现代地质
現代地質
현대지질
GEOSCIENCE-JOURNAL OF GRADUATE SCHOOL CHINA UNIVERSITY OF GEOSCIENCES
2014年
5期
1008-1016
,共9页
左璠璠%林畅松%高达%赵建华%夏世强%李虹
左璠璠%林暢鬆%高達%趙建華%夏世彊%李虹
좌번번%림창송%고체%조건화%하세강%리홍
高精度层序地层格架%沉积微相%沉积相相序%良里塔格组%塔中西部
高精度層序地層格架%沉積微相%沉積相相序%良裏塔格組%塔中西部
고정도층서지층격가%침적미상%침적상상서%량리탑격조%탑중서부
high-resolution sequence stratigraphic framework%microfacies%facies sequence%Lianglitage For-mation%western Tazhzong
良里塔格组作为优质储层,一直以来都是塔中地区勘探研究的重中之重,但对塔中北斜坡西北部(塔中85-49井区)沉积特征的研究尚且薄弱。综合利用岩心、薄片、测井和地震资料,将良里塔格组划分为3个三级层序、5个体系域和9~15个四级层序,建立了研究区的高精度层序地层格架,并识别出研究区发育的8种沉积微相类型,不同的沉积微相以特定的相序组合成礁滩复合体、中-高能粒屑滩、中-低能粒屑滩和泻湖-滩间海4种沉积相类型。在高精度层序地层与沉积特征研究的基础上,结合地震属性资料,分析了 SQ1和 SQ2时期的沉积相分布特征,重点总结了不同时期高位期和海侵期的沉积相剖面演化规律,并对比了各时期沉积相平面分布的差异性,从而揭示了沉积相的演化规律,有利于进一步指导本区今后的油气勘探工作。
良裏塔格組作為優質儲層,一直以來都是塔中地區勘探研究的重中之重,但對塔中北斜坡西北部(塔中85-49井區)沉積特徵的研究尚且薄弱。綜閤利用巖心、薄片、測井和地震資料,將良裏塔格組劃分為3箇三級層序、5箇體繫域和9~15箇四級層序,建立瞭研究區的高精度層序地層格架,併識彆齣研究區髮育的8種沉積微相類型,不同的沉積微相以特定的相序組閤成礁灘複閤體、中-高能粒屑灘、中-低能粒屑灘和瀉湖-灘間海4種沉積相類型。在高精度層序地層與沉積特徵研究的基礎上,結閤地震屬性資料,分析瞭 SQ1和 SQ2時期的沉積相分佈特徵,重點總結瞭不同時期高位期和海侵期的沉積相剖麵縯化規律,併對比瞭各時期沉積相平麵分佈的差異性,從而揭示瞭沉積相的縯化規律,有利于進一步指導本區今後的油氣勘探工作。
량리탑격조작위우질저층,일직이래도시탑중지구감탐연구적중중지중,단대탑중북사파서북부(탑중85-49정구)침적특정적연구상차박약。종합이용암심、박편、측정화지진자료,장량리탑격조화분위3개삼급층서、5개체계역화9~15개사급층서,건립료연구구적고정도층서지층격가,병식별출연구구발육적8충침적미상류형,불동적침적미상이특정적상서조합성초탄복합체、중-고능립설탄、중-저능립설탄화사호-탄간해4충침적상류형。재고정도층서지층여침적특정연구적기출상,결합지진속성자료,분석료 SQ1화 SQ2시기적침적상분포특정,중점총결료불동시기고위기화해침기적침적상부면연화규률,병대비료각시기침적상평면분포적차이성,종이게시료침적상적연화규률,유리우진일보지도본구금후적유기감탐공작。
The Lianglitage Formation,being the high quality reservoir,has always been the important target in the researches for exploration in Tazhong area.However,researches on the sedimentary characteristics of the northwestern part in the northern slope of Tazhong area (Tazhong 85-49 well)still inadequate.Based on cores, thin-sections,well-logging data and seismic data,the Lianglitage Formation is divided into 3 third-order se-quences,5 systems tracts and 9 to 15 fourth-order sequences,and the high-resolution sequence stratigraphy framework is established in the research area.8 microfacies are identified in research area and according to their specific combination,4 sedimentary facies are recognized in fourth-order sequence,including reef complex,me-dium-high energy grain bank,medium-low-energy grain bank and lagoons-sea.Distributional characteristics of sedimentary facies is studied,based on the foundation of high-resolution sequence stratigraphy and sedimentary characteristics,focusing on the analysis of the facies evolution pattern in cross-section of HST and TST in SQ1 and SQ2 and contrast of facies distributions in flat between different periods.As a result,the evolution pattern of sedimentary facies is revealed,which benefits the further guidance of the oil and gas exploration of research area in the future.