2) Fuyu oil layer
扶余油层
1.
Hierarchical division and origin of single sand bodies in Fuyu oil layer,Fuyu Oilfield;
扶余油田扶余油层储集层单砂体划分及成因分析
2.
Sedimentary characteristics of Fuyu oil layer in Toutai area of Songliao basin;
松辽盆地头台地区扶余油层沉积特征
3.
Research on the delta deposits in Fuyu Oil Layer in east area Daqing Placanticline;
大庆长垣东部地区扶余油层三角洲沉积特征研究
3) Fuyu Reservoir
扶余油层
1.
Research on the Fuyu Reservoir Sandstone Diagenesis in South of Songliao Basin——Exempled by the Fuyu and Xinli Oilfields;
松辽盆地南部扶余油层砂岩成岩作用研究——以扶余油田和新立油田为例
2.
Reservoir Damage in Fuyu Reservoir in Chaganhu Area of Songliao Basin
松辽盆地查干湖地区扶余油层储层伤害分析
3.
The depositional facies of Fuyu reservoir in Changchunling anticlinal zone,Daqing Oil-Field is dominated by submerged distributary channel,interdistributary bay and sheet sand micro-facies in delta front sub-facies.
大庆油田长春岭背斜带扶余油层沉积微相类型主要是三角洲前缘亚相带内的水下分流河道微相、分流间湾微相和席状砂微相。
4) Fuyu Formation
扶余油层
1.
Reservoir-forming mechanism of low-permeability reservoir of Fuyu Formation in southern Songliao Basin;
松辽盆地南部扶余油层低渗透油藏形成机制
2.
Using the data of the cores, thin sections, granulometric analysis and well loggings, studying in details the features about the colors of the mudstone, the texture of the rock, sedimentary structures, sedimentary rhythm and the vertical sedimentary sequences, we conclude that the main facies of Fuyu formation are lake facies and shallow water lake delta facies in Toutai area.
利用岩心、薄片、粒度分析以及测井等资料，通过详细研究泥岩的颜色、岩石的结构、沉积构造、沉积韵律以及垂向沉积序列等特征，认为头台地区扶余油层主要发育有湖泊相和浅水湖泊三角洲相。
3.
The major oil pay zones in this area are formed by fluvial channel sandstones within the first and second layer of the Fuyu Formation.
主要产油层位为扶余油层一、二组,储层以河流相为主。
5) Fuyang reservoir
扶杨油层
1.
Prediction technique study for hydrocarbon-rich areas in low permeable oil field——case on Fuyang reservoir in Songliao Basin;
低渗透油田富集区预测技术研究——以松辽盆地扶杨油层为例(为《岩性油气藏》创刊而作)
2.
Characteristics of Diagenesis of Fuyang Reservoir in Yushulin Oilfield;
榆树林油田扶杨油层成岩作用特征
3.
Characters of fluid inclusions in the Fuyang reservoir, Qijia-Gulong area, Songliao Basin;
松辽盆地齐家—古龙地区扶杨油层流体包裹体特征
6) Fuyang oil layer
扶杨油层
1.
Reservoir characteristics of Fuyang oil layer in Q3 and Q4 Member in Daqing placanticline and area to its west;
大庆长垣及以西地区泉三、四段扶杨油层储层特征
2.
Characteristics of hydrocarbon migration in Fuyang oil layer in Daqing placanticline and its western area in Songliao Basin;
松辽盆地大庆长垣及其以西地区扶杨油层油气运移特征
3.
Seismic identification of channel sandbodies in the Fuyang oil layer in North Songliao Basin,China;
松辽盆地北部扶杨油层河道砂体的地震识别方法研究(英文)
补充资料：僧伽婆罗（梁扬都正观寺扶南沙门）《续高僧传》卷一
【僧伽婆罗（梁扬都正观寺扶南沙门）《续高僧传》卷一】
僧伽婆罗。梁言僧养。亦云僧铠。扶南国人也。幼而颖悟。早附法津。学年出家。偏业阿毗昙论。声荣之盛有誉海南。具足已后广习律藏。勇意观方乐崇开化。闻齐国弘法。随舶至都。住正观寺。为天竺沙门求那跋陀之弟子也。复从跋陀研精方等。未盈炎燠博涉多通。乃解数国书语。值齐历亡坠道教凌夷。婆罗静洁身心外绝交。故拥室栖闲养素资业。大梁御宇搜访术能。以天监五年。被敕征召于杨都寿光殿华林园正观寺占云馆扶南馆等五处传译讫十七年。都合一十一部。四十八卷。即大育王经。解脱道论等是也。初翻经日。于寿光殿武帝躬临法座笔受其文。然后乃付译人尽其经本。敕沙门宝唱慧超僧智法云及袁昙允等。相对疏出。华质有序不坠译宗。天子礼接甚厚。引为家僧。所司资给道俗改观。婆罗不畜私财。以为嚫施成立住寺。太尉临川王宏。接遇隆重。普通五年因疾卒于正观。春秋六十有五。梁初又有扶南沙门曼陀罗者。梁言弘弱。大赍梵本远来贡献。敕与婆罗共译宝云法界体性文殊般若经三部合一十一卷。虽事传译未善梁言。故所出经文多隐质。时有居士木道贤。以天监十五年献优娄频经一卷。文既鲜具。不辩来由。又有太学博士江泌女僧法者。小年出家有时静坐。闭目诵出净土妙庄严等经。始从八岁终于十六。总出三十五卷。天监年中在华光殿。亲对武帝诵出异经。杨都道俗咸称神授。若验佛经斯唯宿习未可余谈窃寻外典。生知者圣。学知者次。此则局谈今身昧于过往耳。若不然者。何以辨内外贤圣浅深之通塞哉。如前传昙谛之忆书镇。近俗崔子之念金环。代有斯踪。定非外托。逮太清中。湘东王记室虞孝敬。学周内外。撰内典传要三十卷。该罗经论。条贯释门。诸有要事备皆收录。颇同皇览类苑之流。渚宫陷没便袭染衣。更名道命。流离关辅亦有著述。云云。
僧伽婆罗。梁言僧养。亦云僧铠。扶南国人也。幼而颖悟。早附法津。学年出家。偏业阿毗昙论。声荣之盛有誉海南。具足已后广习律藏。勇意观方乐崇开化。闻齐国弘法。随舶至都。住正观寺。为天竺沙门求那跋陀之弟子也。复从跋陀研精方等。未盈炎燠博涉多通。乃解数国书语。值齐历亡坠道教凌夷。婆罗静洁身心外绝交。故拥室栖闲养素资业。大梁御宇搜访术能。以天监五年。被敕征召于杨都寿光殿华林园正观寺占云馆扶南馆等五处传译讫十七年。都合一十一部。四十八卷。即大育王经。解脱道论等是也。初翻经日。于寿光殿武帝躬临法座笔受其文。然后乃付译人尽其经本。敕沙门宝唱慧超僧智法云及袁昙允等。相对疏出。华质有序不坠译宗。天子礼接甚厚。引为家僧。所司资给道俗改观。婆罗不畜私财。以为嚫施成立住寺。太尉临川王宏。接遇隆重。普通五年因疾卒于正观。春秋六十有五。梁初又有扶南沙门曼陀罗者。梁言弘弱。大赍梵本远来贡献。敕与婆罗共译宝云法界体性文殊般若经三部合一十一卷。虽事传译未善梁言。故所出经文多隐质。时有居士木道贤。以天监十五年献优娄频经一卷。文既鲜具。不辩来由。又有太学博士江泌女僧法者。小年出家有时静坐。闭目诵出净土妙庄严等经。始从八岁终于十六。总出三十五卷。天监年中在华光殿。亲对武帝诵出异经。杨都道俗咸称神授。若验佛经斯唯宿习未可余谈窃寻外典。生知者圣。学知者次。此则局谈今身昧于过往耳。若不然者。何以辨内外贤圣浅深之通塞哉。如前传昙谛之忆书镇。近俗崔子之念金环。代有斯踪。定非外托。逮太清中。湘东王记室虞孝敬。学周内外。撰内典传要三十卷。该罗经论。条贯释门。诸有要事备皆收录。颇同皇览类苑之流。渚宫陷没便袭染衣。更名道命。流离关辅亦有著述。云云。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条