干旱区生态环境知识资源中心(Arid): 岌岌湖现代水下加积扇与东坷里三角洲层序地层学意义比较

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	岌岌湖现代水下加积扇与东坷里三角洲层序地层学意义比较
其他题名	Comparison of Sequence Stratigraphic Significance between East Coulee Delta and Jijihu Modern Subaqueous Aggradational Fan(SAF)
	李绍虎 1; 周继兵 2; 贾丽春 3; 王昭辉 2; 李宝庆 4; 马风华 4; 王程 4
来源期刊	沉积学报
ISSN	1000-0550
出版年	2011
卷号	29 期号:4 页码:613-621
中文摘要	对比研究东坷里三角洲(East Coulee Delta)和岌岌湖现代水下加积扇的层序地层学意义,认为:(1)东坷里三角洲发育LSTTST组合、FSST组合,其分属两个层序;(2)岌岌湖SAF发育FSSTLSTTST组合、FSST组合,亦分属两个层序;(3)两个陆相实例证明最大水泛面之后均未有高位体系域出现,可能代表非海相与海相背景之间的差异。论文对复合层序边界等问题进行了讨论。
英文摘要	Jijihu modern subaqueous aggradational fan(SAF)in Jungar Basin,Xinjiang Province,China,is 24m arch length and 10m radii．Jijihu SAF consists of alluvial fan 1,unit A(SAF),unit B(slop beds,retrogradational beds and flooding mud-sand beds),unit C(alluvial fan 2)and unit D(alluvial fan 3),which have been documented by Li by observing and digging during one week in the condition of 40 degree centigrade Junggar Basin after desert flood in 2007 summery time． Field observation directs as followings:(1)Exception of alluvial fan 1,Jijihu SAF has the similar stacking patterns with East Coulee Delta(Posamentier et al．,1992)．Especially,there is a 1cm red mud bed between alluvial fan 1 and SAF,directing that they belong to continuous sedimentation documented by digging．Although SAF covers alluvial fan 1 in the Northern side of pool,another isochronous unit opposite Jijihu SAF about 10m away in the Southern side directs the lowest alluvial fan clearly．Thereby,alluvial fan 1 becomes the lowest unit that may be interpreted as falling stage systems tract(FSST)during forced regression associated with incision,showing that pond water reaches lowest level．(2)Subsequently,pond level begins to rise,sediments supply exceeds the rate of level rise,and SAF(unit A)develops during normal regression,so that SAF may be interpreted as lowstand systems tract(LST)according to present scenario of sequence stratigraphy．(3)Associated with level rise exceeds sediments supply,unit B develops as follows:Firstly,fine mud-sands begin to accumulate in front of SAF forming slope beds(i．e．,healing phase wedge of Posamentiaer and Allen(1993))．Secondly,coarse sediments such as gravels deposits on the top of SAF,directing retrogression stacking patterns landward．Finely,level reaches to maximum,flooding mud-sand beds begin to precipitate under hot wind in the Junggar Desert．Therefore,three parts(unit B)above may record as transgressive systems tract(TST)during transgression．(4)The second desert flood forms alluvial fan 2(unit C)and 3(unit D)incising one by one,they may be interpreted as falling stage systems tract(FSST)of another sequence during forced regression． This article has compared the sequence stratigraphic significance between East Coulee Delta in Alberta and Jijihu subaqueous aggradational fan(SAF),and concluded as follows:(1)East Coulee Delta develops LST-TST superposition and FSST superposition that belong to two different depositional sequences;(2)Jijihu SAF develops FSST-LST-TST superposition and FSST superpositions that are attributed to two depositional sequences,too;(3)two outcrops has proved that no highstand systems tract develops after maximum flooding surface in modern small-scale pond,it is possible to represent difference between marine and non-marine settings due to transporting energy in non-marine setting not enough to carry sediments into pond．This paper has also discussed some key problems such as sequence boundary that is redefined as remnant maximum flooding surface(RMFS)and its correlative subaerial unconformity(CSU)．Furthermore,this paper suggests avoidance of highstand normal regression term．In subsequent thesis authors will suggest that stillstand normal regression replace highstand normal regression．
中文关键词	岌岌湖现代水下加积扇 ; 东坷里三角洲 ; 层序地层学 ; 下降期体系域 ; 避免高位正常海退
英文关键词	Jijihu modern subaqeous aggradational fan(SAF) East Coulee Delta sequence stratigraphy falling stage systems tract(FSST) avoidance of highstand systems tract
语种	中文
国家	中国
收录类别	CSCD
WOS类目	GEOLOGY
WOS研究方向	Geology
CSCD记录号	CSCD:4271193
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/226240
作者单位	1.(武汉)中国地质大学资源学院, (武汉)构造与油气资源教育部重点实验室, 武汉, 湖北 430074, 中国; 2.新疆地矿局第九地质大队, 乌鲁木齐, 新疆 830000, 中国; 3.山西省第三地质工程勘察院, 榆次, 山西 030600, 中国; 4.(武汉)中国地质大学资源学院, 武汉, 湖北 430074, 中国
推荐引用方式 GB/T 7714	李绍虎,周继兵,贾丽春,等. 岌岌湖现代水下加积扇与东坷里三角洲层序地层学意义比较[J],2011,29(4):613-621.
APA	李绍虎.,周继兵.,贾丽春.,王昭辉.,李宝庆.,...&王程.(2011).岌岌湖现代水下加积扇与东坷里三角洲层序地层学意义比较.沉积学报,29(4),613-621.
MLA	李绍虎,et al."岌岌湖现代水下加积扇与东坷里三角洲层序地层学意义比较".沉积学报 29.4(2011):613-621.