fan delta信息详情
扇形三角洲
delta───n.(Delta)人名；(英、罗、葡)德尔塔；n.（河流的）三角洲；德耳塔（希腊字母的第四个字）
gangetic delta───恒河三角洲
ebro delta───三角洲黑麦
outpost delta───三角洲前哨
fan───v.煽动，激起；吹，吹拂，扇；成扇形散开；飘动；驱散；（棒球、冰球）击球不中；三击不中出局；扩散；辐射；（衣物）呈半圆形展开；n.迷；电扇；风扇；鼓风机；换气扇；折扇，扇子；扇形物；爱好者，崇拜者；山坡脚下的地带；（风车头迎风的）风叶；n.(Fan)（美、法、俄）法恩（人名）
disappearing delta───适合精读
delta dawn───三角洲黎明
kronecker delta───[数]克罗内克符号
delta security───三角洲安全
Various types of fan delta systems have been developed in different evolution stages of faulted basin.───不同类型的扇三角洲沉积可发育在断陷盆地演化的不同阶段。
fan deltaic body can be divided into three subfacies, named fan delta plain, fan delta front and pro-fan delta.───扇三角洲沉积体明显地可划分为：扇三角洲平原亚相、扇三角洲前缘亚相和前扇三角洲亚相。
The sedimentary facies can be classified into alluvial fan, fan delta, lake, stream and swamp.───沉积相可分冲积扇相、扇三角洲相、湖泊相、河流相和沼泽相。
Heterogeneity parameters indicate that the heterogeneity of subaqueous distributary channel of (fan) delta-front is the most serious.───非均质参数表明，（扇）三角洲前缘水下分流河道非均质程度最强。
Alluvial fan and fan delta distribute on the western slope of the depression, and turbidite fan distributes in lake-basin center.───冲积扇、扇三角洲平面上分布在凹陷的西部斜坡带，浊积扇则分布在湖盆中心。
Central low uplifting provides clastic matter for eastern steep slope belt which mainly develops fan delta and nearshore subaqueous fan.───中央低凸起为东部陡坡带提供物源，主要发育扇三角洲和近岸水下扇沉积。
the Upper Cretaceous was in the higher base level, which developed fan delta- lacustrine facies until late Oligocene.───上白垩统基准面快速抬升，沉积区整体处于湖泊-扇三角洲沉积体系，一直持续到古近系渐新统晚期。
from northern and western to southern and eastern , the sedimentary facies transited from fan delta , braided delta to lake facies.───由北、西向南、东，沉积相由扇三角洲、辫状河三角洲向湖泊过渡。
Shuanghe fan delta was high construction composite depositing body. Because the source material and the water stream were steady, the body presented a receding overlain deposition successively.
The eastern part is multi-stages fan delta deposit system witch is controlled by the monocline and step-fault zone and another parts in the area grow alluvial fan system.
The favorable oil bearing facies belts include sublacustrine fan, delta front, fan delta front and the central part of subaqueous fan.
There are six depositional systems classfied for the depression: alluvial fan, underwater fan, fan delta, fluvial, shore-shallow lake sand bar and deep-lake depositional system.
Based on analyses of sedimentary characteristics, the paper is lonsidered that fan delta is a typical set of retrograding ingression lacustrine sequence.
The gentle slope type slope break belt controlled the development of the fan delta system.
The Jurassi reservoir in Wu-Xia area is dominated by lithic sandstone and feldspathic litharenite under alluvial fan, fan delta and braided river sedimentary environments.
It is demonstrated that the west of the depression was the main source supply area during S4 period, where had developed 4 major sources and formed fan delta sands like Shen257, Shen225.