Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Franziska D H, Wilke"'
Autor:
Leila Rezaei, Martin J. Timmerman, Uwe Altenberger, Mohssen Moazzen, Franziska D. H. Wilke, Christina Günter, Masafumi Sudo, Jiří Sláma
Publikováno v:
Swiss Journal of Geosciences, Vol 117, Iss 1, Pp 1-18 (2024)
Abstract The Alborz Mountains in north Iran underwent several tectono-metamorphic events during opening and closure of the Palaeotethys and Neotethys Oceans. These events are recorded by rare and discontinuously exposed metamorphic rocks, such as the
Externí odkaz:
https://doaj.org/article/b8d8f5dcf47d4be4bfb330148fb83ed3
Autor:
Leila Rezaei, Martin J. Timmerman, Mohssen Moazzen, Uwe Altenberger, Jiří Sláma, Masafumi Sudo, Christina Günter, Franziska D. H. Wilke, Anja M. Schleicher
Publikováno v:
Swiss Journal of Geosciences, Vol 116, Iss 1, Pp 1-21 (2023)
Abstract In the Gasht-Masuleh area in the Alborz Mountains, gabbroic magma intruded Palaeozoic metasediments and Mesozoic sediments and crystallised as isotropic and cumulate gabbros. LREE enrichment points to relatively low degrees of mantle melting
Externí odkaz:
https://doaj.org/article/334ca5ad528b4951aa04294e0286243d
Autor:
Alicja Wudarska, Michael Wiedenbeck, Olle Hints, Peep Männik, Aivo Lepland, Michael M. Joachimski, Frédéric Couffignal, Maria Rosa Scicchitano, Franziska D. H. Wilke
Publikováno v:
Estonian Journal of Earth Sciences, Vol 72, Iss 1, Pp 166-0 (2023)
Reliable deep-time environmental and climate reconstructions are needed to understand the drivers of Earthâs system evolution over geological time. Palaeozoic temperature estimates, including reconstructions of the climate change through the Ordovic
Externí odkaz:
https://doaj.org/article/dca4273684e44f368e33a6846a7031dd
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
Autor:
Alicja Wudarska, Michael Wiedenbeck, Ewa Słaby, Małgorzata Lempart‐Drozd, Chris Harris, Michael M. Joachimski, Christophe Lécuyer, Kenneth G. MacLeod, Andreas Pack, Torsten Vennemann, Frédéric Couffignal, Dingsu Feng, Johannes Glodny, Christof Kusebauch, Sathish Mayanna, Alexander Rocholl, Laura Speir, Yadong Sun, Franziska D. H. Wilke
Publikováno v:
Geostandards and Geoanalytical Research, vol. 46, no. 2, pp. 277-306
Geostandards and Geoanalytical Research
Geostandards and Geoanalytical Research
Here we report on the oxygen isotope compositions of four proposed apatite reference materials (chlorapatite MGMH#133648 and fluorapatite specimens MGMH#128441A, MZ-TH, and ES-MM). The samples were initially screened for 18O/16O homogeneity using sec
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8d4870e8b53134d2d5a23160f4f18125
https://doi.org/10.1111/ggr.12416
https://doi.org/10.1111/ggr.12416
Autor:
Franziska D H, Wilke, Georg, Schettler, Andrea, Vieth-Hillebrand, Michael, Kühn, Heike, Rothe
Publikováno v:
Journal of environmental radioactivity.
The production of gas from unconventional resources became an important position in the world energy economics. In 2012, the European Commission's Joint Research Centre estimate 16 trillion cubic meters (Tcm) of technically recoverable shale gas in E
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=pmid________::02a2045f15f7a821fc0ba472706b7e83
https://pubmed.ncbi.nlm.nih.gov/29783196
https://pubmed.ncbi.nlm.nih.gov/29783196
Publikováno v:
Physics and Chemistry of Minerals
The crystal chemistry of tourmaline, XY3Z6(T6O18)(BO3)3V3W, has a strong influence on the structure and physical properties. Since tourmalines occur in a wide range of geological settings and have large temperature and pressure stability fields, the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e51b7e1d8aae6730030b8c33014df793
https://doi.org/10.1007/s00269-017-0914-1
https://doi.org/10.1007/s00269-017-0914-1