DOI: 10.1016/j.gloplacha.2013.01.003
论文题名: Quantifying the mass transfer from mountain ranges to deposition in sedimentary basins: Source to sink studies in the danube basin-black sea system
作者: Matenco L. ; Andriessen P. ; Andriessen P.A.M. ; Avram C. ; Bada G. ; Beekman F. ; Bielik M. ; Ter Borgh M. ; Cifci G. ; Cvetković V. ; Dinu C. ; Dombradi E. ; Dondurur D. ; Ergun M. ; Francu J. ; Fügenschuh B. ; Garcia-Castellanos D. ; Götz J. ; Horváth F. ; Houseman G. ; Knežević S. ; Kovac M. ; Kralikova S. ; Krijgsman W. ; Kucuk M. ; Legosteva O. ; Lericolais G. ; Jipa D. ; Matenco L. ; Maximov G. ; Melinte M. ; Minar J. ; Munteanu I. ; Munt I.J. ; Olariu C. ; Otto J.C. ; Panin N. ; Plašienka D. ; Reiser M. ; Rundić L. ; Rupprechter M. ; Safanda J. ; Schmid S. ; Schrott L. ; Schuster R. ; Starostenko V. ; Steel R.J. ; Stephenson R. ; Stovba S. ; Sokoutis D. ; Stankoviansky M. ; Stoica M. ; Stojadinović U. ; Toljić M. ; Tomljenović B. ; Ter Voorde M. ; Wong H
刊名: Global and Planetary Change
ISSN: 0921-8323
出版年: 2013
卷: 103, 期: 1 起始页码: 1
结束页码: 18
语种: 英语
英文关键词: Basin evolution
; Black sea
; Coupled orogen
; Danube river basin
; Source to sink systems
Scopus关键词: Basin evolution
; Black sea
; Coupled orogen
; Danube river basin
; Source to sinks
; coupled orogen
; Data integration
; Deposition
; Digital storage
; Geochronology
; Geodynamics
; Sedimentology
; Settling tanks
; Surface topography
; Surfaces
; Watersheds
; Mass transfer
; Sediments
; Landforms
; basin evolution
; delta
; floodplain
; mass transfer
; mountain region
; numerical model
; quantitative analysis
; river system
; sedimentary basin
; source-sink dynamics
; topography
; deposition
; geomorphology
; orogeny
; spatiotemporal analysis
; Black Sea
; Danube Basin
英文摘要: A source to sink systemdescribes the natural link betweenmountains, plains and deltas, by analysing the (re)distribution ofmaterial at shallowcrustal depth and at the Earth's surface, exploring the links between coupled tectonic and surface processes. Sediment fluxes are the product of erosion and movement of material in and from sources (mountains), the transport and movement of sediments and solutes by river systems to the plains, and deposition and storage in sink zones. The ESF-EUROCORES TOPO-EUROPE SourceSink programme is a fully integrated research effort to significantly advance our predictive capabilities on the quantitative analyses of coupled active and past drainage systems bymeans of step-wise 4D reconstructions of sedimentsmass transfer, integrating geophysics, geology, geomorphology, state of the art high-resolution dating, and numerical and analoguemodelling. The area selected for this programme is the Danube River Basin-Black Sea source to sink system, aworld-class natural laboratory that is uniquely suited in the heart of Europe's topography, covering almost half of its surface, providing opportunities for excellent field sites to study in integration surface and subsurface data that cover the complete chain of source, carrier and sink. Quantifying andmodelling the complete systemin relation to the controlling parameters has resulted in significant understanding of forcing factors and linking temporal and spatial scales across multiple orogen and basin systems. This research has provided the opportunity to widen the geographical scope to other natural scenarios, where a number of mountain chains with similar geodynamic genesis separate sedimentary basins with comparable evolution. © 2013 Elsevier B.V. All rights reserved. URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84878230708&doi=10.1016%2fj.gloplacha.2013.01.003&partnerID=40&md5=75ec00bc4c79cae2e237b6c04b5dea9d
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/11229
Appears in Collections: 全球变化的国际研究计划
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作者单位: Netherlands Research Centre for Integrated Solid Earth Science, Utrecht University, Faculty of Geosciences, Budapestlaan 4, 3584CD Utrecht, Netherlands
Recommended Citation:
Matenco L.,Andriessen P.,Andriessen P.A.M.,et al. Quantifying the mass transfer from mountain ranges to deposition in sedimentary basins: Source to sink studies in the danube basin-black sea system[J]. Global and Planetary Change,2013-01-01,103(1).