Advanced Search

SHAN JingFu, ZHANG Bin, ZHAO ZhongJun, LI FuPing, WANG Hui, WANG Bo. Single Stage and Sedimentary Evolution Process Analysis of Braided River: A Case from SuX block of western Sulige gas field in Ordos Basin[J]. Acta Sedimentologica Sinica, 2015, 33(4): 773-785. doi: 10.14027/j.cnki.cjxb.2015.04.016
Citation: SHAN JingFu, ZHANG Bin, ZHAO ZhongJun, LI FuPing, WANG Hui, WANG Bo. Single Stage and Sedimentary Evolution Process Analysis of Braided River: A Case from SuX block of western Sulige gas field in Ordos Basin[J]. Acta Sedimentologica Sinica, 2015, 33(4): 773-785. doi: 10.14027/j.cnki.cjxb.2015.04.016

Single Stage and Sedimentary Evolution Process Analysis of Braided River: A Case from SuX block of western Sulige gas field in Ordos Basin

doi: 10.14027/j.cnki.cjxb.2015.04.016
  • Received Date: 2014-07-09
  • Rev Recd Date: 2014-10-12
  • Publish Date: 2015-08-10
  • Currently, Sulige gas field is in increasing production stage, the reservoir of He8 remember in Permian are more and more complex with the rolling exploration in progresses. Originally one well drilled into a thick channel sandbody, but the one of neighboring well was instead of inter-channel mudstone. The characteristics of fast facies transition have brought great challenges for large-scale implementation of horizontal wells. In fact, the main reason is that the overlay rules of sandbody are not clear. The reason of sandbody was not single stage, but multi-stage. The multi-causes, multi-stage and criss-cross stacked channel sandbodies in space were the main reasons which took shape the huge thick braided river sandbody. The center often is made of multi-stage channel sandbodies.
    The Suxi block in Sulige gas field has been researched by predecessors who concluded that He8 member mianly developed braided river, and the result has been achieved wide recognition. The target bed thickness generally is 15~20 m. The study area located between the southeastern Su48 block and he northeastern Su47 block whose area is about 627 km2. The core and drilling well data can not only show the underwater deposition, but also no obvious delta front sedimentary, and the lower He82 sub-member mainly developed braided river deposits. The division time of stage is actually a part of the reservoir configuration. According to the previous configuration theory, braided river reservoir architecture can be divided into four levels (composite channel, single channel, channel bar, hyperplasia body), this study belong to the second level. The braided river of sedimentary micro-facies belongs to level, therefore, the identification of single stage river, compound, and sedimentary evolution analysis from composite channels can been researched based on the result of sedimentary micro-facies.
    It is always the emphasis and difficulty of single stage fluvial sandbodies from composite braided riveway in reservoir architecture. Especially, it is the most difficult at the aspect of single stage identification and combinations from multi-stage stacked sandbodies, and the evolution of sedimentary braided river was finished. In the process of the research, the complex river stages were divided through continuous cores verification and “single stage calibration method based on removal compaction effects”, the riverways had been reset by “relaxation rebound techniques” based on removal compaction effects. The single stage riverway were tracked and compared after using “the sand thickness center line connecting method” based on modern sedimentary and geological models and theories, then, the results were confirmed by interference well testing which can confirm that the time of stage redefinition and the predicted results were reliable. Based on above the evolution and sedimentary history was researched according to the order of sedimentary development. The research result show that these research methods will help to reveal stacked sands, improve the rate of sand drilling, and it is also convenient to carry out large-scale deployment and post-horizontal well geosteering operations and to provide a theoretical basis so on for oil production practice simultaneously.
  • Created with Highcharts 5.0.7Amount of accessChart context menuAbstract Views, HTML Views, PDF Downloads StatisticsAbstract ViewsHTML ViewsPDF Downloads2024-052024-062024-072024-082024-092024-102024-112024-122025-012025-022025-032025-0400.250.50.7511.25
    Created with Highcharts 5.0.7Chart context menuAccess Class DistributionFULLTEXT: 5.6 %FULLTEXT: 5.6 %META: 70.0 %META: 70.0 %PDF: 24.4 %PDF: 24.4 %FULLTEXTMETAPDF
    Created with Highcharts 5.0.7Chart context menuAccess Area Distribution其他: 3.6 %其他: 3.6 %其他: 2.0 %其他: 2.0 %Chandler: 0.4 %Chandler: 0.4 %China: 2.4 %China: 2.4 %United States: 2.4 %United States: 2.4 %[]: 1.6 %[]: 1.6 %上海: 3.2 %上海: 3.2 %东莞: 0.4 %东莞: 0.4 %临汾: 0.4 %临汾: 0.4 %乌鲁木齐: 0.8 %乌鲁木齐: 0.8 %伊犁: 0.4 %伊犁: 0.4 %克拉玛依: 2.0 %克拉玛依: 2.0 %兰州: 2.0 %兰州: 2.0 %兰州市城关区: 0.4 %兰州市城关区: 0.4 %凉山: 0.4 %凉山: 0.4 %北京: 16.0 %北京: 16.0 %十堰: 0.4 %十堰: 0.4 %南京: 0.4 %南京: 0.4 %台州: 0.4 %台州: 0.4 %合肥: 0.8 %合肥: 0.8 %哥伦布: 0.4 %哥伦布: 0.4 %城南: 0.4 %城南: 0.4 %大庆: 0.4 %大庆: 0.4 %天津: 3.2 %天津: 3.2 %太原: 0.4 %太原: 0.4 %巴音郭楞: 0.8 %巴音郭楞: 0.8 %常州: 0.4 %常州: 0.4 %张家口: 2.4 %张家口: 2.4 %成都: 2.0 %成都: 2.0 %扬州: 1.2 %扬州: 1.2 %杭州: 0.8 %杭州: 0.8 %武汉: 1.2 %武汉: 1.2 %海口: 0.4 %海口: 0.4 %深圳: 2.0 %深圳: 2.0 %湛江: 0.4 %湛江: 0.4 %滨州: 0.8 %滨州: 0.8 %漯河: 0.4 %漯河: 0.4 %盘锦: 1.6 %盘锦: 1.6 %芒廷维尤: 7.6 %芒廷维尤: 7.6 %苏州: 0.8 %苏州: 0.8 %衢州: 0.8 %衢州: 0.8 %襄阳: 0.4 %襄阳: 0.4 %西宁: 24.0 %西宁: 24.0 %西安: 3.6 %西安: 3.6 %贵阳: 0.4 %贵阳: 0.4 %运城: 0.4 %运城: 0.4 %运城市盐湖区: 0.4 %运城市盐湖区: 0.4 %郑州: 0.8 %郑州: 0.8 %长沙: 1.2 %长沙: 1.2 %其他其他ChandlerChinaUnited States[]上海东莞临汾乌鲁木齐伊犁克拉玛依兰州兰州市城关区凉山北京十堰南京台州合肥哥伦布城南大庆天津太原巴音郭楞常州张家口成都扬州杭州武汉海口深圳湛江滨州漯河盘锦芒廷维尤苏州衢州襄阳西宁西安贵阳运城运城市盐湖区郑州长沙
  • Cited by

    Periodical cited type(15)

    1. 翟羽佳,马君霞,马旭,杨洋,张润. 基于辫状河储层特征控制的地震反演砂体刻画——以苏里格气田盒_(8下)段为例. 沉积学报. 2024(05): 1711-1722 . 本站查看
    2. 龙盛芳,王玉善,李国良,段传丽,邵映明,何咏梅,陈凌云,焦煦. 苏里格气田苏49区块盒8下亚段致密储层非均质性特征. 岩性油气藏. 2021(02): 59-69 .
    3. 秦国省,吴文丽,秦国利,刘臻,杨超. 东营凹陷沙三中亚段沉积特征及复合砂体沉积过程——以牛庄洼陷南坡为例. 科学技术与工程. 2021(14): 5767-5776 .
    4. 李柱正,李开建,李波,王家辉,钟金银,王海峰,姚武君. 辫状河砂岩储层内部结构解剖方法及其应用——以鄂尔多斯盆地苏里格气田为例. 天然气工业. 2020(04): 30-39 .
    5. 袁纯,张惠良,王波. 大型辫状河三角洲砂体构型与储层特征——以库车坳陷北部阿合组为例. 岩性油气藏. 2020(06): 73-84 .
    6. 周连敏,何书梅,赵郁文,宋舜尧,刘天鹤,王晶晶. 复合曲流河道内的单河道识别. 石油地球物理勘探. 2019(01): 175-181+11-12 .
    7. 邹拓,王永凯,田昀,陈璞,杨宇华,冯国杰. 单一辫流带内部构型单元解析. 录井工程. 2019(02): 116-121+138 .
    8. 王文胜,兰义飞,史红然,田清华,张志刚,薛雯. 基于砂地比的复合河道沉积期次空间解析方法——以鄂尔多斯盆地苏里格气田ST密井网试验区盒8~(下(2))为例. 石油与天然气地质. 2019(05): 1135-1140 .
    9. 王文胜,黄文芳,何光怀,孙艳辉,单敬福. 辫状河内部辫流水道识别与充填结构分析. 科技通报. 2019(08): 39-45 .
    10. 马志欣,范倩倩,孙艳辉,何光怀,单敬福. 辫状河河道砂体内部构型表征方法与层次结构解析. 科技通报. 2019(10): 26-32 .
    11. 卢志远,马世忠,何宇,李杭,何伟,李智阳. 复合砂体内部单河道划分及沉积演化——以苏东27-36密井网区为例. 石油地质与工程. 2018(04): 18-22+123 .
    12. 毛平. 砂质辫状河储集层构型表征研究现状及展望. 新疆石油地质. 2018(04): 492-500 .
    13. 崔连可,单敬福,李浮萍,崔璐,种健. 基于稀疏井网条件下的古辫状河道心滩砂体估算——以苏里格气田苏X区块为例. 岩性油气藏. 2018(01): 155-164 .
    14. 秦国省,邹存友,赵亮,秦国利,吴文丽. 基于沉积过程的储层表征研究进展及发展趋势. 科学技术与工程. 2017(30): 110-120 .
    15. 种健,崔连可. 苏里格气田苏X区块山西组山11亚段沉积相研究. 中国锰业. 2017(01): 62-65+84 .

    Other cited types(16)

通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Article Metrics

Article views(706) PDF downloads(647) Cited by(31)

Proportional views
Related
Publishing history
  • Received:  2014-07-09
  • Revised:  2014-10-12
  • Published:  2015-08-10

Single Stage and Sedimentary Evolution Process Analysis of Braided River: A Case from SuX block of western Sulige gas field in Ordos Basin

doi: 10.14027/j.cnki.cjxb.2015.04.016

Abstract: Currently, Sulige gas field is in increasing production stage, the reservoir of He8 remember in Permian are more and more complex with the rolling exploration in progresses. Originally one well drilled into a thick channel sandbody, but the one of neighboring well was instead of inter-channel mudstone. The characteristics of fast facies transition have brought great challenges for large-scale implementation of horizontal wells. In fact, the main reason is that the overlay rules of sandbody are not clear. The reason of sandbody was not single stage, but multi-stage. The multi-causes, multi-stage and criss-cross stacked channel sandbodies in space were the main reasons which took shape the huge thick braided river sandbody. The center often is made of multi-stage channel sandbodies.
The Suxi block in Sulige gas field has been researched by predecessors who concluded that He8 member mianly developed braided river, and the result has been achieved wide recognition. The target bed thickness generally is 15~20 m. The study area located between the southeastern Su48 block and he northeastern Su47 block whose area is about 627 km2. The core and drilling well data can not only show the underwater deposition, but also no obvious delta front sedimentary, and the lower He82 sub-member mainly developed braided river deposits. The division time of stage is actually a part of the reservoir configuration. According to the previous configuration theory, braided river reservoir architecture can be divided into four levels (composite channel, single channel, channel bar, hyperplasia body), this study belong to the second level. The braided river of sedimentary micro-facies belongs to level, therefore, the identification of single stage river, compound, and sedimentary evolution analysis from composite channels can been researched based on the result of sedimentary micro-facies.
It is always the emphasis and difficulty of single stage fluvial sandbodies from composite braided riveway in reservoir architecture. Especially, it is the most difficult at the aspect of single stage identification and combinations from multi-stage stacked sandbodies, and the evolution of sedimentary braided river was finished. In the process of the research, the complex river stages were divided through continuous cores verification and “single stage calibration method based on removal compaction effects”, the riverways had been reset by “relaxation rebound techniques” based on removal compaction effects. The single stage riverway were tracked and compared after using “the sand thickness center line connecting method” based on modern sedimentary and geological models and theories, then, the results were confirmed by interference well testing which can confirm that the time of stage redefinition and the predicted results were reliable. Based on above the evolution and sedimentary history was researched according to the order of sedimentary development. The research result show that these research methods will help to reveal stacked sands, improve the rate of sand drilling, and it is also convenient to carry out large-scale deployment and post-horizontal well geosteering operations and to provide a theoretical basis so on for oil production practice simultaneously.

SHAN JingFu, ZHANG Bin, ZHAO ZhongJun, LI FuPing, WANG Hui, WANG Bo. Single Stage and Sedimentary Evolution Process Analysis of Braided River: A Case from SuX block of western Sulige gas field in Ordos Basin[J]. Acta Sedimentologica Sinica, 2015, 33(4): 773-785. doi: 10.14027/j.cnki.cjxb.2015.04.016
Citation: SHAN JingFu, ZHANG Bin, ZHAO ZhongJun, LI FuPing, WANG Hui, WANG Bo. Single Stage and Sedimentary Evolution Process Analysis of Braided River: A Case from SuX block of western Sulige gas field in Ordos Basin[J]. Acta Sedimentologica Sinica, 2015, 33(4): 773-785. doi: 10.14027/j.cnki.cjxb.2015.04.016

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return