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)
2009年
6期
968-975
,共8页
杜旭东%赵齐辉%倪国辉%蔡红芽%周开凤%陈杏霞%朱建伟
杜旭東%趙齊輝%倪國輝%蔡紅芽%週開鳳%陳杏霞%硃建偉
두욱동%조제휘%예국휘%채홍아%주개봉%진행하%주건위
尤罗勃钦%油田%裂缝型储层%储层评价%油气分布规律%俄罗斯%油气
尤囉勃欽%油田%裂縫型儲層%儲層評價%油氣分佈規律%俄囉斯%油氣
우라발흠%유전%렬봉형저층%저층평개%유기분포규률%아라사%유기
Yurubcheno%oil fields%fracture reservoir%reservoir evaluation%reservoir distribution%Russia%petroleum gas
利用俄罗斯测井系列的测井曲线,系统评价了尤罗勃钦油田的碳酸盐岩储层.在对岩心分析和岩性、电性、物性和含油性特征研究的基础上,充分分析了该油田储层测井响应,针对该区碳酸盐岩储层双重孔隙介质的特点,建立了识别储层类型、裂缝性质等测井评价参数.据此把储层分为基岩型、微裂缝型和大裂缝型3大类.裂缝型储层发育方向在平面上是北东-南西向和北西-南东向,分别与尤罗勃钦组、多尔戈克金组、库尤姆宾组中白云岩分布和古潜山构造高部位方向一致;纵向上裂缝和大裂缝储层发育段厚度一般在距剥蚀面以下0~100 m左右,与白云岩溶蚀带发育一致.裂缝和大裂缝型储层发育段控制了油气井分布,但裂缝型储层分布仍极不均匀.油气分布主要受储层岩性和其在古潜山的构造位置控制:尤罗勃钦组岩性较单一并处在古潜山构造高部位,油井产量高;多尔戈克金组发育泥岩、泥质白云岩和白云岩互层,虽构造部位较高,但有的井出油,有的井出水,产油量也不高;库尤姆宾组虽岩性单一但构造部位不佳,油气产量也较低.
利用俄囉斯測井繫列的測井麯線,繫統評價瞭尤囉勃欽油田的碳痠鹽巖儲層.在對巖心分析和巖性、電性、物性和含油性特徵研究的基礎上,充分分析瞭該油田儲層測井響應,針對該區碳痠鹽巖儲層雙重孔隙介質的特點,建立瞭識彆儲層類型、裂縫性質等測井評價參數.據此把儲層分為基巖型、微裂縫型和大裂縫型3大類.裂縫型儲層髮育方嚮在平麵上是北東-南西嚮和北西-南東嚮,分彆與尤囉勃欽組、多爾戈剋金組、庫尤姆賓組中白雲巖分佈和古潛山構造高部位方嚮一緻;縱嚮上裂縫和大裂縫儲層髮育段厚度一般在距剝蝕麵以下0~100 m左右,與白雲巖溶蝕帶髮育一緻.裂縫和大裂縫型儲層髮育段控製瞭油氣井分佈,但裂縫型儲層分佈仍極不均勻.油氣分佈主要受儲層巖性和其在古潛山的構造位置控製:尤囉勃欽組巖性較單一併處在古潛山構造高部位,油井產量高;多爾戈剋金組髮育泥巖、泥質白雲巖和白雲巖互層,雖構造部位較高,但有的井齣油,有的井齣水,產油量也不高;庫尤姆賓組雖巖性單一但構造部位不佳,油氣產量也較低.
이용아라사측정계렬적측정곡선,계통평개료우라발흠유전적탄산염암저층.재대암심분석화암성、전성、물성화함유성특정연구적기출상,충분분석료해유전저층측정향응,침대해구탄산염암저층쌍중공극개질적특점,건립료식별저층류형、렬봉성질등측정평개삼수.거차파저층분위기암형、미렬봉형화대렬봉형3대류.렬봉형저층발육방향재평면상시북동-남서향화북서-남동향,분별여우라발흠조、다이과극금조、고우모빈조중백운암분포화고잠산구조고부위방향일치;종향상렬봉화대렬봉저층발육단후도일반재거박식면이하0~100 m좌우,여백운암용식대발육일치.렬봉화대렬봉형저층발육단공제료유기정분포,단렬봉형저층분포잉겁불균균.유기분포주요수저층암성화기재고잠산적구조위치공제:우라발흠조암성교단일병처재고잠산구조고부위,유정산량고;다이과극금조발육니암、니질백운암화백운암호층,수구조부위교고,단유적정출유,유적정출수,산유량야불고;고우모빈조수암성단일단구조부위불가,유기산량야교저.
The carbonate reservoir evaluation based on well logging data of Russian logging series is done in Yurubcheno oil field in Siberian platform. On the basis of the conversional log characteristic analysis, evaluation parameters from the logging data are given for identification of the reservoir types, fractures, shale intervals of the formation and tight reservoirs in the carbonate reservoir with dual porosity. The reservoirs are classified into matrix type, micro fracture type and macro fracture type. The preferential directions of fractured reservoir distribution are NE-SW and NW-SE which are consistent with the distribution of carbonate and the structural high of the buried hill. It generally locates 0-100 m under unconformity which corresponds to the distribution direction of the dolomite corrosion zone, which controls the distribution of the high production wells. But the distribution of the fractured reservoir is heterogeneous and anisotropic in this field. Factors controlling the distribution of oil and gas in this field are the lithology of the reservoir and its structural location in the buried hill. The reservoir in Yurubcheno Formation, which is pure dolomite and has good location in the structure, has high oil and gas yield. There is poor oil and gas production in the reservoirs in Dolgoktinskaya Formation, where the lithology is not pure dolomite, and the Kuyumbinskaya Formation which located at a lower structu-ral location.