Zobrazeno 1 - 10
of 32
pro vyhledávání: '"Matthias Konrad‐Schmolke"'
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 25, Iss 3, Pp n/a-n/a (2024)
Abstract We study the interplay of the thermal structure within subducted oceanic slabs together with the stability fields of hydrous phases that control slab dehydration and the amount of water transported into the deeper mantle. We implement differ
Externí odkaz:
https://doaj.org/article/0a4b6fb6cec04c2cb2944c9979ec6cce
Publikováno v:
Frontiers in Earth Science, Vol 8 (2020)
Externí odkaz:
https://doaj.org/article/c0bb91610ca948db93fabecf84cd90fb
Autor:
Matthias Konrad-Schmolke, Ralf Halama, Richard Wirth, Aurélien Thomen, Nico Klitscher, Luiz Morales, Anja Schreiber, Franziska D. H. Wilke
Publikováno v:
Nature Communications, Vol 9, Iss 1, Pp 1-9 (2018)
Fluid-mediated mineral dissolution is a key mechanism for mineral reactions in the Earth. Here, the authors show that element transport during mineral dissolution and reprecipitation reactions can be mediated by an amorphous phase, which can contain
Externí odkaz:
https://doaj.org/article/617d2a465c764081bb96821e9691bf65
Publikováno v:
Konrad-schmolke, M, Halama, R, Chew, D, Heuzé, C, De Hoog, J & Ditterova, H 2022, ' Discrimination of thermodynamic and kinetic contributions to the heavy rare earth element patterns in metamorphic garnet ', Journal of Metamorphic Geology . https://doi.org/10.1111/jmg.12703
Variations of rare earth element (REE) concentrations in metamorphic garnet are an important source of information of geodynamic and geochemical processes in the deeper Earth. In order to extract this information, the thermodynamic equilibrium and ki
Metamorphic garnet can be the ultimate source of information about geodynamic and geochemical processes in the Earth’s crust. Compositionally zoned garnet porphyroblasts preserve records of the host rock’s reaction path, its element transport pro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3fb8dd05e41ba9254bb003cf0879504f
https://doi.org/10.5194/egusphere-egu23-11106
https://doi.org/10.5194/egusphere-egu23-11106
Publikováno v:
European Journal of Mineralogy. 32:77-87
Monteneveite, ideally Ca 3 Sb 2 5 + ( Fe 2 3 + Fe 2 + ) O12 , is a new member of the garnet supergroup (IMA 2018-060). The mineral was discovered in a small specimen belonging to the Swedish Museum of Natural History coming from the now abandoned Mon
Autor:
Einar Jon Asbjornsson, Mark Peternell, Erik Sturkell, Matthias Konrad-Schmolke, Hrafnhildur Hannesdóttir, Hlynur Stefansson
Publikováno v:
Sustainability
Volume 13
Issue 8
Sustainability, Vol 13, Iss 4183, p 4183 (2021)
Volume 13
Issue 8
Sustainability, Vol 13, Iss 4183, p 4183 (2021)
Microplastic particles, as a second-phase material in ice, may contribute to the effect such particles have on the melting and rheological behaviour of glaciers, and thus influence the future meltwater contribution to the oceans and rising sea levels
Autor:
Matthias Konrad-Schmolke, Nils Gies
Publikováno v:
Goldschmidt2021 abstracts.
Autor:
Ralf Halama, Matthias Konrad-Schmolke
Absolute dating of rock deformation is often hampered by the observation that the affected minerals are only partly re-equilibrated with respect to their isotopic composition.Generally, three different processes enable mineral grains to adjust isotop
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::62cc698b631ecdbd524a1893ce742980
https://doi.org/10.5194/egusphere-egu2020-7963
https://doi.org/10.5194/egusphere-egu2020-7963
Publikováno v:
Frontiers Research Topics ISBN: 9782889662654
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a7139cf421381f7b215027f16d937b80
https://doi.org/10.3389/978-2-88966-265-4
https://doi.org/10.3389/978-2-88966-265-4