梨树断陷十屋油田营城组物源体系、沉积特征及储层特征研究
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摘要
梨树断陷十屋油田位于松辽盆地东南部,为晚侏罗世以来发育而成的断坳叠置型复合盆地,其中十屋油田位于盆地的中心部位,是盆地内油气资源最富集的区带之一。本论文在综合利用岩心、录井、测井及大量分析化验等资料的基础上,以沉积学理论和方法为指导,结合地质统计学,对十屋油田营城组的物源体系和沉积特征等进行了系统的研究,并对其储层特征和储层物性的控制因素进行了初步探讨。
十屋油田营城组沉积时期盆地内发育有多个物源体系,本文通过聚类分析法、碎屑颗粒组分法、重矿物法、砂砾岩百分含量分布法和地层倾角测井法等方法对十屋油田营城组物源体系进行了综合分析,认为研究区在营城组沉积时期存在有三大物源体系,分别是西北方向的西北物源区、北部斜坡物源区和东部斜坡物源区。三个物源体系在营城组各时期继承发育,其中西北部物源区母岩类型以沉积岩和岩浆岩为主;北部斜坡物源区母岩类型以岩浆岩为主;东部斜坡物源区母岩类型以岩浆岩和变质岩为主。
十屋油田营城组时期主要发育了扇三角洲、辫状河三角洲和湖泊等沉积体系类型。营五段沉积时期,三个物源体系均在研究区形成扇三角洲沉积;营四段沉积时期,西北和北部物源体系仍然发育扇三角洲沉积,但扇三角洲范围较营五段时期有所减小,而东部物源体系仍为辫状河三角洲沉积;营三段到营一段沉积时期,三个物源体系均形成辫状河三角洲沉积,形成研究区的混源沉积特征。梨树断陷十屋油田营城组各沉积时期物源体系和沉积体系特征继承性较强,形成了该区“多物源混源沉积、各物源源间存异、各时期继承发育”的沉积格局。十屋油田营城组发育的扇三角洲是缓坡背景下发育的粗碎屑三角洲,发育有扇三角洲平原、前缘和前扇三角洲等亚相,水下分流河道、河口坝和席状砂等砂体构成扇三角洲的骨架砂体,兼具重力流沉积(泥石流)和牵引流沉积特征;研究区发育的辫状河三角洲沉积物粒度细于扇三角洲,也发育有辫状河三角洲平原、前缘和辫状河前三角洲,不发育重力流沉积;湖泊相主要发育滨浅湖和深湖-半深湖相沉积,滨浅湖以薄层砂岩与泥岩互层为特征,发育有生物钻孔构造;深湖-半深湖以大套灰黑色、黑色泥岩或夹薄层泥质砂岩为特征。
十屋油田营城组储层属低孔低渗储层,储集空间由原生孔隙、次生溶解孔隙和裂缝构成。并认为研究区储层物性主要受沉积作用的控制,以扇三角洲沉积相的储层物性最好,辫状河三角洲次之,扇三角洲中的泥石流沉积储层物性最差。
Shiwu Oilfield in Lishu fault Depression, located in the southeast of Songliao basin, has developed into a composite basin of fault depression superposition since Late Jurassic. And Shiwu Oilfield, in the center of the basin, is one of the richest oil and gas zone. In this paper, on the basis of core, logging, and a lot of analysis data, using sedimentary theories and methods as a guide, combined with mathematic theory of statistics, conducts a study of provenance Systems and sedimentary characteristics of Yingcheng Formation in Shiwu Oilfield.
Through the methods of cluster analysis, clastic particles component, heavy minerals, the percentages of glutenite and dipmeter, carrying out a comprehensive analysis of provenance systems of Yingcheng Formation with the character of multi-source deposition in Shiwu Oilfield leads to a perspective that there are three depositional source systems, which are North Slope provenance, east Slope provenance and northwest provenance. And rock type is mainly igneous rock in the North Slope source Area. Rock types of the eastern slope source area are mainly magmatic rocks and metamorphic rocks. In Northwest source area rock types are mainly sedimentary and igneous rocks.Clastic grains from three directions gather in the study area, where the distribution extent of sediments from north slope and northwest are borader.
In this study area, it mainly developed fan delta, braided river delta and lake sedimentary system types: fan delta forming in the early sedimentary period of Yingcheng Formation, distributing in the northern part and the eastern slope of the basin, is made up of sand bodies such as underwater distributary channel, mouth bar and sheet sand, which are current deposits and gravity flow deposits like mud flow. Braided river delta developing in the whole basin in the mid and late of the Yingcheng Formation, also has distributary channel and mouth bar and sheet sand microfacies, however, because of some factors leading to unstable deposition, such as terrain slope relief and frequent lake level change, sand distribution of braided river delta is relatively wider and thinner. Sedimentation of Lake face is mainly composed of the depositon of shore-shallow lake and deep lake. Shore-shallow lake is characterized with thin sand mud interbed, with bio-drilling construction; Deep lake and semi- deep lake have the feature of a large section of dark gray, black shale or of the argillaceous sandstone
Shiwu Oilfield in Lishu fault depression, controled by multi-source, developed several sedimentary types. And in each deposition period, Provenance Systems and Sedimentary Characteristics have the strong inheritance, forming a sedimentation pattern of mixed-source deposition, differences in sources, development with inheritance.
十屋油田营城组沉积时期盆地内发育有多个物源体系,本文通过聚类分析法、碎屑颗粒组分法、重矿物法、砂砾岩百分含量分布法和地层倾角测井法等方法对十屋油田营城组物源体系进行了综合分析,认为研究区在营城组沉积时期存在有三大物源体系,分别是西北方向的西北物源区、北部斜坡物源区和东部斜坡物源区。三个物源体系在营城组各时期继承发育,其中西北部物源区母岩类型以沉积岩和岩浆岩为主;北部斜坡物源区母岩类型以岩浆岩为主;东部斜坡物源区母岩类型以岩浆岩和变质岩为主。
十屋油田营城组时期主要发育了扇三角洲、辫状河三角洲和湖泊等沉积体系类型。营五段沉积时期,三个物源体系均在研究区形成扇三角洲沉积;营四段沉积时期,西北和北部物源体系仍然发育扇三角洲沉积,但扇三角洲范围较营五段时期有所减小,而东部物源体系仍为辫状河三角洲沉积;营三段到营一段沉积时期,三个物源体系均形成辫状河三角洲沉积,形成研究区的混源沉积特征。梨树断陷十屋油田营城组各沉积时期物源体系和沉积体系特征继承性较强,形成了该区“多物源混源沉积、各物源源间存异、各时期继承发育”的沉积格局。十屋油田营城组发育的扇三角洲是缓坡背景下发育的粗碎屑三角洲,发育有扇三角洲平原、前缘和前扇三角洲等亚相,水下分流河道、河口坝和席状砂等砂体构成扇三角洲的骨架砂体,兼具重力流沉积(泥石流)和牵引流沉积特征;研究区发育的辫状河三角洲沉积物粒度细于扇三角洲,也发育有辫状河三角洲平原、前缘和辫状河前三角洲,不发育重力流沉积;湖泊相主要发育滨浅湖和深湖-半深湖相沉积,滨浅湖以薄层砂岩与泥岩互层为特征,发育有生物钻孔构造;深湖-半深湖以大套灰黑色、黑色泥岩或夹薄层泥质砂岩为特征。
十屋油田营城组储层属低孔低渗储层,储集空间由原生孔隙、次生溶解孔隙和裂缝构成。并认为研究区储层物性主要受沉积作用的控制,以扇三角洲沉积相的储层物性最好,辫状河三角洲次之,扇三角洲中的泥石流沉积储层物性最差。
Shiwu Oilfield in Lishu fault Depression, located in the southeast of Songliao basin, has developed into a composite basin of fault depression superposition since Late Jurassic. And Shiwu Oilfield, in the center of the basin, is one of the richest oil and gas zone. In this paper, on the basis of core, logging, and a lot of analysis data, using sedimentary theories and methods as a guide, combined with mathematic theory of statistics, conducts a study of provenance Systems and sedimentary characteristics of Yingcheng Formation in Shiwu Oilfield.
Through the methods of cluster analysis, clastic particles component, heavy minerals, the percentages of glutenite and dipmeter, carrying out a comprehensive analysis of provenance systems of Yingcheng Formation with the character of multi-source deposition in Shiwu Oilfield leads to a perspective that there are three depositional source systems, which are North Slope provenance, east Slope provenance and northwest provenance. And rock type is mainly igneous rock in the North Slope source Area. Rock types of the eastern slope source area are mainly magmatic rocks and metamorphic rocks. In Northwest source area rock types are mainly sedimentary and igneous rocks.Clastic grains from three directions gather in the study area, where the distribution extent of sediments from north slope and northwest are borader.
In this study area, it mainly developed fan delta, braided river delta and lake sedimentary system types: fan delta forming in the early sedimentary period of Yingcheng Formation, distributing in the northern part and the eastern slope of the basin, is made up of sand bodies such as underwater distributary channel, mouth bar and sheet sand, which are current deposits and gravity flow deposits like mud flow. Braided river delta developing in the whole basin in the mid and late of the Yingcheng Formation, also has distributary channel and mouth bar and sheet sand microfacies, however, because of some factors leading to unstable deposition, such as terrain slope relief and frequent lake level change, sand distribution of braided river delta is relatively wider and thinner. Sedimentation of Lake face is mainly composed of the depositon of shore-shallow lake and deep lake. Shore-shallow lake is characterized with thin sand mud interbed, with bio-drilling construction; Deep lake and semi- deep lake have the feature of a large section of dark gray, black shale or of the argillaceous sandstone
Shiwu Oilfield in Lishu fault depression, controled by multi-source, developed several sedimentary types. And in each deposition period, Provenance Systems and Sedimentary Characteristics have the strong inheritance, forming a sedimentation pattern of mixed-source deposition, differences in sources, development with inheritance.
引文
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