FORMING CON DITION OF HIGH-QUALITY RESERVOIR AND ITS RELATIVEPROBLEMS IN LOW POROSITY AND PERMEABILITY ENRICHMENT ZONE
Received date: 2002-02-24
Revised date: 2003-03-28
Online published: 2003-04-20
Pertoleum accumulation of low porosity (is smaller than 12% in general)and perme ability (in mostly is 1×10-3μm2 or so)of fragmental rock which become s reservoir is the most primary types of pertoleum accumulations at stabilize cr atonic basin or superposed basin in center and west areas of our country. Howeve r it find that there are many prolific oil and gas accumulations which have high -quality reservoir sandstones in low porosity and permeability oil and gas zone s by the recently exploration. The authors discuss the forming condition of the high-quality reservoirs from the structure, sediment and diagensis of high-qua l ity reservoirs formation and enumerate much element. Expound the principle and m ethod basis that describe and discriminate them. Authors believe that original c omposition and structure of reservoirs are the most crucial element which effect the feature of physical property, congenital provenance condition is ultimate s ource of high-quality reservoir. It is important to explain their genetic from tectonic and deposit environmental condition.
WANG Duo-yun, ZHENG Xi-min, L I Feng-jie, WANG Feng,LIU Zi-liang, WANG Zhi-kun . FORMING CON DITION OF HIGH-QUALITY RESERVOIR AND ITS RELATIVEPROBLEMS IN LOW POROSITY AND PERMEABILITY ENRICHMENT ZONE[J]. Natural Gas Geoscience, 2003 , 14(2) : 87 -91 . DOI: 10.11764/j.issn.1672-1926.2003.02.87
［1］ 李道品，罗迪强，刘雨芬.低渗透油田概念及我国储量分布状况［J ］.低渗透油气田，1996，1(1)：1-7.
［2］ 杨俊杰低渗透率油气藏开发技术，低渗透砂岩油气层的地质特征［M］.北京：石油工业出版社，1993.
［3］ 谢庆邦，贺静中国油气储层研究论文集，陕甘宁盆地南部上三叠统延长组低渗透砂岩储层评价［M］.北京：石油工业出版社，1993:313-332.
［4］ 李凤杰，王多云，郑希民，等陕甘宁盆地华池地区延长组缓坡带三角洲前缘的微相构成［J］.沉积学报，2002，20(4)：582-587.
［5］ 王多云，陈应泰，徐洪生受周期性湖平面升降控制的冲积扇－扇三角洲沉积体系［J］.沉积学报，1991，9(4)：43-48.
［6］ 王多云沼泽环境中的河流类型及其侧向演化模式［J］.沉积学报，1993， 11(3)：1-6.
［7］ 史基安，陈国俊，王琪，等塔里木盆地西部层序地层与沉积、成岩演化［M ］.北京科技出版社，2001:186-214.
［8］Salem A M，Morad S，Luiz F, et al.Diagenesis and reservoir-qua lity evolution of fluvial sandstones during progressive burial and uplift:eviden ce from the upper jurassic boipeda member,Reconcavo basin,Northeastern Brazil［J ］. AAPG Bulletin, 2002, 84(7):1015-1040.
［9］Salman Bloch, Robert H, Lander B. Anomalously high porosi ty and permeability in deeply burried sandstone reservoies:Origin and predictabi lity［J］. AAPG Bulletin, 2002,86(2):1-328.
［10］ Sylvia M C, Luiz F, Rogerio Schiffer,et al. Depositional and diagen etic controls on the reservoir quality of lower Cretaceous Pendencia sandstones, Potiguar rift basin,Brazil［J］. AAPG Bulletin, 2002,86(11):1719-1742.
［11］ 王琪，史基安，陈国俊，等.石油侵位对碎屑储集岩成岩序列的影响及其与孔隙演化的关系［J］.沉积学报，1999，17(4)：115-122.
［12］ Robert S T，James J HPermeability characterization of diat- ri butary mouth bar sandstones in Prudhoe Bay field,Alaska:How horizontal co res reduce isk in developing deltaic reservoirs［J］. AAPG Bulletin, 2002, 85(3 ):159-475.
［13］Galloway W E, Habday D K. Terrigeneous Clastics Deposi- tional S ystem［M］.New York: Spring-Verlag, 1983.
［14］ Bertaux J. Treatment-fluid selection for sandstone acidizing: Permeab ility impairment in potassic mineral sandstones［J］. SPEPE,1989,(2):41-48.
［15］ Chandle M A, Goggin D J, Lake L W. A mechanical field permeameter for ma king rapid, non-destructive, permeability measurements［J］. Journal of Sedimen tary Petology, 1989,59(4):613-615.
［16］ Civan F, Knapp R M. Effect of Clay Swelling and Fines Mig- ratio n on Formtion Permeability［R］. SPE paper 16235,1987.
［17］ Necmettin Mungan. Permeability reduction through change in pH and salini ty［J］. JPT Dec, 1965，1449-1453.
［18］ Vaddilellis G D, Graves R M, Crafton J W. Point Permeab- ili ty Measurements Using a liquid Minipermeameter to Study Formation Damage Mechanisms［R］. SPE Paper 23785, 2000.
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