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View article: Experimental hydrogenation of pure and Cr-doped rutile at variable temperature, pressure and oxygen fugacity
Experimental hydrogenation of pure and Cr-doped rutile at variable temperature, pressure and oxygen fugacity Open
Rutile is a nominally anhydrous mineral that can incorporate significant amounts of hydrogen through different trace element related H+-defects. The hydrogen content in rutile has been proposed to be pressure- and redox dependent. To evalu…
View article: Chemical discrimination of rutile from different metamorphic source rocks
Chemical discrimination of rutile from different metamorphic source rocks Open
Rutile belongs to the group of ultra-stable minerals during processes of the sedimentary cycle, along with zircon and tourmaline. While detrital zircon mostly derives from felsic igneous rocks and tourmaline is hardly datable, rutile is ma…
View article: Mechanisms of Aqueous Fluid Infiltration and Redistribution in a Lower‐Crustal Pseudotachylyte‐Bearing Fault
Mechanisms of Aqueous Fluid Infiltration and Redistribution in a Lower‐Crustal Pseudotachylyte‐Bearing Fault Open
Coseismic fracturing in the strong, dry, and metastable plagioclase‐rich lower‐crust is an effective mechanism for creating pathways for fluids to infiltrate the host rock, kick‐start metamorphism, and potentially lead to rheological weake…
View article: Mechanical Impact of Heterogeneously Distributed H<sub>2</sub>O on Quartz Deformation
Mechanical Impact of Heterogeneously Distributed H<sub>2</sub>O on Quartz Deformation Open
In order to identify relations between mechanical behavior, deformation mechanisms, microstructural properties, and H 2 O distribution, Tana‐quartzite samples with added H 2 O ranging from 0 to 0.5 wt.% were deformed by axial shortening at…
View article: Tracing modern-style cold subduction in the Proterozoic &#8211; evidence from H2O and trace elements in detrital rutile
Tracing modern-style cold subduction in the Proterozoic – evidence from H2O and trace elements in detrital rutile Open
To understand the onset and evolution of cold subduction on Earth, detrital sedimentary rocks of Precambrian age, potentially derived from exposed high-P low-T metamorphic rocks can be investigated. This requires the estimation of peak met…
View article: H2O-rich rutile as an indicator for modern-style cold subduction
H2O-rich rutile as an indicator for modern-style cold subduction Open
The trace-element and isotope geochemistry of rutile are robust tools to determine metamorphic temperatures, age, and host-/source lithologies. The use of rutile as single grain indicator for pressure, temperature, time and composition (P–…
View article: Multi-phase quantitative compositional mapping by LA-ICP-MS: Analytical approach and data reduction protocol implemented in XMapTools
Multi-phase quantitative compositional mapping by LA-ICP-MS: Analytical approach and data reduction protocol implemented in XMapTools Open
Mapping of trace element signatures is an expanding tool in geoscience and material sciences, which allows the study of solid materials, and processes that may not be captured by major elements. Developments in laser-ablation inductively-c…
View article: Dataset for publication "Multi-phase quantitative compositional mapping by LA-ICP-MS: analytical approach and data reduction protocol implemented in XMapTools"
Dataset for publication "Multi-phase quantitative compositional mapping by LA-ICP-MS: analytical approach and data reduction protocol implemented in XMapTools" Open
Datasets for the publication "Multi-phase quantitative compositional mapping by LA-ICP-MS: analytical approach and data reduction in XMapTools"
View article: Dataset for publication "Multi-phase quantitative compositional mapping by LA-ICP-MS: analytical approach and data reduction protocol implemented in XMapTools"
Dataset for publication "Multi-phase quantitative compositional mapping by LA-ICP-MS: analytical approach and data reduction protocol implemented in XMapTools" Open
Datasets for the publication "Multi-phase quantitative compositional mapping by LA-ICP-MS: analytical approach and data reduction in XMapTools"
View article: A framework for quantitative in situ evaluation of coupled substitutions between H<sup>+</sup> and trace elements in natural rutile
A framework for quantitative in situ evaluation of coupled substitutions between H<sup>+</sup> and trace elements in natural rutile Open
The coupling behaviour of H+ and trace elements in rutile has been studied using in situ polarised Fourier transform infrared (FTIR) spectroscopy and laser ablation inductively coupled plasma mass spectrometry (LA–ICP–MS) analysis. H2O con…
View article: Rutile as a tracer of subduction zone conditions
Rutile as a tracer of subduction zone conditions Open
Rutile is a common accessory mineral in subducted oceanic crust and its trace element geochemistry is frequently used to investigate subduction zone processes.To understand the evolution of subduction on Earth, sedimentary equivalents of m…