Zobrazeno 1 - 10
of 254
pro vyhledávání: '"Jürgen Förster"'
Autor:
Flora P. Gittinger, Martin Lemos, Jan L. Neumann, Jürgen Förster, Daniel Dohmen, Birgit Berke, Anke Olmeo, Gisela Lucas, Stephan M. Jonas
Publikováno v:
BMC Medical Education, Vol 22, Iss 1, Pp 1-10 (2022)
Abstract Background Reliable and objective assessment of psychomotor skills in physiotherapy students’ education is essential for direct feedback and skill improvement. The aim of this study is to determine the interrater reliability in the assessm
Externí odkaz:
https://doaj.org/article/6d18c1316b35407488f3d1c81bd6fb77
Publikováno v:
Geothermal Energy, Vol 8, Iss 1, Pp 1-19 (2020)
Abstract Precise knowledge of the subsurface thermal field plays a key role in the assessment of geothermal targets. Unfortunately, deep underground temperature data is generally scarce and a matter of research. To achieve first estimates for subsurf
Externí odkaz:
https://doaj.org/article/67d3c7ba4f3c468dbcc3601dc74a9e08
Autor:
Ralf Blank, Jörg Echternkamp, Karola Fings, Jürgen Förster, Winfried Heinemann, Tobias Jersak, Armin Nolzen, Christoph Rass
The Second World War affected the lives and shaped the experience of millions of individuals in Germany - soldiers at the front, women, children and the elderly sheltering in cellars, slave labourers toiling in factories, and concentration-camp priso
Publikováno v:
International Journal of Terrestrial Heat Flow and Applications. 5:34-44
This study compares the performance of three analytical methods, hyperspectral imaging in the short-wave infrared range (SWIR), X-ray powder diffraction (XRD), and electron-microprobe analysis (EMPA) for the identification of minerals frequently form
Publikováno v:
Crystals, Vol 10, Iss 8, p 687 (2020)
Tilkerodeite, ideally Pd2HgSe3, is a new platinum-group selenide from the Eskaborner Stollen (Adit Eskaborn) at Tilkerode, Harz Mountains, Germany. Tilkerodeite crystals occur as euhedral inclusions in tiemannite or as extremely fine-grained lamellar
Externí odkaz:
https://doaj.org/article/5fb98f99da4d4508a11a272691db37a5
Autor:
Hans-Jürgen Förster, Ulf B. Andersson
Publikováno v:
Neues Jahrbuch für Mineralogie Abhandlungen
Ca−REE fluorocarbonates occur in various geological environments, including A-type granite systems. Here we investigate the character and paragenesis of fluorocarbonates in the A-type Rödö rapakivi complex, central Sweden, and their importance fo
Publikováno v:
Lithos
We present a comprehensive Li and B isotope study of granites, aplites, and igneous enclaves from the multi-phase Eibenstock granite in the Western Erzgebirge-Vogtland metallogenic province of Germany. The studied samples cover the entire composition
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::04b3f77373fa2a1d9ceb23bf6169ba58
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5011951
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5011951
Publikováno v:
Mineralogical Magazine
Garpenbergite is a new mineral (IMA2020-099) from the Garpenberg Norra mine, Hedemora, Dalarna, Sweden. It occurs with carlfrancisite and minor stibarsen, paradocrasite and filipstadite in a fractured skarn matrix of granular jacobsite, alleghanyite,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::89cd05cf75a4164efbe6acd0bb255e60
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5011750
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5011750
Publikováno v:
Canadian Mineralogist
Nickeltyrrellite, ideally CuNi2Se4, is a new selenide species from the El Dragón mine, Department of Potosí, Bolivia. It most frequently occurs as anhedral to subhedral grains (up to 20 μm in size) in association with cerromojonite, klockmannite,
Autor:
Alicja Wudarska, Hans-Jürgen Förster, Jens Götze, Izabela Moszumańska, Ewa Słaby, Morihisa Hamada, Mudlappa Jayananda, Katarzyna Gros, Hervé Martin, Jean-François Moyen, Łukasz Birski
Publikováno v:
Geological Society, London, Special Publications. 489:293-314
The chemical composition of different rocks as well as volatile-bearing and volatile-free minerals has been used to assess the presence of fluids in the Closepet batholith and to estimate the intensity of the fluid−rock interactions. The data were