry Geophysics Geosystems|2020Cited by 11
Postmagmatic Tectonic Evolution of the Outer Izu‐Bonin Forearc Revealed by Sediment Basin Structure and Vein Microstructure Analysis: Implications for a 15 Ma Hiatus Between Pacific Plate Subduction Initiation and Forearc ExtensionWalter Kurz, Dennis Quandt, Peter Micheuz et al.|Geochemistry Geophysics Geosystems|2019Cited by 10
Microtextures and fluid inclusions from vein minerals hosted in the Pillow Lavas of the Troodos supra-subduction zoneDennis Quandt, Kurt Krenn, Peter Micheuz et al.|Lithosphere|2018Cited by 8
δ¹⁸O, δ¹³C, Δ₄₇ (clumped) and ⁸⁷Sr/⁸⁶Sr isotopic compositions, and trace element concentrations of calcite veins pervading the Troodos pillow lavasDennis Quandt, Christoph Hauzenberger, Peter Micheuz et al.|Figshare|2019Cited by 1