Items where Author is "de Riese, Tamara"
Number of items: 9.
Article
Jansen, D. , Franke, S. ORCID: https://orcid.org/0000-0001-8462-4379, Bauer, C. C. , Binder, T. , Dahl-Jensen, D. , Eichler, J. , Eisen, O. ORCID: https://orcid.org/0000-0002-6380-962X, Hu, Y. , Kerch, J. , Llorens, M. G. , Miller, H. , Neckel, N. , Paden, J. , de Riese, T. , Sachau, T. , Stoll, N. , Weikusat, I. , Wilhelms, F. , Zhang, Y. and Bons, P. D.
(2024)
Shear margins in upper half of Northeast Greenland Ice Stream were established two millennia ago
,
Nature Communications,
15
(1),
1193-
.
doi:
10.1038/s41467-024-45021-8
, hdl:
10013/epic.d8727543-b730-4306-ad28-eb365acf28a1
Article
Llorens, M. G. , Griera, A. , Bons, P. D. , Weikusat, I. ORCID: https://orcid.org/0000-0002-3023-6036, Prior, D. J. , Gomez-Rivas, E. , de Riese, T. , Jimenez-Munt, I. , García-Castellanos, D. and Lebensohn, R. A.
(2022)
Can changes in deformation regimes be inferred from crystallographic preferred orientations in polar ice?
,
The Cryosphere,
16
(5),
pp. 2009-2024
.
doi:
10.5194/TC-16-2009-2022
, hdl:
10013/epic.06ef7a16-6202-4d94-90a3-c10ff53e8838
Article
Bons, P. D. , de Riese, T. , Franke, S. ORCID: https://orcid.org/0000-0001-8462-4379, Llorens, M. G. , Sachau, T. , Stoll, N. ORCID: https://orcid.org/0000-0002-3219-8395, Weikusat, I. ORCID: https://orcid.org/0000-0002-3023-6036, Westhoff, J. and Zhang, Y.
(2021)
Comment on “Exceptionally high heat flux needed to sustain the Northeast Greenland Ice Stream” by Smith-Johnsen et al. (2020)
,
The Cryosphere,
15
,
pp. 2251-2254
.
doi:
10.5194/tc-15-2251-2021
, hdl:
10013/epic.d042d462-959f-4516-a28d-97f99676c64b
Conference
-Talk
Bons, P. D. , de Riese, T. , Franke, S. ORCID: https://orcid.org/0000-0001-8462-4379, Llorens, M. G. , Sachau, T. , Stoll, N. ORCID: https://orcid.org/0000-0002-3219-8395, Weikusat, I. ORCID: https://orcid.org/0000-0002-3023-6036 and Zhang, Y.
(2021)
Heat flux and the North East Greenland Ice Stream
,
EGU General Assembly 2021,
Online,
19 April 2021 - 30 April 2021
.
doi:
10.5194/egusphere-egu21-13450
, hdl:
10013/epic.6ea8cc5b-94bc-4f26-ae40-4ae7fbba2e74
Conference
-Lecture
de Riese, T. , Bons, P. D. , Gomez-Rivas, E. , Griera, A. , Llorens, M. G. and Weikusat, I.
(2021)
Deformation structures resulting from anisotropy during high-strain deformation of ice 1h with initial CPO
doi:
10.5194/egusphere-egu21-10209
, hdl:
10013/epic.547d455a-fac2-4fe5-ab9d-d0c512673e07
Conference
-Talk
de Riese, T. , Bons, P. D. , Gomez-Rivas, E. , Griera, A. , Llorens, M. G. and Weikusat, I. ORCID: https://orcid.org/0000-0002-3023-6036
(2020)
Influence of initial preferred orientations on strain localisation and fold patterns in non-linear viscous anisotropic materials
,
GeoUtrecht2020,
Utrecht, 100% virtual,
24 August 2020 - 26 August 2020
.
hdl:
10013/epic.d806b75a-e91b-49d6-b357-7a7626dfd613
Conference
-Poster
de Riese, T. , Bons, P. D. , Gomez Rivas, E. , Griera, A. , Llorens, M. G. and Weikusat, I. ORCID: https://orcid.org/0000-0002-3023-6036
(2020)
Influence of initial preferred orientations on strain localisation in non-linear viscous anisotropic materials
,
Tectonics Community Science Workshop,
virtual,
27 July 2020 - 31 July 2020
.
hdl:
10013/epic.803f91be-c18c-412c-94d9-caf1eeeb6b7f
Conference
-Lecture
Bons, P. D. , de Riese, T. , Gomez-Rivas, E. , Griera, A. , Llorens, M. G. and Weikusat, I.
(2020)
Stress and strain rate variations and strain localisation in ice: Another complexity to be considered apart from a simple enhancement factor
doi:
10.5194/egusphere-egu2020-17864
, hdl:
10013/epic.fd910e71-aacf-4b7d-a539-a38991a9ff6f
Article
de Riese, T. , Evans, L. , Gomez-Rivas, E. , Griera, A. , Lebensohn, R. A. , Llorens, M. G. , Ran, H. , Sachau, T. , Weikusat, I. ORCID: https://orcid.org/0000-0002-3023-6036 and Bons, P. D.
(2019)
Shear localisation in anisotropic, non-linear viscous materials that develop a CPO: A numerical study
,
Journal of Structural Geology,
124
,
pp. 81-90
.
doi:
10.1016/j.jsg.2019.03.006
, hdl:
10013/epic.dd338a55-089a-4e41-90d3-1f86ece11c1c
This list was generated on Wed Nov 27 05:15:05 2024 UTC.