Advanced Search

WANG Feng, WANG Duo-yun, GAO Ming-shu, YAO Yong-chao, WANG Zhi-kun, LI Shu-tong, QIN Hong. The Microfacies Combination and Character istics of Delta Front in Yanchang Formation (Triassic) of Jiyuan Area Shaanxi-Gansu-Ningxia Basin[J]. Acta Sedimentologica Sinica, 2005, 23(2): 218-224.
Citation: WANG Feng, WANG Duo-yun, GAO Ming-shu, YAO Yong-chao, WANG Zhi-kun, LI Shu-tong, QIN Hong. The Microfacies Combination and Character istics of Delta Front in Yanchang Formation (Triassic) of Jiyuan Area Shaanxi-Gansu-Ningxia Basin[J]. Acta Sedimentologica Sinica, 2005, 23(2): 218-224.

The Microfacies Combination and Character istics of Delta Front in Yanchang Formation (Triassic) of Jiyuan Area Shaanxi-Gansu-Ningxia Basin

  • Received Date: 2004-02-26
  • Rev Recd Date: 2004-05-29
  • Publish Date: 2005-06-10
  • A series of gentle slope delta are developed in Yanchang Formation in Jiyuan Area of Shaanxi-Gansu-Ningxia Basin. The delta front in this area can be divided into mesa delta front and slop ing delta front. The deposition models of delta along gentle slop are proposed based on the strength of the current in distributary channel and the depth of water in the lake. According to the research of underwater distributary channel, recombination bars and mouth bar, we can establish the assorted scheme and discriminating characteristics. For example, the distributary channels are composed of truncated underwater distributary channels and underwater superposition channels. The rivermouth bars are composed of the integrated mouth bars and recombination bars. The recombination bars consist of mouse bars at the bottom and underwater distributary channels at the top, and it can be subdivide into up side deformity recombination bars, integral recombination bars and downside recombination bars. This type of compartmentation scheme can be helpful to identify and distributing prognosticate of high quality reservoir, and it can also serve to subdivide the flow unit in oil exploitation.
  • [1] 1 吴崇筠,薛叔浩. 中国含油气盆地沉积学[M].北京:石油工业出版社,1992.48-56.

    2 Frideman G M,Sanders J E. Principles of Sedimentology[M].New York:John Wiley & Sons,1978.5-121.

    3 Haszeldine R S. Muddy deltas in freshwater lake, and tectonism in the Upper Carboniferous coalfield of NE England[J].Sedimentology,1984,(06):811-822.

    4 梅志超. 湖泊三角洲的地层模式和骨架砂体的特征[J].沉积学报,1991,(04):1-8.

    5 何义中,郑荣才,吴朝容. 湖泊三角洲研究的回顾与展望[J].岩相古地理,1999,(03):40-41.

    6 杨俊杰. 鄂尔多斯盆地构造演化与油气分布规律[M].北京:石油工业出版社,2002.104-108.

    7 马正. 应用自然电位测井曲线解释沉积环境[J].石油与天然气地质,1982,(01):25-40.

    8 薛叔浩. 湖盆沉积地质与油气勘探[M].北京:石油工业出版社,2002.221-230.

    9 陈钟惠. 煤和含煤岩系的沉积环境[M].武汉:中国地质大学出版社,1988.102-106.

    10 梅志超. 沉积相与古地理重建[M].西安:西北大学出版社,1994.86-95.

    11 周丽清,吴胜和,熊琦华. 吐哈盆地WM油田辫状河三角洲前缘砂体分析[J].沉积学报,2000,(02):248-252.

    12 李凤杰,王多云,郑希民. 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,(04):582-586.

    13 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:柴达木盆地阿尔金山前西段干柴沟组[J].沉积学报,1991,(04):43-48.

    14 李凤杰,王多云,宋广寿. 陕甘宁盆地坳陷型湖盆缓坡带三角洲前缘短期基准面旋回与储层成因分析[J].沉积学报,2004,(01):75-76.
  • 加载中
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(620) PDF downloads(924) Cited by()

Proportional views
Related
Publishing history
  • Received:  2004-02-26
  • Revised:  2004-05-29
  • Published:  2005-06-10

The Microfacies Combination and Character istics of Delta Front in Yanchang Formation (Triassic) of Jiyuan Area Shaanxi-Gansu-Ningxia Basin

Abstract: A series of gentle slope delta are developed in Yanchang Formation in Jiyuan Area of Shaanxi-Gansu-Ningxia Basin. The delta front in this area can be divided into mesa delta front and slop ing delta front. The deposition models of delta along gentle slop are proposed based on the strength of the current in distributary channel and the depth of water in the lake. According to the research of underwater distributary channel, recombination bars and mouth bar, we can establish the assorted scheme and discriminating characteristics. For example, the distributary channels are composed of truncated underwater distributary channels and underwater superposition channels. The rivermouth bars are composed of the integrated mouth bars and recombination bars. The recombination bars consist of mouse bars at the bottom and underwater distributary channels at the top, and it can be subdivide into up side deformity recombination bars, integral recombination bars and downside recombination bars. This type of compartmentation scheme can be helpful to identify and distributing prognosticate of high quality reservoir, and it can also serve to subdivide the flow unit in oil exploitation.

WANG Feng, WANG Duo-yun, GAO Ming-shu, YAO Yong-chao, WANG Zhi-kun, LI Shu-tong, QIN Hong. The Microfacies Combination and Character istics of Delta Front in Yanchang Formation (Triassic) of Jiyuan Area Shaanxi-Gansu-Ningxia Basin[J]. Acta Sedimentologica Sinica, 2005, 23(2): 218-224.
Citation: WANG Feng, WANG Duo-yun, GAO Ming-shu, YAO Yong-chao, WANG Zhi-kun, LI Shu-tong, QIN Hong. The Microfacies Combination and Character istics of Delta Front in Yanchang Formation (Triassic) of Jiyuan Area Shaanxi-Gansu-Ningxia Basin[J]. Acta Sedimentologica Sinica, 2005, 23(2): 218-224.
Reference (1)

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return