Zobrazeno 1 - 10
of 55
pro vyhledávání: '"Michael Stipp"'
Publikováno v:
Progress in Earth and Planetary Science, Vol 6, Iss 1, Pp 1-11 (2019)
Abstract Combined knowledge on the magnitude as well as the orientation of paleo-stress is usually not given. Based on drilling investigations and laboratory experiments, we are able to provide both, constraints on paleo-stress magnitude as well as o
Externí odkaz:
https://doaj.org/article/a1743d32f0bf4c4e9e8dcdef59e0ca10
The microstructural evolution of clay-rich sedimentary rocks starts with the settlement and alignment of particles. With the accordance between shape preferred orientation and crystallographic preferred orientation (CPO) in the case of disk-like clay
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::091f0eed7c0ed71b2da007c8c67cbdad
https://doi.org/10.5194/egusphere-egu23-14690
https://doi.org/10.5194/egusphere-egu23-14690
The Tauern Window in the European Alps has a high tectonic complexity. It is a key area to understand a number of important orogenic processes, including nappe stacking, exhumation, indentation as well as escape tectonics. The polyphase Alpine deform
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::53e0aa289217c0cae8fc52f63da36e30
https://doi.org/10.5194/egusphere-egu23-15666
https://doi.org/10.5194/egusphere-egu23-15666
Autor:
Rüdiger Kilian, Michael Stipp
Microstructures in quartz are widely used to draw inferences on conditions and history of deformation. In particular quartz recrystallization microstructures are often assumed to provide an interdependent information on e.g., deformation temperatures
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::09a4752769d638480b337f50ccd3960d
https://doi.org/10.5194/egusphere-egu23-15284
https://doi.org/10.5194/egusphere-egu23-15284
Publikováno v:
Journal of Nuclear Materials. 581:154440
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::28129b9d3bf0780b3f8972840c05ac6e
https://doi.org/10.1016/j.jnucmat.2023.154440
https://doi.org/10.1016/j.jnucmat.2023.154440
At the Hikurangi convergent margin the Pacific plate is subducted westward beneath the Australian plate. This margin has been the location of major earthquakes as well as slow slip events related to the ongoing subduction. Drill site U1518 which was
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9fd3b44e348b166fa22dd25f10a87437
https://doi.org/10.5194/egusphere-egu22-11265
https://doi.org/10.5194/egusphere-egu22-11265
Autor:
Stephan Schnapperelle, Ulf Linnemann, Mandy Hofmann, Andreas Gärtner, Jochen E. Mezger, Michael Stipp
Publikováno v:
Gondwana Research. 81:291-311
Alkaline granitic dikes intruding the metasedimentary mantle and orthogneiss cores of the Aston and Hospitalet domes of the Axial Zone of the Pyrenees are subjects of a laser ablation ICP-MS U-Pb zircon geochronology study. The age spectra recorded b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8a2621e3a022d7b9898a7e4fda2a1d89
https://doi.org/10.1016/j.gr.2019.11.013
https://doi.org/10.1016/j.gr.2019.11.013
The physical properties of claystones, shales, and slates are highly dependent on the alignment of phyllosilicate minerals. With increasing overburdening, the shape and the crystallographic preferred orientation of these minerals are affected by unia
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::968dc8b17c3e3dd214746c2eb336a64e
https://sand.copernicus.org/articles/1/69/2021/
https://sand.copernicus.org/articles/1/69/2021/
Autor:
Michael Stipp, Rüdiger Kilian
Permeability of crystalline rocks depends on parameters such as density and interconnectivity of fractures and pores. While in pristine crystalline rocks porosity is usually considered to be low, low-grade solution phenomena such as the formation of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::735ff72b436818cd76726f14f6e4cadb
https://sand.copernicus.org/articles/1/65/2021/
https://sand.copernicus.org/articles/1/65/2021/
Publikováno v:
International Journal of Earth Sciences. 108:1741-1753
Four samples of garnet-bearing metapsammitic gneisses and one sample of a kinzigitic sillimanite-garnet-cordierite gneiss from the Eckergneiss Complex (Harz Mountains, Germany) were studied in detail for U–Th-total Pb dating with the electron micro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2025b5e7ac1ab8be5ccb6da0dad68dca
https://doi.org/10.1007/s00531-019-01735-5
https://doi.org/10.1007/s00531-019-01735-5