新疆地质
新疆地質
신강지질
XINJIANG GEOLOGY
2009年
4期
350-353
,共4页
准噶尔盆地%沙湾组%坡折带%低位体系域%车排子凸起
準噶爾盆地%沙灣組%坡摺帶%低位體繫域%車排子凸起
준갈이분지%사만조%파절대%저위체계역%차배자철기
Slop break zone%Lowstand system%ChePaizi Uplift%Junggar basin%ShaWan formation
研究表明准噶尔盆地车排子凸起新近系沙湾组在沉积时期,发育有一个与石炭系古潜山有关的古坡折带.古坡折带控制了区内主要目的层沙湾组Ⅱ段沉积和地层圈闭的发育,古坡折带附近是地层型圈闭发育有利区带,具重要油气勘探意义.
研究錶明準噶爾盆地車排子凸起新近繫沙灣組在沉積時期,髮育有一箇與石炭繫古潛山有關的古坡摺帶.古坡摺帶控製瞭區內主要目的層沙灣組Ⅱ段沉積和地層圈閉的髮育,古坡摺帶附近是地層型圈閉髮育有利區帶,具重要油氣勘探意義.
연구표명준갈이분지차배자철기신근계사만조재침적시기,발육유일개여석탄계고잠산유관적고파절대.고파절대공제료구내주요목적층사만조Ⅱ단침적화지층권폐적발육,고파절대부근시지층형권폐발육유리구대,구중요유기감탐의의.
It is be identified by research that ChePaizi Uplift developed a paleoslop break zone related with buried high of Carboniferous system when ShaWan formation deposited.Paleoslop break zone controlled the deposition of N1s2 which is the mainly intended interval and the development of Stratigraphic trap.Around the paleoslop break zone is favorable to the development of Stratigraphic trap,and has important significance to hydrocarbon exploration.