松辽盆地北部他拉哈—英台—大安地区黑帝庙油层精细地层研究
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摘要
本项研究综合采用层序地层学、沉积学的最新理论和方法，运用地震、测井、录井、岩心等分析资料，对松辽盆地北部他拉哈-英台-大安地区黑帝庙油层的层序地层格架、沉积相进行了深入细致的分析和研究，并对有利储层及岩性圈闭进行了初步分析和预测。
研究区位于松辽盆地北部他拉哈—英台—大安地区，构造上位于大庆长垣以西古龙凹陷和龙虎泡大安阶地毗邻地区。按传统地层分层，研究层段包括嫩江组一、二、三段。从层序地层学的观点来看，这是一个完整的三级层序。
根据地震、综合录井、测井、岩心等资料，依据井间可对比的原则，研究层段的三级层序划分为三个四级层序。层序界面上便是湖进体系域，湖进体系域顶界为最大湖泛面，在岩性上表现为区域上广泛分布的油页岩段。高位域为深湖、半深湖沉积，岩性上主要为泥岩，有时可以出现进积或加积的砂体，大致相当于嫩二段。湖退体系域大致相当于嫩三段，其上部界面为沉积转换面，即由进积到加积的转换面，下部界面为湖泛面。
本文重点探讨这个三级层序的湖退体系域。依据层序地层叠加样式，湖退体系域可划分为3个准层序组，9个准层序，即上部准层序组、中部准层序组和下部准层序组，分别大致相当于已习惯应用的黑帝庙第二油层组上部的H_2~1，中部的H_2~2和下部的H_2~3。在此基础上，对各个准层序进行了沉积相和砂体特征的研究。把砂体展布特征和构造特征加以叠合，以此进行有利储层和圈闭的分析和预测。
研究区内收缩体系域共发现圈闭31个，其中构造圈闭10个，岩性圈闭16个，复合圈闭5个。31个圈闭中有20个圈闭经钻探、测试或试油已获工业油流，已经形成具有工业价值的油气藏。其中，其中最有利圈闭4个，有利圈闭13个，较有利圈闭14个。
The latest theory and method of sequence stratigraphy and sedimentology are adopted in this paper. By using the data of seism, well logging, mud well logging and cores, the framework of sequence strata and sedimentary facies in the areas of Talaha-Yingtai-Da'an in the north of Song-Liao basin are analyzed and studied deeply, also the favorable reservoir and lithologic traps are researched and forecasted primarily.
The studied area locates in Talaha-Yingtai-Da'an in the north of Song-Liao basin, and the tectonic location is in the Gulong depression and Longhupao-Da'an terrace in the west of Daqing placanticline. According to the traditional methods, the studied area can be divided into three parts. It is a whole third hierarchy sequence.
According to the data of seism, mud well logging, well logging, cores and the principles of well correlation, this third hierarchy sequence is divided into three fourth-hierarchy sequences. The bottom sequence boundary is the lacustrine transgressional system tract, and the top boundary of the lacustrine transgression system tract is the maximum lacustrine flooding surface. The lithology is albert shale distributing in the whole basin. Highstand system tract is deep lake and half-deep lake sediment. The lithology is mud stone. Sometimes the sandbody of transgression and accretion can be found, equals to N2. the lacustrine retrogradational system tract equals to N3, and its upper is conversion surface , that is the surface from transgression to accretion. The bottom is lacustrine flooding surface.
This paper gives emphasis to lacustrine retrogradational system tract of the third hierarchy sequence. According to the stacking patterns, the lacustrine retrogradational system tract is partitioned into three parasequence sets and nine parasequences, that is upper parasequence middle parasequence and bottom parasequence, equal to H2' , H22 and H23. Basing on these, the sediment faces and sandbody characteristics of each parasequence are studied, overlapping sandbody distribution structural characteristics, then the favorable reservoirs and traps are analysed and forecasted.
Thirty one traps are found in the shrinking system tracks, including 10 tectonic traps 16 lithology traps and 5 combination traps. 20 traps of the 31 are drilled or found industry oil stream and form commercial pools, including 4 best traps, 13 better traps, 14 good traps.
研究区位于松辽盆地北部他拉哈—英台—大安地区，构造上位于大庆长垣以西古龙凹陷和龙虎泡大安阶地毗邻地区。按传统地层分层，研究层段包括嫩江组一、二、三段。从层序地层学的观点来看，这是一个完整的三级层序。
根据地震、综合录井、测井、岩心等资料，依据井间可对比的原则，研究层段的三级层序划分为三个四级层序。层序界面上便是湖进体系域，湖进体系域顶界为最大湖泛面，在岩性上表现为区域上广泛分布的油页岩段。高位域为深湖、半深湖沉积，岩性上主要为泥岩，有时可以出现进积或加积的砂体，大致相当于嫩二段。湖退体系域大致相当于嫩三段，其上部界面为沉积转换面，即由进积到加积的转换面，下部界面为湖泛面。
本文重点探讨这个三级层序的湖退体系域。依据层序地层叠加样式，湖退体系域可划分为3个准层序组，9个准层序，即上部准层序组、中部准层序组和下部准层序组，分别大致相当于已习惯应用的黑帝庙第二油层组上部的H_2~1，中部的H_2~2和下部的H_2~3。在此基础上，对各个准层序进行了沉积相和砂体特征的研究。把砂体展布特征和构造特征加以叠合，以此进行有利储层和圈闭的分析和预测。
研究区内收缩体系域共发现圈闭31个，其中构造圈闭10个，岩性圈闭16个，复合圈闭5个。31个圈闭中有20个圈闭经钻探、测试或试油已获工业油流，已经形成具有工业价值的油气藏。其中，其中最有利圈闭4个，有利圈闭13个，较有利圈闭14个。
The latest theory and method of sequence stratigraphy and sedimentology are adopted in this paper. By using the data of seism, well logging, mud well logging and cores, the framework of sequence strata and sedimentary facies in the areas of Talaha-Yingtai-Da'an in the north of Song-Liao basin are analyzed and studied deeply, also the favorable reservoir and lithologic traps are researched and forecasted primarily.
The studied area locates in Talaha-Yingtai-Da'an in the north of Song-Liao basin, and the tectonic location is in the Gulong depression and Longhupao-Da'an terrace in the west of Daqing placanticline. According to the traditional methods, the studied area can be divided into three parts. It is a whole third hierarchy sequence.
According to the data of seism, mud well logging, well logging, cores and the principles of well correlation, this third hierarchy sequence is divided into three fourth-hierarchy sequences. The bottom sequence boundary is the lacustrine transgressional system tract, and the top boundary of the lacustrine transgression system tract is the maximum lacustrine flooding surface. The lithology is albert shale distributing in the whole basin. Highstand system tract is deep lake and half-deep lake sediment. The lithology is mud stone. Sometimes the sandbody of transgression and accretion can be found, equals to N2. the lacustrine retrogradational system tract equals to N3, and its upper is conversion surface , that is the surface from transgression to accretion. The bottom is lacustrine flooding surface.
This paper gives emphasis to lacustrine retrogradational system tract of the third hierarchy sequence. According to the stacking patterns, the lacustrine retrogradational system tract is partitioned into three parasequence sets and nine parasequences, that is upper parasequence middle parasequence and bottom parasequence, equal to H2' , H22 and H23. Basing on these, the sediment faces and sandbody characteristics of each parasequence are studied, overlapping sandbody distribution structural characteristics, then the favorable reservoirs and traps are analysed and forecasted.
Thirty one traps are found in the shrinking system tracks, including 10 tectonic traps 16 lithology traps and 5 combination traps. 20 traps of the 31 are drilled or found industry oil stream and form commercial pools, including 4 best traps, 13 better traps, 14 good traps.
引文
[1] 马力．论松辽盆地的演化和构造格局对沉积建造的控制．北京：石油工业出版社，1985．7～13
[2] 高瑞祺、蔡希源著。松辽盆地油气田形成条件及分布规律。第一版。北京：石油工业出版社，1997．7～9
[3] 张明坤等．中国石油地质志，卷2第一版．北京：石油工业出版社，1993．402～409
[4] Vail P. R., Mitchum R. M., Todd R. G., etal. Seismic stratigraphy and global changes of sea level. In: Dayton C E, ed. Seismic stratigraphy-applications to hydrocarbon exploration. AAPG Memoir, 1977, (26)
[5] Van Wag0ner J. C., Mitchum R. M., Campion K. M., et al. Siliciclastic sequence stratigraphy in well logs, cores and outcrops: concepts for high-resohtion correlation of time and facies. AAPG Methods in Exploration Series, 1990, (7)
[6] 徐怀大 陆相层序地层学研究中的某些问题[J]．石油与天然气地质，1997．18(2)
[7] Posamentier H. W. Forced regressions in a sequence stratigraphic framework: concepts, examples, and exploration significance. America Association Petroleum Geology Belletin, 1992, 76(7)
[8] Van Wagoner J. C., Mitchum R. M., Campion K. M., et al. Siliciclastic sequence stratigraphy in well logs, cores and outcrops: concepts for high-resolution correlation of time and facies. AAPG Methods in Exploration Series, 1990. (7)
[9] Posamentier H. W. Forced regressions in a sequence stratigraphic framework: concepts, examples, and exploration significance. America Association Petroleum Geology Belletin, 1992. 76(7)
[10] Hunt et al. Stranded parasequences and the forced regressive wedge systems tract: deposition during base-level fall. Sedimentary Geology, 1992. 81(1)
[11] 任延广，杨玉峰。松辽盆地中浅层地层层序及沉积相研究．大庆勘探开发研究院，1999．9～10
[12] 张明学，胡玉双．层序地层学与油气，1999．60～84
[13] 顾家裕，邓宏文，朱筱敏主编 层序地层学及其在油气勘探开发中的应用[M] 北京：石油工业出版社，1997
[14] 张顺等。松辽盆地北部黑帝庙油层成藏条件与勘探目标优选研究．大庆勘探开发研究院，2003．4～15
[15] 熊继辉，王毅等著．层序地层学及其再塔里木盆地石炭系研究中的应用[M]．北京：石油工业出版社，1996
[16] 蔡希源，陈章明，王玉华，辛仁臣著．松辽两江地区石油地质分析[M]．北京：石油工业出版社，1999
[17] Van Wagoner J. C., Mitchum R. M., Campion K. M., et al. Siliciclastic sequence stratigraphy in well logs, cores and outcrops: concepts for high-resolution correlation of time and facies. AAPG Methods in Exploration Series, 1990. (7)
[18] 张万选，张厚福，曾洪流等著．陆相地震地层学[M]．山东：石油大学出版社，1993
[19] 贾爱林等著．湖盆沉积学新进展[C]．北京：石油工业出版社，1999．P109
[20] 邓宏文著．高分辨率层序地层学原理及应用[M]．北京：地质出版社，2002
[21] 刘震著．储层地震地层学[M]．北京：地质出版社，1997
[22] 刘志国．1999年度新增石油探明储量年报．大庆石油管理局内部资料，2000．6
[23] 刘平略．松辽盆地嫩江组三、四段元素分布与沉积环境．勘探开发研究院报告，1983．12
[24] 解习农，程守田等．陆相盆地幕式构造旋回与层序构成[J]．地球科学，1996．21 (1)：27～33
[25] 许文志．松辽盆地嫩江组三、四段沉积特征。大庆油田勘探开发研究院科研报告，1981．11
[26] 吴智勇，姜衍文．全球旋回地层学述评[J]．石油与天然气地质，1996．17 (1)：15～20
[27] 吴智勇．米兰柯维奇旋回及其年代地层意义[J]．地学杂志，1995．19 (2)：156～160
[28] 陈均亮，朱德丰，殷进垠等编．松辽盆地中浅层构造特征及形成机制研究．大庆油田勘探开发研究院科研报告，1999．11
[29] 陈兴壁．松辽盆地北部古龙地区黑地庙油气藏形成条件的几点认识．大庆油田勘探开发研究院科研报告，1983．12
[30] 张宏逵等译，Sangree．J．B．Vail．P．R 著．应用层序地层学[M]．东营：石油大学出版社，1990，17～27
[31] 张革，他拉哈—英台地区油气成藏条件及目标评价研究，大庆油田勘探开发研究院科研报告，2000，10
[32] 张惠．松辽盆地南部层特征及定量评价[M]．吉林油田内部资料，1985
[33] 韩殿杰，孙新波．松辽盆地下白垩统层序地层格架及油气勘探方向[J]，石油与天然气地质，1995，16 (4)：384～389
[34] 李思田，杨士荣等．论沉积盆地的等时地层格架和基本建造单元[J]．沉积学报，1992．10 (4)：11～21
[35] 杜宁平译，陈开远校，T．A．Cross著．译自Research report of the genetic stratigraphy research group, Department of Geology and Geological Engineering．Colorado School of Mine, 1994
[36] 周永柄．新站油田石油探明储量评价部署总体设计．大庆油田勘探开发研究院，1998
[37] 武法东，陈建渝等．东营凹陷第三纪层序地层各架及沉积体系类型[J]．现代地质，1998．12 (4)：559～565
[38] 姜衍文，朱忠德，肖传桃等．全息地层学——新的挑战[J]．石油与天然气地质，1995，16 (2)：110～118
[39] 胡受权．泌阳断陷陆相层序外部构型研究[J]．现代地质，1998．12 (4)：568～575
[40] 徐怀大，魏魁生，洪卫东等译．Cloetingh．S．板内应力：视海平面中三级周期的构造起因[A]．见：威尔格斯C．K．层序地学原理[C]．北京：石油工业出版社，1993．23～37
[41] 杨万里主编．松辽陆相盆地石油地质[M]，北京：石油工业出版社，1985
[42] 殷鸿福，童金南．层序地层界面与年代地层界线的关系[J]．科学通报，1995，40 (6)：539～541
[43] 贾爱林，穆龙新等．储层露头精细研究和露头现场实验室的建立[A]．见：吴因业，姚根顺，贾爱林等著．湖盆沉积学新进展[C]．北京：石油工业出版社，1999．51～56
[44] 贾爱林．综合野外露头研究、地下成图和随机模拟进行高分辨率沉积各架建模[A]．见：吴因业，姚根顺，贾爱林等著．湖盆沉积学新进展[C]．北京：石油工业出版社，1999．8～9
[45] 郭建华．高频湖平面升降旋回与等时储层对比[J]．地质论平，1998．44 (5)：529～534
[46] 高振中，罗顺社等．鄂尔多斯西缘奥陶纪海底扇沉积体系[J]．石油与天然气地质，1995．16 (2)：119～124
[47] Embry. A. F. Transgressive-regressive (T-R) sequence analysis of the Jurassic succession of the Sverdrup Basin, Canadian Arctic Archipieago, Can. J. Earth. Sci. 1993, 30:301～320
[48] Galloway. W. E. Genetic stratigraphic sequences in basin analysis I:architecture and genesis Of flooding-surface bounded depositional units. Bull. Amer. Assoc. Petrol. Geologists, 1989. 73: 125～142
[49] Haq. B. U. Hardenboi. J, Vail. P. R. Chronology of fluctuating sea leval since the Triassic. Science. 1987, 235: 1156～1167
[50] Johnson. J. G, Klapper. G, Sandberg. C. A. Devonian eustatic fluctuations in Euramerica,
Bull. Geol. Soc. America, 1985, 99:567～587
[51] Li. Y. Y. Lerche. I. Perlmutter. M. A. Global stratigraphy:a model of carbonate growth patterns. Marine and Petroleum Geology, 1993.10: 620～631
[53] Sloos. L. L. Sequence in the cratonic interior of North America. Geological Societyof America Bulletin, 1963, 74: 93～114
[54] T. A. Cross. Controls on coal distribution in transgressive-regressive cyc;es, Upper Cretaceous, Western Interior, U. S. A.. In: C. K. Wilgaus. et al. Sea-level changes:An integrated approach. SEPM Special Publication, 1998, 42, 371～380.
[55] Vail. P. R. Seismic stratigraphy interpretation using sequence stratigraphy. Part:seismic stratigraphy interpretation procedure. In:Bally A W, ed. Atlas of seismic stratigraphy. American Association of Petroleum Geologists, Studies in Geology. 1987, 27:1～10
[56] Wheeler. H. E. Baselevel, lithosphere surfsce and time-stratigraphy. Bull. Geol. Soc. America, 1964,75: 599～610
[2] 高瑞祺、蔡希源著。松辽盆地油气田形成条件及分布规律。第一版。北京：石油工业出版社，1997．7～9
[3] 张明坤等．中国石油地质志，卷2第一版．北京：石油工业出版社，1993．402～409
[4] Vail P. R., Mitchum R. M., Todd R. G., etal. Seismic stratigraphy and global changes of sea level. In: Dayton C E, ed. Seismic stratigraphy-applications to hydrocarbon exploration. AAPG Memoir, 1977, (26)
[5] Van Wag0ner J. C., Mitchum R. M., Campion K. M., et al. Siliciclastic sequence stratigraphy in well logs, cores and outcrops: concepts for high-resohtion correlation of time and facies. AAPG Methods in Exploration Series, 1990, (7)
[6] 徐怀大 陆相层序地层学研究中的某些问题[J]．石油与天然气地质，1997．18(2)
[7] Posamentier H. W. Forced regressions in a sequence stratigraphic framework: concepts, examples, and exploration significance. America Association Petroleum Geology Belletin, 1992, 76(7)
[8] Van Wagoner J. C., Mitchum R. M., Campion K. M., et al. Siliciclastic sequence stratigraphy in well logs, cores and outcrops: concepts for high-resolution correlation of time and facies. AAPG Methods in Exploration Series, 1990. (7)
[9] Posamentier H. W. Forced regressions in a sequence stratigraphic framework: concepts, examples, and exploration significance. America Association Petroleum Geology Belletin, 1992. 76(7)
[10] Hunt et al. Stranded parasequences and the forced regressive wedge systems tract: deposition during base-level fall. Sedimentary Geology, 1992. 81(1)
[11] 任延广，杨玉峰。松辽盆地中浅层地层层序及沉积相研究．大庆勘探开发研究院，1999．9～10
[12] 张明学，胡玉双．层序地层学与油气，1999．60～84
[13] 顾家裕，邓宏文，朱筱敏主编 层序地层学及其在油气勘探开发中的应用[M] 北京：石油工业出版社，1997
[14] 张顺等。松辽盆地北部黑帝庙油层成藏条件与勘探目标优选研究．大庆勘探开发研究院，2003．4～15
[15] 熊继辉，王毅等著．层序地层学及其再塔里木盆地石炭系研究中的应用[M]．北京：石油工业出版社，1996
[16] 蔡希源，陈章明，王玉华，辛仁臣著．松辽两江地区石油地质分析[M]．北京：石油工业出版社，1999
[17] Van Wagoner J. C., Mitchum R. M., Campion K. M., et al. Siliciclastic sequence stratigraphy in well logs, cores and outcrops: concepts for high-resolution correlation of time and facies. AAPG Methods in Exploration Series, 1990. (7)
[18] 张万选，张厚福，曾洪流等著．陆相地震地层学[M]．山东：石油大学出版社，1993
[19] 贾爱林等著．湖盆沉积学新进展[C]．北京：石油工业出版社，1999．P109
[20] 邓宏文著．高分辨率层序地层学原理及应用[M]．北京：地质出版社，2002
[21] 刘震著．储层地震地层学[M]．北京：地质出版社，1997
[22] 刘志国．1999年度新增石油探明储量年报．大庆石油管理局内部资料，2000．6
[23] 刘平略．松辽盆地嫩江组三、四段元素分布与沉积环境．勘探开发研究院报告，1983．12
[24] 解习农，程守田等．陆相盆地幕式构造旋回与层序构成[J]．地球科学，1996．21 (1)：27～33
[25] 许文志．松辽盆地嫩江组三、四段沉积特征。大庆油田勘探开发研究院科研报告，1981．11
[26] 吴智勇，姜衍文．全球旋回地层学述评[J]．石油与天然气地质，1996．17 (1)：15～20
[27] 吴智勇．米兰柯维奇旋回及其年代地层意义[J]．地学杂志，1995．19 (2)：156～160
[28] 陈均亮，朱德丰，殷进垠等编．松辽盆地中浅层构造特征及形成机制研究．大庆油田勘探开发研究院科研报告，1999．11
[29] 陈兴壁．松辽盆地北部古龙地区黑地庙油气藏形成条件的几点认识．大庆油田勘探开发研究院科研报告，1983．12
[30] 张宏逵等译，Sangree．J．B．Vail．P．R 著．应用层序地层学[M]．东营：石油大学出版社，1990，17～27
[31] 张革，他拉哈—英台地区油气成藏条件及目标评价研究，大庆油田勘探开发研究院科研报告，2000，10
[32] 张惠．松辽盆地南部层特征及定量评价[M]．吉林油田内部资料，1985
[33] 韩殿杰，孙新波．松辽盆地下白垩统层序地层格架及油气勘探方向[J]，石油与天然气地质，1995，16 (4)：384～389
[34] 李思田，杨士荣等．论沉积盆地的等时地层格架和基本建造单元[J]．沉积学报，1992．10 (4)：11～21
[35] 杜宁平译，陈开远校，T．A．Cross著．译自Research report of the genetic stratigraphy research group, Department of Geology and Geological Engineering．Colorado School of Mine, 1994
[36] 周永柄．新站油田石油探明储量评价部署总体设计．大庆油田勘探开发研究院，1998
[37] 武法东，陈建渝等．东营凹陷第三纪层序地层各架及沉积体系类型[J]．现代地质，1998．12 (4)：559～565
[38] 姜衍文，朱忠德，肖传桃等．全息地层学——新的挑战[J]．石油与天然气地质，1995，16 (2)：110～118
[39] 胡受权．泌阳断陷陆相层序外部构型研究[J]．现代地质，1998．12 (4)：568～575
[40] 徐怀大，魏魁生，洪卫东等译．Cloetingh．S．板内应力：视海平面中三级周期的构造起因[A]．见：威尔格斯C．K．层序地学原理[C]．北京：石油工业出版社，1993．23～37
[41] 杨万里主编．松辽陆相盆地石油地质[M]，北京：石油工业出版社，1985
[42] 殷鸿福，童金南．层序地层界面与年代地层界线的关系[J]．科学通报，1995，40 (6)：539～541
[43] 贾爱林，穆龙新等．储层露头精细研究和露头现场实验室的建立[A]．见：吴因业，姚根顺，贾爱林等著．湖盆沉积学新进展[C]．北京：石油工业出版社，1999．51～56
[44] 贾爱林．综合野外露头研究、地下成图和随机模拟进行高分辨率沉积各架建模[A]．见：吴因业，姚根顺，贾爱林等著．湖盆沉积学新进展[C]．北京：石油工业出版社，1999．8～9
[45] 郭建华．高频湖平面升降旋回与等时储层对比[J]．地质论平，1998．44 (5)：529～534
[46] 高振中，罗顺社等．鄂尔多斯西缘奥陶纪海底扇沉积体系[J]．石油与天然气地质，1995．16 (2)：119～124
[47] Embry. A. F. Transgressive-regressive (T-R) sequence analysis of the Jurassic succession of the Sverdrup Basin, Canadian Arctic Archipieago, Can. J. Earth. Sci. 1993, 30:301～320
[48] Galloway. W. E. Genetic stratigraphic sequences in basin analysis I:architecture and genesis Of flooding-surface bounded depositional units. Bull. Amer. Assoc. Petrol. Geologists, 1989. 73: 125～142
[49] Haq. B. U. Hardenboi. J, Vail. P. R. Chronology of fluctuating sea leval since the Triassic. Science. 1987, 235: 1156～1167
[50] Johnson. J. G, Klapper. G, Sandberg. C. A. Devonian eustatic fluctuations in Euramerica,
Bull. Geol. Soc. America, 1985, 99:567～587
[51] Li. Y. Y. Lerche. I. Perlmutter. M. A. Global stratigraphy:a model of carbonate growth patterns. Marine and Petroleum Geology, 1993.10: 620～631
[53] Sloos. L. L. Sequence in the cratonic interior of North America. Geological Societyof America Bulletin, 1963, 74: 93～114
[54] T. A. Cross. Controls on coal distribution in transgressive-regressive cyc;es, Upper Cretaceous, Western Interior, U. S. A.. In: C. K. Wilgaus. et al. Sea-level changes:An integrated approach. SEPM Special Publication, 1998, 42, 371～380.
[55] Vail. P. R. Seismic stratigraphy interpretation using sequence stratigraphy. Part:seismic stratigraphy interpretation procedure. In:Bally A W, ed. Atlas of seismic stratigraphy. American Association of Petroleum Geologists, Studies in Geology. 1987, 27:1～10
[56] Wheeler. H. E. Baselevel, lithosphere surfsce and time-stratigraphy. Bull. Geol. Soc. America, 1964,75: 599～610
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