Journal of Palaeogeography
 
Apr. 3, 2025  Home  |  About JOP  |  Editorial Committee  |  Subscription  |  Message  |  Meetings  |  Call for Papers  |  Contact
Journal of Palaeogeography  2022, Vol. 11 Issue (2): 194-221    DOI: 10.1016/j.jop.2022.03.006
Lithofacies palaeogeography and sedimentology Current Issue| Next Issue| Archive| Adv Search Previous  |  Next
Initiation and evolution of coarse-grained deposits in the Late Quaternary Lake Chenghai source-to-sink system: From subaqueous colluvial apron (subaqueous fans) to Gilbert-type delta
Dao-Tao Donga, Long-Wei Qiua,*, Peng-Jie Maa, Guo-Ding Yua, Yu-Zhe Wanga, Shi-Bo Zhoub, Bao-Liang Yanga, He-Qing Huangc, Yong-Qiang Yanga, Xin Lia
aSchool of Geosciences, China University of Petroleum (East China), Qingdao 266580, Shandong Province, China;
bSINOPEC Geophysical Research Institute, Nanjing 211103, Jiangsu Province, China;
cCCCC Second Highway Consultants Co. Ltd., Wuhan 430056, Hubei Province, China
Download: PDF (123283 KB)   HTML (1 KB) 
Export: BibTeX | EndNote (RIS)      Supporting Info
Abstract Investigating the formation and evolution of coarse-grained deposits in modern lakes and the relevant controlling conditions is indispensable to the prediction of reservoir sandbodies, disaster prediction, and limnological research. The source-to-sink system of coarse-grained deposits in Lake Chenghai, a deep, scarped Late Quaternary lake, was investigated in this study based on 62 outcrops, Advanced Land Observing Satellite (ALOS) digital elevation model (DEM) data, and regional geological survey data. The findings include the following: (1) the source areas of coarse-grained deposits in Lake Chenghai were lithologically classified into carbonate source areas, basaltic source areas and siliciclastic source areas, and were geomorphically categorized as scarp type or confluence type. Subaqueous colluvial aprons have formed downstream of the carbonate source areas and scarp-type basaltic source areas, while Gilbert-type deltas have formed downstream of siliciclastic source areas and confluence-type basaltic source areas. (2) The formation and evolution of coarse-grained deposits are controlled by the sediment flux that evolves in synchrony with the geomorphic evolution of the source areas and the sink regimes. Scarps represent the initial landform of the source areas. Source material rolls off or slides down scarps or forms small-scale debris flows before entering the lake. The source material initially formed subaqueous colluvial apron (synonymous with subaqueous fans) where sufficient space was present to accommodate sediments and the basement angle exceeded than the natural angle of repose. As weathering and denudation have progressed, the initial scarps have transformed into confluence-type slopes, and the source material has formed medium- and large-scale debris flows that have entered the lake, resulting in an increase in sediment flux. Consequently, the subaqueous colluvial aprons have rapidly grown and developed subaerial deposits, which have evolved into larger-scale Gilbert-type deltas that overlie the initial aprons. (3) The morphology and distribution of coarse-grained deposits vary in response to differences in quantity and composition of materials from different source areas, which resulting from different rates of weathering and denudation and different sediment input regimes. Firstly, the size and surface slope angle of a subaqueous colluvial apron from a carbonate source are smaller than those of a subaqueous colluvial apron of basaltic origin. Secondly, a Gilbert-type delta from a basaltic source features a greater slope angle and a thicker topset than does a Gilbert-type delta of siliciclastic origin, and the latter exhibits a longer foreset and a thicker bottomset than in the former. Thirdly, the sizes of subaqueous colluvial aprons are not strongly correlated with the sizes of the source areas, while the sizes of Gilbert-type deltas are.
Service
E-mail this article
Add to my bookshelf
Add to citation manager
E-mail Alert
RSS
Articles by authors
Key words: Coarse-grained deposits   Gilbert-type delta   Subaqueous colluvial apron   Subaqueous fans   Source-to-sink   Weathering and denudation   Sediment input regime   Lake Chenghai   Quaternary     
Received: 15 June 2021
Corresponding Authors: * qiulwsd@163.com   
Cite this article:   
. Initiation and evolution of coarse-grained deposits in the Late Quaternary Lake Chenghai source-to-sink system: From subaqueous colluvial apron (subaqueous fans) to Gilbert-type delta[J]. Journal of Palaeogeography, 2022, 11(2): 194-221.
. Initiation and evolution of coarse-grained deposits in the Late Quaternary Lake Chenghai source-to-sink system: From subaqueous colluvial apron (subaqueous fans) to Gilbert-type delta[J]. Journal of Palaeogeography, 2022, 11(2): 194-221.
URL:  
http://journal09.magtechjournal.com/Jweb_jop/EN/10.1016/j.jop.2022.03.006     OR     http://journal09.magtechjournal.com/Jweb_jop/EN/Y2022/V11/I2/194
Copyright © 2014 JOURNAL OF PALAEOGEOGRAPHY
Editorial Office of Journal of Palaeogeography, 20 Xueyuan Road, P. O. Box 902, Beijing 100083, China
Tel: +86-10-62394320; +86–10–62396149     Email: Jpalaeo2012@163.com