Zobrazeno 1 - 10
of 21
pro vyhledávání: '"Tamara de Riese"'
Autor:
Daniela Jansen, Steven Franke, Catherine C. Bauer, Tobias Binder, Dorthe Dahl-Jensen, Jan Eichler, Olaf Eisen, Yuanbang Hu, Johanna Kerch, Maria-Gema Llorens, Heinrich Miller, Niklas Neckel, John Paden, Tamara de Riese, Till Sachau, Nicolas Stoll, Ilka Weikusat, Frank Wilhelms, Yu Zhang, Paul D. Bons
Publikováno v:
Nature Communications, Vol 15, Iss 1, Pp 1-12 (2024)
Abstract Only a few localised ice streams drain most of the ice from the Greenland Ice Sheet. Thus, understanding ice stream behaviour and its temporal variability is crucially important to predict future sea-level change. The interior trunk of the 7
Externí odkaz:
https://doaj.org/article/b9fee28e06734e99a011c16d4228042e
Publikováno v:
Geofluids, Vol 2020 (2020)
Crustal-scale fluid flow can be regarded as a bimodal transport mechanism. At low hydraulic head gradients, fluid flow through rock porosity is slow and can be described as diffusional. Structures such as hydraulic breccias and hydrothermal veins bot
Externí odkaz:
https://doaj.org/article/0d201e82f5744581a8c0a6a3cc2ed2fc
Autor:
Paul D Bons, Catherine C Bauer, Hervé Bocherens, Tamara de Riese, Dorothée G Drucker, Michael Francken, Lumila Menéndez, Alexandra Uhl, Boudewijn P van Milligen, Christoph Wißing
Publikováno v:
PLoS ONE, Vol 14, Iss 4, p e0201998 (2019)
Hominin evolution is characterized by progressive regional differentiation, as well as migration waves, leading to anatomically modern humans that are assumed to have emerged in Africa and spread over the whole world. Why or whether Africa was the so
Externí odkaz:
https://doaj.org/article/7f3a6fdfcae64411a8fad0c7512d4014
Autor:
Paul D Bons, Dongsheng Cao, Tamara de Riese, Eloi González-Esvertit, Daniel Koehn, Isaac Naaman, Till Sachau, He Tian, Enrique Gomez-Rivas
Publikováno v:
Geological Magazine. 159:1952-1977
Hydrofractures, or hydraulic fractures, are fractures where a significantly elevated fluid pressure played a role in their formation. Natural hydrofractures are abundant in rocks and are often preserved as magmatic dykes or sills, and mineral-filled
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a6c3718d0b1e542ff34f0f56066d08b6
https://doi.org/10.1017/s0016756822001042
https://doi.org/10.1017/s0016756822001042
Autor:
Hao Ran, Paul D. Bons, Genhou Wang, Albert Griera, Tamara de Riese, Enrique Gomez-Rivas, Maria-Gema Llorens, Shuming Ran, Yao Wang, Shubiao Wang
The analysis of folds within pebbles in conglomerates has been used to infer deformation events before deposition of the conglomerate. However, it is not clear whether folds can develop within pebbles during subsequent conglomerate deformation. We us
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2ba7372989222077062e0675f0336199
http://hdl.handle.net/10261/306608
http://hdl.handle.net/10261/306608
Fluid flow through the crust can be described as “bimodal”. At low hydraulic head gradients, fluid flows slowly through the rock porosity, which can be described as diffusional. Hydraulic breccias such as the massive Hidden Valley Breccia in Sout
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aaa4145226cb9d2c35410b96c7ce469a
https://doi.org/10.5194/egusphere-egu22-5013
https://doi.org/10.5194/egusphere-egu22-5013
Autor:
Maria-Gema Llorens, Albert Griera, Paul D. Bons, Ilka Weikusat, David J. Prior, Enrique Gomez-Rivas, Tamara de Riese, Ivone Jimenez-Munt, Daniel García-Castellanos, Ricardo A. Lebensohn
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
EPIC3The Cryosphere, 16(5), pp. 2009-2024, ISSN: 1994-0424
instname
EPIC3The Cryosphere, 16(5), pp. 2009-2024, ISSN: 1994-0424
Creep due to ice flow is generally thought to be the main cause for the formation of crystallographic preferred orientations (CPOs) in polycrystalline anisotropic ice. However, linking the development of CPOs to the ice flow history requires a proper
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c16291e37562984751f51bc5df5426c3
http://hdl.handle.net/10261/270644
http://hdl.handle.net/10261/270644
Autor:
Ilka Weikusat, David J. Prior, Enrique Gomez-Rivas, Ricardo A. Lebensohn, Paul D. Bons, Tamara de Riese, Daniel García Castellanos, Albert Griera, Ivone Jimenez-Munt, Maria-Gema Llorens
Creep due to ice flow is generally thought to be the main cause for the formation of crystallographic preferred orientations (CPOs) in polycrystalline anisotropic ice. However, linking the development of CPOs to the ice flow history requires a proper
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6ad1a781f4ba7e98f16dbc8f853eef6c
https://doi.org/10.5194/tc-2021-224
https://doi.org/10.5194/tc-2021-224
Autor:
Maria-Gema Llorens, Lynn Evans, Melanie Finch, Tamara de Riese, Hao Ran, Sandra Piazolo, Paul D. Bons, Ricardo A. Lebensohn, Enrique Gomez-Rivas, Mark Jessell, Albert Griera
Publikováno v:
Dipòsit Digital de la UB
Universidad de Barcelona
Universidad de Barcelona
The forty-year history of the Journal of Structural Geology has recorded an enormous increase in the description, interpretation and modelling of deformation structures. Amongst factors that control deformation and the resulting structures, mechanica
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4513b794417bc9d3725398de815e1c88
https://doi.org/10.1016/j.jsg.2018.04.019
https://doi.org/10.1016/j.jsg.2018.04.019
Autor:
Paul D. Bons, Steven Franke, Yu Zhang, Till Sachau, Maria-Gema Llorens, Tamara de Riese, Ilka Weikusat, Nicolas Stoll
Publikováno v:
EPIC3EGU General Assembly 2021, Online, 2021-04-19-2021-04-30
Digital.CSIC. Repositorio Institucional del CSIC
instname
Digital.CSIC. Repositorio Institucional del CSIC
instname
vEGU21: Gather Online | 19-30 April 2021
The prominent North East Greenland Ice Stream (NEGIS) is an exceptionally large ice stream in the Greenland Ice sheet. It is over 500 km long, originates almost at the central ice divide, and contributes
The prominent North East Greenland Ice Stream (NEGIS) is an exceptionally large ice stream in the Greenland Ice sheet. It is over 500 km long, originates almost at the central ice divide, and contributes
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6a3dba3b80b0ee15a9dd52a3959f3d8c
https://hdl.handle.net/10013/epic.6ea8cc5b-94bc-4f26-ae40-4ae7fbba2e74
https://hdl.handle.net/10013/epic.6ea8cc5b-94bc-4f26-ae40-4ae7fbba2e74