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Experimental sequence stratigraphy of submarine fans on the basis of the theory of shoreline autoretreat

Experimental sequence stratigraphy of submarine fans on the basis of the theory of shoreline autoretreat
基于海岸线自动后退理论的海底扇层序地层学实验
批准号:
12440139
负责人:
MURO Tetsuji
金额:
$5.38万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for Scientific Research (B)
财政年份:
2000
资助国家:
日本
项目状态:
已结题
起止时间:
2000 至 2002

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中文摘要
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英文摘要
The present research was to investigate how the development of deep-water, coarse-grained clastic environments is related to shoreline autoretreat. This problem has been solved by means of flume experiments and theoretical examinations, summarized as below.Deepwater clastic depositional systems can respond sensitively with shoreline autoretreat River deltas cannot prograde over hundreds of kilometers across their shelves during the interval of highstand systems tract development. Even if unlimited time is available to delta growth, there is a clear limit in delta progradation owing to a mechanism ('autobreak') inbuilt in a delta evolving during relative sea-level rise. The termination of the progradation may be far landward of shelf edge. The main factors controlling the limit of delta progradation and the occurrence time of the autobreak event include shelf width, rate of sediment supply, rate of relative-sea level rise, and geometrical parameters of the delta and shelf. It is not abs … More olutely impossible for shelf-edge deltas to be built during slightly rising relative sea level. However, stillstand and falling relative sea level much favor the development of shelf-edge deltas and of sand supply to deep-marine areas, in terms of the delta's travel time to shelf edge. The present study therefore supports the maintenance of the conventional sequence stratigraphic interpretation that sand-rich deep-marine systems are most easily developed during falling and lowstand of relative sea level.A comprehensive understanding of the autogenic response of fluvial deltas to the steady forcing is provided from the theory of shoreline autoretreat. Besides, both autoincision and autobreak represent the moment at which the delta has to lose its original geometry. Any of autostepping and autogenic terrace formation comes out from the effect of the principle of shoreline autoretreat combined with its autocyclic behavior. Allocyclic changes of dynamic conditions only enhance or reduce the inbuilt process of delta systems. Less
期刊论文(33)
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会议论文
T.Muto,R.J.Steel: "The 'autostepping' of delta in a transgressive system"2001 American Association of Petroleum Geologists Annual Meeting, Abstracts & Programs. (印刷中). (2001)
T. Muto, R. J. Steel:“海侵系统中三角洲的‘自动步进’”2001 年美国石油地质学家协会年会,摘要和议程(2001 年出版)。
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Tetsuji Muto: "Shoreline autoretreat substantiated in flume experiments"Journal of Sedimentary Research. 71. 246-254 (2001)
Tetsuji Muto:“水槽实验证实了海岸线自动后退”沉积研究杂志。
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T.Muto: "Autoretreat of shoreline : substantiated in flume experiments"Journal of Sedimentary Research. vol.71(印刷中). (2001)
T.Muto:“海岸线的自动后退:在水槽实验中得到证实”《沉积研究杂志》第 71 卷(出版中)。
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Atsushi Urabe: "Lithostratigraphy and depositional history of the Late Cenozoic hominid-bearing succession in the Yuanmou Basin, Southwest China"Quaternary Science Reviews. 20. 1671-1681 (2001)
Atsushi Urabe:“中国西南元谋盆地晚新生代含原始人类序列的岩石地层学和沉积历史”第四纪科学评论。
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