吉林大学学报(地球科学版)
吉林大學學報(地毬科學版)
길림대학학보(지구과학판)
JOURNAL OF JILIN UNIVERSITY(EARTH SCIENCE EDITION)
2010年
1期
30-37
,共8页
曹金舟%任战利%高兴军%康立明%张娜%韩伟%王敏
曹金舟%任戰利%高興軍%康立明%張娜%韓偉%王敏
조금주%임전리%고흥군%강립명%장나%한위%왕민
鄂尔多斯盆地%涧峪岔地区%三叠系%三角洲平原%分流河道%油田
鄂爾多斯盆地%澗峪岔地區%三疊繫%三角洲平原%分流河道%油田
악이다사분지%간욕차지구%삼첩계%삼각주평원%분류하도%유전
Ordos basin%Jianyucha region%Triassic%delta plain%distributary channel%oil fields
运用石油地质综合方法,结合现代测试技术、测井技术,将宏观与微观相结合、区域资料与单井资料相结合,在对岩石学、粒度、岩心沉积相标志及测井曲线等进行详细研究的基础上,对子北油田涧峪岔油区三叠系长6油层组各小层沉积微相及其分布规律进行了深入研究.长6油层组储层均属于三角洲平原沉积,发育分流河道和分流间湾两种主要的沉积微相.砂体展布受北东-南西走向的分流河道控制,自长6~2至长6~1,主砂体走向及分布位置有一定的继承性.分流河道砂体对本地区油气聚集有重要控制作用.
運用石油地質綜閤方法,結閤現代測試技術、測井技術,將宏觀與微觀相結閤、區域資料與單井資料相結閤,在對巖石學、粒度、巖心沉積相標誌及測井麯線等進行詳細研究的基礎上,對子北油田澗峪岔油區三疊繫長6油層組各小層沉積微相及其分佈規律進行瞭深入研究.長6油層組儲層均屬于三角洲平原沉積,髮育分流河道和分流間灣兩種主要的沉積微相.砂體展佈受北東-南西走嚮的分流河道控製,自長6~2至長6~1,主砂體走嚮及分佈位置有一定的繼承性.分流河道砂體對本地區油氣聚集有重要控製作用.
운용석유지질종합방법,결합현대측시기술、측정기술,장굉관여미관상결합、구역자료여단정자료상결합,재대암석학、립도、암심침적상표지급측정곡선등진행상세연구적기출상,대자북유전간욕차유구삼첩계장6유층조각소층침적미상급기분포규률진행료심입연구.장6유층조저층균속우삼각주평원침적,발육분류하도화분류간만량충주요적침적미상.사체전포수북동-남서주향적분류하도공제,자장6~2지장6~1,주사체주향급분포위치유일정적계승성.분류하도사체대본지구유기취집유중요공제작용.
By means of comprehensive study on petroleum geology, modern test technology,well logging technology, and the combination of macroexamination with microexamination, regional information with well data, through the petrology, grain size, signs of logging, etc, the authors studied micro-sedimentary facies and distribution law for the Chang 6 reservoir of Triassic in Jianyucha region in Zibei oil field. New understanding of sedimentary microfacies is concluded as followed:Chang 6 reservoir belongs to the delta plain distributary channel sedimentary which includes two main types of sedimentary microfacies-distributary channel and distributary bay.The sandbody is controled by distributary channel which alignment is from northeast to southwest, and the main sandbody trend and distribution have a certain succession in profile section. The delta plain distributary channel sedimentary is beneficial to oil-gas gathering.