石油与天然气地质
石油與天然氣地質
석유여천연기지질
OIL & GAS GEOLOGY
2013年
6期
758-764
,共7页
王俊辉%姜在兴%张元福%高丽明%魏小洁%张文昭
王俊輝%薑在興%張元福%高麗明%魏小潔%張文昭
왕준휘%강재흥%장원복%고려명%위소길%장문소
水槽实验%三角洲模拟%河口坝%分流河道%滑动-滑塌沉积%优质储层
水槽實驗%三角洲模擬%河口壩%分流河道%滑動-滑塌沉積%優質儲層
수조실험%삼각주모의%하구패%분류하도%활동-활탑침적%우질저층
flume experiment%delta simulation%mouth bar%distributary channel%slide-slump deposit%high quality reservoir
为进一步清晰地认识三角洲的沉积特征及砂体发育规律,利用水槽实验对三角洲的发育过程进行了物理模拟,追踪了河口坝、分流河道和滑动-滑塌砂体的沉积过程与沉积特征。通过观察与分析,认为三角洲生长是多次侵蚀与沉积交替的结果,其中洪水期侵蚀作用小于沉积作用,表现为“填低补平”;枯水期侵蚀作用大于沉积作用,表现为“削高填低”。河口坝的发育从水下浅滩开始,按照向前-垂向-向后-横向的顺序进行生长,并且存在单个河口坝的多级分流与多列河口坝的同时分流两种分流方式。三角洲平原河道演变包括河流改道与分流两种方式,分别与洪水和河口坝有关。洪水事件可以作为三角洲前缘滑动-滑塌沉积的触发因素。三角洲是河流搬运、卸载与蓄水体接受、改造沉积物动态变化过程中的产物,在此过程中形成沉积坡折带,它是优质储层发育的有利场所。
為進一步清晰地認識三角洲的沉積特徵及砂體髮育規律,利用水槽實驗對三角洲的髮育過程進行瞭物理模擬,追蹤瞭河口壩、分流河道和滑動-滑塌砂體的沉積過程與沉積特徵。通過觀察與分析,認為三角洲生長是多次侵蝕與沉積交替的結果,其中洪水期侵蝕作用小于沉積作用,錶現為“填低補平”;枯水期侵蝕作用大于沉積作用,錶現為“削高填低”。河口壩的髮育從水下淺灘開始,按照嚮前-垂嚮-嚮後-橫嚮的順序進行生長,併且存在單箇河口壩的多級分流與多列河口壩的同時分流兩種分流方式。三角洲平原河道縯變包括河流改道與分流兩種方式,分彆與洪水和河口壩有關。洪水事件可以作為三角洲前緣滑動-滑塌沉積的觸髮因素。三角洲是河流搬運、卸載與蓄水體接受、改造沉積物動態變化過程中的產物,在此過程中形成沉積坡摺帶,它是優質儲層髮育的有利場所。
위진일보청석지인식삼각주적침적특정급사체발육규률,이용수조실험대삼각주적발육과정진행료물리모의,추종료하구패、분류하도화활동-활탑사체적침적과정여침적특정。통과관찰여분석,인위삼각주생장시다차침식여침적교체적결과,기중홍수기침식작용소우침적작용,표현위“전저보평”;고수기침식작용대우침적작용,표현위“삭고전저”。하구패적발육종수하천탄개시,안조향전-수향-향후-횡향적순서진행생장,병차존재단개하구패적다급분류여다렬하구패적동시분류량충분류방식。삼각주평원하도연변포괄하류개도여분류량충방식,분별여홍수화하구패유관。홍수사건가이작위삼각주전연활동-활탑침적적촉발인소。삼각주시하류반운、사재여축수체접수、개조침적물동태변화과정중적산물,재차과정중형성침적파절대,타시우질저층발육적유리장소。
In order to fully understand the sedimentary characteristics of deltaic deposits and the development patterns of associated sand bodies ,this paper presents a physical simulation of delta development through flume experiment and intro -duces the experiment results in respects of sedimentary process and characteristics of distributary channels ,mouth bars,and slide-slump deposits .The experiment reveals that the development of delta is an alternating process of deposition and ero -sion.Deposition is dominant in flood season when distributary channels carry a heavy sediment load ,while erosion is domi-nant in non-flood season .The growth of mouth bars initiates from an underwater shoal in an order of forward ,upward ,back-ward and transverse .In addition,there are two modes of bifurcation ,i.e.multi-stage bifurcation by one mouth bar and sim-ultaneous bifurcation by multiple mouth bars .The channels on a deltaic plain may evolve in two modes ,i.e.redirection and diversion ,which are related with flood and mouth bar respectively .Flood events could be the trigger of delta front slide-slump deposits .Deltas are formed in the process of sediment transportation and sedimentation determined by the interaction of alluvial and basinal dynamics .In this process ,sedimentary slope break is formed ,which is favorable for the development of high quality reservoirs .