Source‐to‐sink analysis for the mud and sand in the late‐Quaternary Qiantang River incised‐valley fill and its implications for delta‐shelf‐estuary dispersal systems globally

Sedimentology ◽  
2021 ◽  
Author(s):  
Xia Zhang ◽  
Chun‐Ming Lin ◽  
Robert W. Dalrymple ◽  
SHOU‐YE Yang
Keyword(s):  
Late Quaternary ◽  
Incised Valley ◽  
Valley Fill ◽  
Qiantang River ◽  
Source To Sink

Characteristics and Formation of Late Quaternary Incised-Valley-Fill Sequences in Sediment-Rich Deltas and Estuaries: Case Studies from China

2006 ◽  
pp. 141-160 ◽  
Author(s):  
CONGXIAN LI ◽  
PING WANG ◽  
DAIDU FAN ◽  
SHOUYE YANG
Keyword(s):  
Case Studies ◽  
Late Quaternary ◽  
Incised Valley ◽  
Valley Fill

scholarly journals Variation of Sulfur Isotopes in Sediments from the Late Quaternary Qiantang River Incised Valley, Eastern China

2020 ◽  
Author(s):  
Kaixi Jiang ◽  
Chunming Lin ◽  
Xia Zhang
Keyword(s):  
Sulfur Isotopes ◽  
Late Quaternary ◽  
Eastern China ◽  
Incised Valley ◽  
Qiantang River

Late Quaternary incised-valley fill of the Yangtze delta (China): its stratigraphic framework and evolution

2002 ◽  
Vol 152 (1-2) ◽  
pp. 133-158 ◽  
Author(s):  
Congxian Li ◽  
Ping Wang ◽  
Heping Sun ◽  
Jiaqiang Zhang ◽  
Daidu Fan ◽  
...  
Keyword(s):  
Late Quaternary ◽  
Yangtze Delta ◽  
Incised Valley ◽  
Valley Fill ◽  
Stratigraphic Framework

Late Quaternary multiple incised valley systems: An unusually well-preserved stratigraphic record of two interglacial valley-fill successions from the Arno Plain (northern Tuscany, Italy)

Sedimentology ◽  
2017 ◽  
Vol 64 (7) ◽  
pp. 1901-1928 ◽  
Author(s):  
Veronica Rossi ◽  
Alessandro Amorosi ◽  
Giovanni Sarti ◽  
Sara Mariotti
Keyword(s):  
Late Quaternary ◽  
Incised Valley ◽  
Valley Fill ◽  
Stratigraphic Record

Sedimentary architecture and chronostratigraphy of a late Quaternary incised-valley fill: A case study of the late Middle and Late Pleistocene Rhine system in the Netherlands

2016 ◽  
Vol 131 ◽  
pp. 211-236 ◽  
Author(s):  
J. Peeters ◽  
F.S. Busschers ◽  
E. Stouthamer ◽  
J.H.A. Bosch ◽  
M.W. Van den Berg ◽  
...  
Keyword(s):  
The Netherlands ◽  
Late Pleistocene ◽  
Late Quaternary ◽  
Incised Valley ◽  
Valley Fill ◽  
Sedimentary Architecture ◽  
Middle And Late Pleistocene

A well-preserved Eemian incised-valley fill in the southern North Sea Basin, Belgian Continental Shelf - Coastal Plain: Implications for northwest European landscape evolution

2018 ◽  
Vol 43 (9) ◽  
pp. 1913-1942 ◽  
Author(s):  
M. De Clercq ◽  
T. Missiaen ◽  
J. Wallinga ◽  
O. Zurita Hurtado ◽  
A. Versendaal ◽  
...  
Keyword(s):  
Continental Shelf ◽  
North Sea ◽  
Coastal Plain ◽  
Landscape Evolution ◽  
Incised Valley ◽  
Valley Fill ◽  
Southern North Sea ◽  
Belgian Continental Shelf

scholarly journals Cryostratigraphy, sedimentology, and the late Quaternary evolution of the Zackenberg River delta, northeast Greenland

2017 ◽  
Vol 11 (3) ◽  
pp. 1265-1282 ◽  
Author(s):  
Graham L. Gilbert ◽  
Stefanie Cable ◽  
Christine Thiel ◽  
Hanne H. Christiansen ◽  
Bo Elberling
Keyword(s):  
Late Quaternary ◽  
Sediment Cores ◽  
River Delta ◽  
Optically Stimulated Luminescence ◽  
Delta Plain ◽  
Valley Fill ◽  
Subaerial Exposure ◽  
Facies Associations ◽  
Delta Progradation ◽  
Ice Content

Abstract. The Zackenberg River delta is located in northeast Greenland (74°30′ N, 20°30′ E) at the outlet of the Zackenberg fjord valley. The fjord-valley fill consists of a series of terraced deltaic deposits (ca. 2 km2) formed during relative sea-level (RSL) fall. We investigated the deposits using sedimentological and cryostratigraphic techniques together with optically stimulated luminescence (OSL) dating. We identify four facies associations in sections (4 to 22 m in height) exposed along the modern Zackenberg River and coast. Facies associations relate to (I) overriding glaciers, (II) retreating glaciers and quiescent glaciomarine conditions, (III) delta progradation in a fjord valley, and (IV) fluvial activity and niveo-aeolian processes. Pore, layered, and suspended cryofacies are identified in two 20 m deep ice-bonded sediment cores. The cryofacies distribution, together with low overall ground-ice content, indicates that permafrost is predominately epigenetic in these deposits. Fourteen OSL ages constrain the deposition of the cored deposits to between approximately 13 and 11 ka, immediately following deglaciation. The timing of permafrost aggradation was closely related to delta progradation and began following the subaerial exposure of the delta plain (ca. 11 ka). Our results reveal information concerning the interplay between deglaciation, RSL change, sedimentation, permafrost aggradation, and the timing of these events. These findings have implications for the timing and mode of permafrost aggradation in other fjord valleys in northeast Greenland.

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