FLOW-DEPOSIT INTERACTION IN SUBMARINE LOBES: INSIGHTS FROM OUTCROP OBSERVATIONS AND REALIZATIONS OF A PROCESS-BASED NUMERICAL MODEL

被引:76
作者
Groenenberg, Remco M. [1 ]
Hodgson, David M. [2 ]
Prelat, Amandine [2 ]
Luthi, Stefan M. [1 ]
Flint, Stephen S. [2 ]
机构
[1] Delft Univ Technol, Dept Geotechnol, NL-2628 CN Delft, Netherlands
[2] Univ Liverpool, Dept Earth & Ocean Sci, Stratig Grp, Liverpool L69 3GP, Merseyside, England
关键词
TURBIDITY CURRENTS; KAROO BASIN; SEDIMENT TRANSPORT; STRATIGRAPHIC EVOLUTION; TANQUA DEPOCENTER; HYDRAULIC JUMPS; CHANNEL-MOUTH; FAN; ARCHITECTURE; HYDRODYNAMICS;
D O I
10.2110/jsr.2010.028
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Sediment gravity flows have a propensity to infill lows and build depositional relief, which influences subsequent flows. This flow deposit interaction is intrinsic to the evolution of submarine fans at a range of scales. A novel approach is presented that assesses the interaction of turbidity currents with a subtle but evolving depositional topography. Conceptual models developed from outcrop observations are tested with a process-based numerical model. The outcrop dataset was collected from submarine lobe deposits extensively exposed in the Tanqua depocenter, SW Karoo Basin, South Africa. The process-based numerical model of turbidity-current flow and sedimentation (FanBuilder) is used to mimic the process sedimentology. Input parameters of flows are constrained by observations of the outcrop geology (sedimentology and depositional architecture). Modeling results are analyzed and compared with outcrop observations and, where necessary, lead to iterative refinement of the underlying conceptual process-sedimentological model. The model successfully developed characteristic features of the depositional architecture, such as finger-like geometries and stacking patterns, which are comparable in scale and geometry to those observed in outcrop. The results highlight that lobe deposits have intricate geometries that, when stacked, form a complicated internal stratigraphy, in contrast to simple models of lobes consisting of laterally extensive sheets. In addition, new insights into the processes of lobe growth have come from the modeling that can be tested at outcrop in the future. Process modeling indicates that the stratigraphic complexity can be controlled by a subtle and dynamic depositional surface that drives instability in the position of distributive channels and the site of deposition. As such, this research emphasizes the importance of autogenic controls on the depositional architecture of submarine fan systems.
引用
收藏
页码:252 / 267
页数:18
相关论文
共 56 条
[1]   Laboratory sustained turbidity currents form elongate ridges at channel mouths [J].
Alexander, Jan ;
McLelland, Stuart J. ;
Gray, Thomas E. ;
Vincent, Chris E. ;
Leeder, Mike R. ;
Ellett, Susanna .
SEDIMENTOLOGY, 2008, 55 (04) :845-868
[2]   Flow structure in turbidity currents [J].
Altinakar, MS ;
Graf, WH ;
Hopfinger, EJ .
JOURNAL OF HYDRAULIC RESEARCH, 1996, 34 (05) :713-718
[3]   WEAKLY DEPOSITING TURBIDITY-CURRENT ON A SMALL SLOPE [J].
ALTINAKAR, S ;
GRAF, WH ;
HOPFINGER, EJ .
JOURNAL OF HYDRAULIC RESEARCH, 1990, 28 (01) :55-80
[4]  
[Anonymous], 2006, SEPM SPECIAL PUBLICA
[5]  
BEAUBOEUF RT, 1999, DEEP WATER SANDSTONE
[6]  
Bouma A.H., 1991, GULF COAST ASS GEOLO, V41, P30
[7]  
BOUMA AH, 2000, SEPM SPEC PUBL, V68, P291
[8]   Hydrodynamics of turbid underflows. II: Aggradation, avulsion, and channelization [J].
Bradford, SF ;
Katopodes, ND .
JOURNAL OF HYDRAULIC ENGINEERING, 1999, 125 (10) :1016-1028
[9]   Hydrodynamics of turbid underflows. I: Formulation and numerical analysis [J].
Bradford, SF ;
Katopodes, ND .
JOURNAL OF HYDRAULIC ENGINEERING, 1999, 125 (10) :1006-1015
[10]   Characteristic analysis of turbid underflows [J].
Bradford, SF ;
Katopodes, ND ;
Parker, G .
JOURNAL OF HYDRAULIC ENGINEERING-ASCE, 1997, 123 (05) :420-431