西南石油大学学报(自然科学版) ›› 2007, Vol. 29 ›› Issue (4): 1-6.DOI: 10.3863/j.issn.1000-2634.2007.04.01

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特征不同的两种扇三角洲相识别与对比

陈景山1 唐青松1 代宗仰1 谭秀成1 刘景环2   

  1. 1.西南石油大学资源与环境学院,四川 成都 610500;2.中国海洋石油南海西部公司,广东 湛江 524057
  • 收稿日期:2007-03-27 修回日期:1900-01-01 出版日期:2007-08-20 发布日期:2007-08-20
  • 通讯作者: 陈景山

RECOGNITION AND CORRELATION OF TWO DISTINCT TYPES OF FAN DELTA FACIES

CHEN Jing-shan1 TANG Qing-song1 DAI Zong-yang1 et al   

  1. Southwest Petroleum University,Chengdu Sichuan 610500,China
  • Received:2007-03-27 Revised:1900-01-01 Online:2007-08-20 Published:2007-08-20
  • Contact: CHEN Jingshan

摘要: 根据构造背景、海平面升降变化、沉积特征等的研究,在琼东南盆地渐新统崖城组中识别出特征明显不同的两种海洋扇三角洲相。靠山型扇三角洲相紧邻高地物源区,发育于盆缘断层下降盘坡度较陡的斜坡区,沉积物往往很粗,分选较差,粒度概率曲线多呈弧形或一段式斜线形,常见重力流成因的递变层理和块状层理,表明沉积水动力以重力流作用为主,兼有牵引流作用。靠扇型扇三角洲相以紧邻陆上冲积扇为特征,通常发育于盆缘断层下降盘坡度相对平缓的斜坡区,沉积物一般较粗,分选较好,粒度概率曲线以两段式和多段式为主,常见牵引流成因的各种交错层理、平行层理和砂纹层理,表明沉积水动力以牵引流作用为主,兼有沉积物重力流作用。靠扇型扇三角洲相砂体的储集性能优于靠山型扇三角洲。盆地边缘斜坡较陡和海平面较高,有利于靠山型扇三角洲相的发育;当盆地边缘斜坡较平缓和海平面相对较低时,则有利于靠扇型扇三角洲相的发育。随盆缘斜坡坡度和海平面升降变化,这两种扇三角洲相可以互相演替。

关键词: 扇三角洲, 沉积特征, 水动力, 重力流, 牵引流, 琼东南盆地

Abstract: According to the research of tectonic setting, eustatic sea level change, depositional feature et al, two distinct types of marine fandelta facies in Yacheng Formation, Oligocene, Qiongdongnan Basin are identified. The fandelta facies, near mountains closely neighbor upon highland source area, are developed on the steeper slope at downthrow block of basinmargin fault. The sediments deposited in these fan deltas are frequently very coarse in the grain size and poor sorting. The pattern of grainsize probability plot mostly displays arcuate or oblique shapes. Graded and massive bedding resulted from gravity flow is common. These show that depositional hydrodynamics is dominated by the gravitycurrent action accompanied with tractional current action. The fandelta facies, near alluvial fan and characterized by being close neighboring upon subaerial alluvial fan, are usually developed on the relatively gentle slope at downthrow block of basinmargin fault. The sediments deposited in these fan deltas are commonly coarser in the grain size and good sorting. The pattern of grainsize probability graph is dominated by double segment and multisegment shapes. Crossbedding, parallel and ripple bedding resulted from tractional current is common, which shows that depositional hydrodynamics is dominated by the tractional current action accompanied with sediment gravity flow action. The reservoir performance of sand body is worse in fandelta facies near mountains than that in the fandelta facies near alluvial fan. It′s in favor of growing fandelta facies near mountains when there are steeper slope and higher sea level in the basin margin and when there are gentle slope at downthrow block and relatively low sea level, then, it is in favor of growing fandelta facies near alluvial fan. Along with the change of slope gradient and sealevel fluctuation in basin margin, these two kinds of fan delta may have the succession mutually.

Key words: fan delta, depositional characteristics, hydrodynamics, gravity current, tractional current, Qiongdongnan Basin

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