Zobrazeno 1 - 10
of 49
pro vyhledávání: '"Sean F. Gallen"'
Autor:
Richard F. Ott, Karl W. Wegmann, Sean F. Gallen, Frank J. Pazzaglia, Mark T. Brandon, Kosuke Ueda, Charalampos Fassoulas
Publikováno v:
AGU Advances, Vol 2, Iss 2, Pp n/a-n/a (2021)
Abstract The hallmark of great earthquakes in the Mediterranean is the 21 July 365 CE earthquake and tsunami that destroyed cities and killed thousands of people throughout the Eastern Mediterranean. This event is intriguing because most Mediterranea
Externí odkaz:
https://doaj.org/article/a5a635222880498d829552a0436e4d4f
Autor:
Maya F. Stokes, Daemin Kim, Sean F. Gallen, Edgar Benavides, Benjamin P. Keck, Julia Wood, Samuel L. Goldberg, Isaac J. Larsen, Jon Michael Mollish, Jeffrey W. Simmons, Thomas J. Near, J. Taylor Perron
Publikováno v:
Science. 380:855-859
The high levels of biodiversity supported by mountains suggest a possible link between geologic processes and biological evolution. Freshwater biodiversity is high not only in tectonically active settings but also in tectonically quiescent montane re
Autor:
Eyal Marder, Sean F. Gallen
Publikováno v:
Geology. 51:424-427
Conceptual and theoretical models for landscape evolution suggest that fluvial topography is sensitive to climate. However, it remains challenging to demonstrate a compelling link between fluvial topography and climate in natural landscapes. One poss
Publikováno v:
Earth Surface Processes and Landforms, 47 (9)
The effect of punctuated mass-wasting events on longer-term erosion rates is not fully understood, and yet it is key to quantifying sediment generation, source-to-sink dynamics, and landscape evolution in active orogens. The measurement of terrestria
Autor:
Sean F. Gallen, Eyal Marder
Additional details of the analyses and supporting figures and tables.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::185b6f796cefab09f06a922950f38d5a
https://doi.org/10.1130/geol.s.22120286.v1
https://doi.org/10.1130/geol.s.22120286.v1
Publikováno v:
Earth Surface Dynamics
Earth Surface Dynamics, 11 (2)
eISSN
Earth Surface Dynamics, 11 (2)
eISSN
Carbonate rocks are highly reactive and can have higher ratios of chemical weathering to total denudation relative to most other rock types. Their chemical reactivity affects the first-order morphology of carbonate-dominated landscapes and their clim
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0a89963d5f7982b7f4e2923d9f94b32f
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5015915
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5015915
Autor:
Zuze Dulanya, Sean F. Gallen, Folarin Kolawole, Jack N. Williams, Luke N. J. Wedmore, Juliet Biggs, Åke Fagereng
Tectonic and paleo-environmental reconstructions of rift evolution typically rely on the interpretation of sedimentary sequences, but this is rarely possible in early-stage rifts where sediment volumes are low. To overcome this challenge, we use geom
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8b0a3baa304428505c43b78263863d50
https://orca.cardiff.ac.uk/id/eprint/152754/1/Dulanya_etal_2022_BasinResearch_postprint.pdf
https://orca.cardiff.ac.uk/id/eprint/152754/1/Dulanya_etal_2022_BasinResearch_postprint.pdf
Publikováno v:
Geochronology
Cosmogenic radionuclides (CRNs) are the standard tool to derive centennial-to-millennial timescale denudation rates; however, it has been demonstrated that chemical weathering in some settings can bias CRNs as a proxy for landscape denudation. Curren
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::255fc272a3c1ed7a102acd6bcad114e7
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5012229_1/component/file_5012230/5012229.pdf
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5012229_1/component/file_5012230/5012229.pdf
Autor:
Karl W. Wegmann, Sean F. Gallen
Publikováno v:
Reference Module in Earth Systems and Environmental Sciences
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::09fa8988c7d28c8570a5938520649a92
https://doi.org/10.1016/b978-0-12-818234-5.00223-6
https://doi.org/10.1016/b978-0-12-818234-5.00223-6