Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Martin D. Clark"'
Publikováno v:
Geosciences, Vol 11, Iss 2, p 96 (2021)
Better characterization features borne from long-term crustal modification processes is essential for understanding the dynamics of large basin-forming impact structures on Earth. Within the deeply eroded 2.02 Ga Vredefort Impact Structure in South A
Externí odkaz:
https://doaj.org/article/4e280fc3bbe44929942692a960c7c600
The Vredefort granophyre dikes have long been recognized as being derived from the now-eroded Vredefort melt sheet. One dike, in particular, the Daskop granophyre dike, is notable for a high abundance of lithic clasts derived from various stratigraph
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::89c3518520b7da8103763d48e0a2ec57
https://doi.org/10.1130/2021.2550(10)
https://doi.org/10.1130/2021.2550(10)
Autor:
Lisa Bendschneider, Lisa Gibson, Ulrich Riller, Peter C. Lightfoot, Martin D. Clark, Sebastian Reimers, Torben Wüstemann, Paul Leon Göllner
Publikováno v:
Meteoritics & Planetary Science. 54:1228-1245
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cdd3631c4e7a585fc81dc767866c4b23
https://doi.org/10.1111/maps.13268
https://doi.org/10.1111/maps.13268
Publikováno v:
Geosciences
Geosciences, Vol 11, Iss 96, p 96 (2021)
Volume 11
Issue 2
Geosciences, Vol 11, Iss 96, p 96 (2021)
Volume 11
Issue 2
Better characterization features borne from long-term crustal modification processes is essential for understanding the dynamics of large basin-forming impact structures on Earth. Within the deeply eroded 2.02 Ga Vredefort Impact Structure in South A
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a37d2aa67a43083e8a588c527d5955fd
http://hdl.handle.net/11427/35267
http://hdl.handle.net/11427/35267
Publikováno v:
Icarus. 374:114812
The timescale of the modification stage of basin-sized impact structures is not well understood. Owing to ca. 10 km of erosion since its formation, the Vredefort impact structure, South Africa, is an ideal testing ground for deciphering post-impact m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bbfd9aa6ccdaaf8a89af4553edb176e7
https://doi.org/10.1016/j.icarus.2021.114812
https://doi.org/10.1016/j.icarus.2021.114812
Autor:
Martin D. Clark, Ulrich Riller
Publikováno v:
Journal of Structural Geology. 115:266-269
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cc2e9686c5c8ce91b65a505436201ffe
https://doi.org/10.1016/j.jsg.2017.12.003
https://doi.org/10.1016/j.jsg.2017.12.003
Autor:
Ulrich Riller, Martin D. Clark
Publikováno v:
Ore Geology Reviews. 101:199-210
Kinematic restorations of deformed igneous terranes have rarely been attempted due to the general absence of (1) planar primary lithological contacts, (2) tightly constrained deformation kinematics, and (3) geometric constraints on lithologies and st
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7e906233826fc0dbf7ded5825866f54f
https://doi.org/10.1016/j.oregeorev.2018.07.019
https://doi.org/10.1016/j.oregeorev.2018.07.019
Autor:
Martin D. Clark, Ulrich Riller
Publikováno v:
Journal of Structural Geology. 95:113-126
The Sudbury Basin is a non-cylindrical fold basin demarcated by the layered Sudbury Igneous Complex (SIC), the eastern part of which is transected by prominent curved faults. Folding of the SIC and adjacent rock units occurred in the brittle field an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::62c536cf4e45df0b08822e28148f6330
https://doi.org/10.1016/j.jsg.2016.12.010
https://doi.org/10.1016/j.jsg.2016.12.010
Autor:
Martin D. Clark, Daniel Doman, S. Plath, Tasca Santimano, Ulrich Riller, Heidi Daxberger, I. Lenauer
Publikováno v:
Journal of Structural Geology
Heterogeneous deformation is intrinsic in natural deformation, but often underestimated in the analysis and interpretation of mesoscopic brittle shear faults. Based on the analysis of 11,222 faults from two distinct tectonic settings, the Central And
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9373de9c6c4f9f65b4091482920fbf59
http://gfzpublic.gfz-potsdam.de/pubman/item/escidoc:2684892
http://gfzpublic.gfz-potsdam.de/pubman/item/escidoc:2684892