Zobrazeno 1 - 8
of 8
pro vyhledávání: '"ddc:552.4"'
Autor:
Eberhard, L., Thielmann, M., Eichheimer, P., Néri, A., Suzuki, A., Ohl, M., Fujita, W., Uesugi, K., Nakamura, M., Golabek, G. J., Frost, D. J., 1 Bayerisches Geoinstitut University of Bayreuth Bayreuth Germany, 4 Department of Earth Science Tohoku University Sendai Japan, 2 Department of Earth Sciences Utrecht University Utrecht The Netherlands, 5 Japan Synchrotron Radiation Research Institute (JASRI/Spring‐8) Hyogo Japan
A new method to determine fluid flux at high pressures and temperatures has been developed and used to study serpentinites at subduction zone conditions. Drill cores of a natural antigorite‐serpentinite with a strong foliation were used in multi‐
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::915995302726b411f5c3e412b717d68f
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/10327
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/10327
Autor:
Walters, Jesse B., Cruz‐Uribe, Alicia M., Song, Won Joon, Gerbi, Christopher, Biela, Kimberly, 2 School of Earth and Climate Sciences University of Maine Orono Maine USA, 3 Department of Anthropology and Geography Colorado State University Fort Collins Colorado USA
Titanite is a potentially powerful U–Pb petrochronometer that may record metamorphism, metasomatism, and deformation. Titanite may also incorporate significant inherited Pb, which may lead to inaccurate and geologically ambiguous U–Pb dates if a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b5aa94d5dfa9ede4f6108432cf8c50da
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/10167
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/10167
Autor:
Gose, Jürgen, Schmädicke, Esther, 1 Geozentrum Nordbayern University Erlangen‐Nürnberg Erlangen Germany
Major and trace elements in omphacite, including hydrogen, were determined in eclogites from two Variscan basement complexes in Germany: Erzgebirge (EG) and Fichtelgebirge (FG). Erzgebirge eclogite is derived from three units, showing different peak
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::876359348e831899657f29d1cba9071d
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/9977
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/9977
Autor:
Menningen, Johanna, Sassoni, Enrico, Sobott, Robert, Siegesmund, Siegfried, Geoscience Centre of the Georg August University Göttingen, Göttingen, Germany, Department of Civil, Chemical, Environmental and Materials Engineering, University of Bologna, Bologna, Italy, Labor für Baudenkmalpflege, Naumburg, Germany
Publikováno v:
Environmental Earth Sciences. 80
In the present study, 5 different consolidants were tested on 5 different marble varieties preliminarily subjected to artificial weathering, to evaluate their consolidating effectiveness and thermal behavior after consolidation, in terms of residual
Autor:
Bucher, Kurt, Stober, Ingrid, Institute of Earth and Environmental Sciences, University of Freiburg, Freiburg, Germany
The composition of meta-gabbro and meta-basalt occurring abundant and widespread in all nappes of the nappe stack exposed in the Zermatt region of the Western Alp shows distinct patterns related to the geodynamic origin of metamorphic basic rocks. Ec
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2497::dfaeb5cfedace885da72f2bdebf7f723
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/10698
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/10698
Autor:
Fonseca, Raúl O. C., Michely, Lina T., Kirchenbaur, Maria, Prytulak, Julie, Ryan, Jeffrey, Hauke, Kerstin, Leitzke, Felipe P., Almeev, Renat R., Marien, Chris S., Gerdes, Axel, Schellhorn, Rico, Institut für Geologie, Mineralogie und Geophysik, Ruhr-Universität Bochum, Bochum, Germany, Agroislab GmbH, Jülich, Germany, Institut für Mineralogie, Leibniz Universität Hannover, Hannover, Germany, Science Labs, Department of Earth Sciences, Durham University, Durham, UK, School of Geosciences, University of South Florida, Tampa, USA, Institut für Geowissenschaften, Universität Bonn, Bonn, Germany, Laboratório de Geologia Isotópica, Universidade Federal do Rio Grande do Sul, Porto Alegre, Brasil, Institut für Geologie und Mineralogie, Universität zu Köln, Köln, Germany, Institut für Geowissenschaften - Frankfurt Isotope and Element Research Center (FIERCE), Goethe Universität Frankfurt, Frankfurt am Main, Germany
Publikováno v:
Contributions to Mineralogy and Petrology 176 (2021), Nr. 1
Contributions to mineralogy and petrology, 2021, Vol.176(1) [Peer Reviewed Journal]
Contributions to mineralogy and petrology, 2021, Vol.176(1) [Peer Reviewed Journal]
The Izu–Bonin–Mariana volcanic arc is situated at a convergent plate margin where subduction initiation triggered the formation of MORB-like forearc basalts as a result of decompression melting and near-trench spreading. International Ocean Disco
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::63023929fcbd5818d927a3e1b7f85b7d
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/10805
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/10805
Autor:
Fassmer, K., Martinet, I., Miladinova, I., Sprung, P., Froitzheim, N., Fonseca, R. O. C., Münker, C., Janák, M., Kullerud, K., Institute of Geology, University of Innsbruck, Innsbruck, Austria, Institute of Geology and Mineralogy, University of Cologne, Cologne, Germany, Institute of Earth Sciences, NAWI Graz Geocenter, University of Graz, Graz, Austria, Abteilung Hotlabor, Paul Scherrer Institut, Villigen, Switzerland, Institute of Geosciences, University of Bonn, Bonn, Germany, Earth Science Institute, Slovak Academy of Sciences, Bratislava, Slovak Republic, Norwegian Mining Museum, Kongsberg, Norway
Geochronology of ultra-high-pressure metamorphic rocks is able to constrain the timing and rates of subduction-zone processes. Lu–Hf garnet dating has the potential to yield information about the timing of the prograde evolution of subducting rocks
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::05781bd28099e9154a055e9dfd6efd02
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/10614
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/10614
Autor:
Schneider, Gerwulf, Büsch, Wilhelm
Publikováno v:
Herausgeberexemplar
Anatektische Schmelzen haben bei der Entstehung granitischer bis dioritischer Magmen in der Erdkruste eine entscheidende Bedeutung. Die große Tiefe und breite Ausdehnung, in der sich sialische Granitisations-Prozesse vollziehen, bedingen aber auch d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ad6468a5ea3c6ab5a412e871568b466c
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/10289
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/10289