Zobrazeno 1 - 10
of 130
pro vyhledávání: '"Kurt Stüwe"'
Publikováno v:
Nature Communications, Vol 13, Iss 1, Pp 1-8 (2022)
Testing feedbacks between climatic and geological processes are challenging. Here, the authors show that geomorphological features of the southern Red Sea margin are best interpreted by a feedback cycle between orographic precipitation, mid-ocean spr
Externí odkaz:
https://doaj.org/article/00e6d93b41114cd4b8eef0db780452fb
Publikováno v:
Liebl, M, Robl, J, Hergarten, S, Egholm, D L & Stüwe, K 2023, ' Modeling large-scale landform evolution with a stream power law for glacial erosion (OpenLEM v37) : benchmarking experiments against a more process-based description of ice flow (iSOSIA v3.4.3) ', Geoscientific Model Development, vol. 16, no. 4, pp. 1315-1343 . https://doi.org/10.5194/gmd-16-1315-2023
Following the tradition of modeling fluvial landscape evolution, a novel approach describing glacial erosion based on an empirical stream power law was proposed. This approach differs substantially from well-established process-based models applied t
Publikováno v:
Austrian Journal of Earth Sciences. 116:17-38
The Bohemian Massif is the relic of a major Paleozoic mountain range that is known to have exhumed and its surface levelled in the Permian, but its Neogene landscape evolution is largely unconstrained. The landscape is characterized by rolling hills
Retrogression and hydration commonly affect large portions of the crust, causing variable degrees of chloritization, sericitization and/or serpentinization depending on the protolith and the conditions of fluid ingression. Retrograde overprint involv
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c5e29512c750a7160211405fe15d9740
https://doi.org/10.5194/egusphere-egu23-5769
https://doi.org/10.5194/egusphere-egu23-5769
We present cosmogenic nucleide data that help to understand the ill-constrained uplift history of the Eastern Aps. Well accepted, but indirect evidence for this uplift history includes: (a) the onset of flexural subsidence of the foreland basins, or
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::524f671e253f58c8bce3421bdb6f1127
https://doi.org/10.5194/egusphere-egu23-2346
https://doi.org/10.5194/egusphere-egu23-2346
We report studies of an ancient, ~10 km wide fold/thrust nappe belt developed as one zone of a 150 km wide, Archean collisional orogen in the North China Craton. Principles of cross-section construction and balancing were utilized to derive the first
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::20a33202ee44f68e56da6ddda45a4f92
https://doi.org/10.5194/egusphere-egu23-6785
https://doi.org/10.5194/egusphere-egu23-6785
Feedbacks between climatic and geological processes are highly controversialand testing them is a key challenge in Earth sciences. The Great Escarpment ofthe Arabian Red Sea margin has several features that make it a useful naturallaboratory for stud
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2a3c66613ce47f5ba2075fb67484318c
https://doi.org/10.5194/egusphere-egu23-16771
https://doi.org/10.5194/egusphere-egu23-16771
The Bohemian Massif is the relic of a major Paleozoic mountain range that is known to have exhumed and its surface levelled in the Permian. The southern part of the Bohemian Massif with high grade metamorphic rocks and magmatic intrusions dips toward
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::19318afd08e6d440f689d6b410c61839
https://doi.org/10.5194/egusphere-egu23-2068
https://doi.org/10.5194/egusphere-egu23-2068
The affiliation of the Ennstal Phyllite Zone (EPZ) to either the micaschist units of the Koralpe-Wölz nappe system (KW-NS) to its south or to nappes of the “Greywacke Zone” to its north and east is still debated. Due to similarities with phyllit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f1c32d762da2c083858e09694fe5989e
https://doi.org/10.5194/egusphere-egu23-8495
https://doi.org/10.5194/egusphere-egu23-8495
Publikováno v:
eISSN
Following the tradition of modeling fluvial landscape evolution, a novel approach describing glacial erosion based on an empirical stream power law was proposed. This approach differs substantially from well established process-based models applied t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::815f74eba620c222dbda60a219a64b67
https://doi.org/10.5194/egusphere-2022-352
https://doi.org/10.5194/egusphere-2022-352