天然气工业
天然氣工業
천연기공업
NATURAL GASINDUSTRY
2009年
10期
28-30
,共3页
张延充%杨爱国%梅燕%邓清华%陈华
張延充%楊愛國%梅燕%鄧清華%陳華
장연충%양애국%매연%산청화%진화
地震勘探%四川盆地%晚二叠世%台地%海槽%地震相%沉积相%预测
地震勘探%四川盆地%晚二疊世%檯地%海槽%地震相%沉積相%預測
지진감탐%사천분지%만이첩세%태지%해조%지진상%침적상%예측
seismic exploration%Sichuan Basin%Late Permian%platform%trough%seismic facies%sedimentary facies%prediction
四川盆地上二叠统长兴组生物礁的预测工作,在20世纪80~90年代主要以地质研究为主,研究初期常有生物礁目标井打不到生物礁,而非目标井又时而钻遇生物礁的现象.近年来,结合地质、钻测井资料,利用区域大剖面地震相预测技术,建立了一套识别晚二叠世末期台地-海槽沉积相带的方法,首次分别在川北、川中及川东地区地震大剖面发现了台地-海槽地震相形迹.在此基础上,对上述地区生物岩隆(礁、滩)有利相带进行了重点识别,总结了台地边缘生物岩隆的地震相预测方法,并编制了四川盆地晚二叠世末期泛开江-梁平海槽古地貌及沉积相预测图,表明环海槽周缘生物岩隆具有延伸远、勘探潜力大的基本态势.通过川东五百梯、川中LG等区块的钻井表明,所应用的技术是预测二叠系碳酸盐岩礁、滩有利区带及勘探部署的实用技术.
四川盆地上二疊統長興組生物礁的預測工作,在20世紀80~90年代主要以地質研究為主,研究初期常有生物礁目標井打不到生物礁,而非目標井又時而鑽遇生物礁的現象.近年來,結閤地質、鑽測井資料,利用區域大剖麵地震相預測技術,建立瞭一套識彆晚二疊世末期檯地-海槽沉積相帶的方法,首次分彆在川北、川中及川東地區地震大剖麵髮現瞭檯地-海槽地震相形跡.在此基礎上,對上述地區生物巖隆(礁、灘)有利相帶進行瞭重點識彆,總結瞭檯地邊緣生物巖隆的地震相預測方法,併編製瞭四川盆地晚二疊世末期汎開江-樑平海槽古地貌及沉積相預測圖,錶明環海槽週緣生物巖隆具有延伸遠、勘探潛力大的基本態勢.通過川東五百梯、川中LG等區塊的鑽井錶明,所應用的技術是預測二疊繫碳痠鹽巖礁、灘有利區帶及勘探部署的實用技術.
사천분지상이첩통장흥조생물초적예측공작,재20세기80~90년대주요이지질연구위주,연구초기상유생물초목표정타불도생물초,이비목표정우시이찬우생물초적현상.근년래,결합지질、찬측정자료,이용구역대부면지진상예측기술,건립료일투식별만이첩세말기태지-해조침적상대적방법,수차분별재천북、천중급천동지구지진대부면발현료태지-해조지진상형적.재차기출상,대상술지구생물암륭(초、탄)유리상대진행료중점식별,총결료태지변연생물암륭적지진상예측방법,병편제료사천분지만이첩세말기범개강-량평해조고지모급침적상예측도,표명배해조주연생물암륭구유연신원、감탐잠력대적기본태세.통과천동오백제、천중LG등구괴적찬정표명,소응용적기술시예측이첩계탄산염암초、탄유리구대급감탐부서적실용기술.
The prediction of bioherm in the Upper Permian Changxing Formation in the Sichuan Basin focused on geologic research in the 1980s and 1990s. It was common in the early stage of the study that wells being targeted at bioherm did not encounter bioherm, while wells that were not targeted at bioherm sometimes encountered bioherm. In recent years, a set of methods for identifying seismic facies of platforms at the end of Late Permian have been developed by using seismic facies prediction techniques of regional large section as well as geologic, drilling and log data. Evidences of platform-trough seismic facies have been identified, for the first time, on Chuanbei (north Sichuan), Chuanzhong (middle Sichuan) and Chuandong (east Sichuan) regional large seismic sections respectively. Based on these jobs, the favorable facies belts on biogenic buildups (reef facies, beach facies) are identified, the seismic facies prediction techniques of biogenic buildups on platform margin are summerized, and the palaeogeomorphology and sedimentary facies of Kaijiang-Liangping Pan-trough at the end of Late Permian in the Sichuan Basin are mapped. The study results show that the biogenic platforms on the periphery of the trough are long in extension and huge in exploration potential. Drilling results in the Wubaiti block of Chuandong (east Sichuan) area and the LG block in the Chuanzhong (middle Sichuan) area indicate that these techniques are suitable for the identification of the favorable targets of reef and beach facies in the Permian carbonates and for exploration planning.