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)
2015年
6期
1567-1579
,共13页
操应长%张会娜%葸克来%赵贤正%周磊%崔周旗%金杰华
操應長%張會娜%葸剋來%趙賢正%週磊%崔週旂%金傑華
조응장%장회나%사극래%조현정%주뢰%최주기%금걸화
中深层%有效储层%物性下限%控制因素%饶阳凹陷
中深層%有效儲層%物性下限%控製因素%饒暘凹陷
중심층%유효저층%물성하한%공제인소%요양요함
medium-deep reservoirs%effective reservoirs%petrophysical parameter cutoff%controlling factors%Raoyang sag
综合运用实测物性、测井解释物性、试油等资料,分别应用分布函数曲线法、测试法、试油法求取饶阳凹陷南部古近系中深层不同深度段的有效储层物性下限,并对物性下限与深度的关系进行了回归拟合。在此基础上,引入孔隙度差值,结合饶阳凹陷南部古近系中深层储层的沉积特征、成岩作用特征及地层压力特征分析,探讨了有效储层发育的控制因素。结果显示:研究区辫状河三角洲前缘水下分流河道、河口坝沉积微相有利于有效储层的发育,而席状砂、水下分流间湾砂体有效储层发育较少,储层物性较差;厚度大于3 m 的砂体有利于有效储层的发育。研究表明:成岩作用对储层的影响主要表现为压实作用和胶结作用使储层物性降低,而溶蚀作用使储层形成次生孔隙、提高储集物性;地层超压的存在促进有效储层的发育。
綜閤運用實測物性、測井解釋物性、試油等資料,分彆應用分佈函數麯線法、測試法、試油法求取饒暘凹陷南部古近繫中深層不同深度段的有效儲層物性下限,併對物性下限與深度的關繫進行瞭迴歸擬閤。在此基礎上,引入孔隙度差值,結閤饒暘凹陷南部古近繫中深層儲層的沉積特徵、成巖作用特徵及地層壓力特徵分析,探討瞭有效儲層髮育的控製因素。結果顯示:研究區辮狀河三角洲前緣水下分流河道、河口壩沉積微相有利于有效儲層的髮育,而席狀砂、水下分流間灣砂體有效儲層髮育較少,儲層物性較差;厚度大于3 m 的砂體有利于有效儲層的髮育。研究錶明:成巖作用對儲層的影響主要錶現為壓實作用和膠結作用使儲層物性降低,而溶蝕作用使儲層形成次生孔隙、提高儲集物性;地層超壓的存在促進有效儲層的髮育。
종합운용실측물성、측정해석물성、시유등자료,분별응용분포함수곡선법、측시법、시유법구취요양요함남부고근계중심층불동심도단적유효저층물성하한,병대물성하한여심도적관계진행료회귀의합。재차기출상,인입공극도차치,결합요양요함남부고근계중심층저층적침적특정、성암작용특정급지층압력특정분석,탐토료유효저층발육적공제인소。결과현시:연구구변상하삼각주전연수하분류하도、하구패침적미상유리우유효저층적발육,이석상사、수하분류간만사체유효저층발육교소,저층물성교차;후도대우3 m 적사체유리우유효저층적발육。연구표명:성암작용대저층적영향주요표현위압실작용화효결작용사저층물성강저,이용식작용사저층형성차생공극、제고저집물성;지층초압적존재촉진유효저층적발육。
Based on measured properties ,such as physical properties of log interpretation an d oil production tests ,the petrophysical parameter cutoff and depth of medium‐deep effective reservoirs of Paleogene in the southern Raoyang sag are determined by distribution function curve method , test method ,oil production test method ,and the fitting formula of petrophysical parameters .Further ,the porosity difference is introduced combining with the analysis on the characteristics of sediments , diagenesis ,and reservoir pressure of the medium‐deep reservoirs in southern Raoyang sag ; and the controlling factors of effective reservoirs are discussed . The results show that the subaqueous distributary channel and estuary bar of fan delta front subfacies are suitable for the grow th of effective reservoirs ;while the properties of delta‐front sheet sand and inter distributary bays are weak ,where less effective reservoirs are developed .When the thickness of sand is greater than 3 meters ,the sand could be developed into an effective reservoir .Compaction and cementation are the main factors to decrease porosity and permeability of reservoirs ;while dissolution increases the secondary pores ,and in turn ,makes the physical property of reservoir better . The existence of overpressure promotes the development of effective reservoirs .