All Outputs (3)

Alkaline magmas in zones of continental convergence: The Tezhsar volcano-intrusive ring complex, Armenia (2018)
Journal Article
Sokol, K., Halama, R., Meliksetian, K., Savov, I., Navasardyan, G., & Sudo, M. (2018). Alkaline magmas in zones of continental convergence: The Tezhsar volcano-intrusive ring complex, Armenia. Lithos, 172-191. https://doi.org/10.1016/j.lithos.2018.08.028

Alkaline igneous rocks are relatively rare in settings of tectonic convergence and little is known about their petrogenesis in these settings. This study aims to contribute to a better understanding of the formation of alkaline igneous rocks by an in... Read More about Alkaline magmas in zones of continental convergence: The Tezhsar volcano-intrusive ring complex, Armenia.

Rb-Sr and in situ 40Ar/39Ar dating of exhumation-related shearing and fluid-induced recrystallization in the Sesia zone (Western Alps, Italy) (2018)
Journal Article
Konrad-Schmolke, M., Sudo, M., Halama, R., & Glodny, J. (2018). Rb-Sr and in situ 40Ar/39Ar dating of exhumation-related shearing and fluid-induced recrystallization in the Sesia zone (Western Alps, Italy). Geosphere, 1425-1450. https://doi.org/10.1130/GES01521.1

The Sesia zone in the Italian Western Alps is a piece of continental crust that has been subducted to eclogite-facies conditions and records a complex metamorphic history. The exact timing of events and the significance of geochronological informatio... Read More about Rb-Sr and in situ 40Ar/39Ar dating of exhumation-related shearing and fluid-induced recrystallization in the Sesia zone (Western Alps, Italy).

Mineral dissolution and reprecipitation mediated by an amorphous phase (2018)
Journal Article
Schreiber, A., Wilke, F., Klitscher, N., Morales, L., Wirth, R., Thomen, A., Konrad-Schmolke, M., & Halama, R. (2018). Mineral dissolution and reprecipitation mediated by an amorphous phase. Nature communications, 1637 -1637. https://doi.org/10.1038/s41467-018-03944-z

Fluid-mediated mineral dissolution and reprecipitation processes are the most common mineral reaction mechanism in the solid Earth and are fundamental for the Earth’s internal dynamics. Element exchange during such mineral reactions is commonly thoug... Read More about Mineral dissolution and reprecipitation mediated by an amorphous phase.