Quantitative prediction model for the depth limit of oil accumulation in the deep carbonate rocks: A case study of Lower Ordovician in Tazhong area of Tarim Basin

被引:3
|
作者
Wang, Wen -Yang [1 ]
Pang, Xiong-Qi [2 ,3 ]
Wang, Ya-Ping [3 ,4 ]
Chen, Zhang-Xin [5 ]
Jiang, Fu-Jie [2 ,3 ]
Chen, Ying [1 ,3 ]
机构
[1] Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
[2] China Univ Petr, State Key Lab Petr Resources & Prospecting, Beijing 102249, Peoples R China
[3] China Univ Petr, Coll Geosci, Beijing 102249, Peoples R China
[4] PetroChina Southwest Oil & Gas Field Co, Res Inst Explorat & Dev, Chengdu 610051, Sichuan, Peoples R China
[5] Univ Calgary, Schulich Sch Engn, Chem & Petr Engn, Calgary, AB T2N 1N4, Canada
基金
中国国家自然科学基金;
关键词
Deep layer; Tarim Basin; Hydrocarbon accumulation; Depth limit of oil accumulation; Prediction model; HYDROCARBON ACCUMULATION; SICHUAN BASIN; GAS; CRACKING; CHALLENGES; RESERVOIRS; PROGRESS; EXAMPLE; MARINE;
D O I
10.1016/j.petsci.2023.11.013
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
With continuous hydrocarbon exploration extending to deeper basins, the deepest industrial oil accumulation was discovered below 8,200 m, revealing a new exploration field. Hence, the extent to which oil exploration can be extended, and the prediction of the depth limit of oil accumulation (DLOA), are issues that have attracted significant attention in petroleum geology. Since it is difficult to characterize the evolution of the physical properties of the marine carbonate reservoir with burial depth, and the deepest drilling still cannot reach the DLOA. Hence, the DLOA cannot be predicted by directly establishing the relationship between the ratio of drilling to the dry layer and the depth. In this study, by establishing the relationships between the porosity and the depth and dry layer ratio of the carbonate reservoir, the relationships between the depth and dry layer ratio were obtained collectively. The depth corresponding to a dry layer ratio of 100% is the DLOA. Based on this, a quantitative prediction model for the DLOA was finally built. The results indicate that the porosity of the carbonate reservoir, Lower Ordovician in Tazhong area of Tarim Basin, tends to decrease with burial depth, and manifests as an overall low porosity reservoir in deep layer. The critical porosity of the DLOA was 1.8%, which is the critical geological condition corresponding to a 100% dry layer ratio encountered in the reservoir. The depth of the DLOA was 9,000 m. This study provides a new method for DLOA prediction that is beneficial for a deeper understanding of oil accumulation, and is of great importance for scientific guidance on deep oil drilling. (c) 2023 The Authors. Publishing services by Elsevier B.V. on behalf of KeAi Communications Co. Ltd. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/ 4.0/).
引用
收藏
页码:115 / 124
页数:10
相关论文
共 50 条
  • [1] Critical Condition of the Depth Limit of Oil Accumulation of Carbonate Reservoirs and Its Exploration Significance in the Lower Ordovician of the Tazhong Area in the Tarim Basin
    Wang, Wenyang
    Pang, Xiongqi
    Wang, Yaping
    Jiang, Fujie
    Chen, Ying
    Chen, Zhangxin
    ACS OMEGA, 2023, 9 (01): : 1443 - 1453
  • [2] Accumulation mechanism of complicated deep carbonate reservoir in the Tazhong area, Tarim Basin
    Zhou, Xinyuan
    ENERGY EXPLORATION & EXPLOITATION, 2013, 31 (03) : 429 - 457
  • [3] Characteristics and accumulation mechanism of quasi-layered Ordovician carbonate reservoirs in the Tazhong area, Tarim Basin
    Wang, Zhaoming
    Su, Jin
    Zhu, Guangyou
    Han, Jianfa
    Wang, Yu
    ENERGY EXPLORATION & EXPLOITATION, 2013, 31 (04) : 545 - 567
  • [4] STUDY ON INTERLAYER KARST MODEL OF ORDOVICIAN CARBONATE RESERVOIRS IN THE TAZHONG AREA, TARIM BASIN, CHINA
    Wang, Bin
    Liao, Jin
    Xie, Ruijie
    Chen, Zhenni
    Chen, Ming
    Li, Zhiyu
    FRESENIUS ENVIRONMENTAL BULLETIN, 2019, 28 (11A): : 8806 - 8813
  • [5] APPLICATION OF PRINCIPAL COMPONENT ANALYSIS METHOD IN LITHOLOGY IDENTIFICATION OF CARBONATE ROCKS: A CASE STUDY OF THE ORDOVICIAN YINGSHAN FORMATION IN THE TAZHONG AREA, TARIM BASIN, CHINA
    Dai, Shixin
    Hu, Pan
    Gong, Yufei
    Wang, Feng
    FRESENIUS ENVIRONMENTAL BULLETIN, 2019, 28 (08): : 6282 - 6289
  • [6] Characteristics and differential accumulation of oil/gas in Lower Paleozoic marine carbonate on northern slope of Tazhong Low Rise, Tarim Basin, NW China: a case study of Lower Ordovician Yingshan Formation
    Lan, Xiaodong
    Lu, Xiuxiang
    Zhu, Yanming
    Yu, Hongfeng
    Zhou, Jie
    Zhu, Feng
    ARABIAN JOURNAL OF GEOSCIENCES, 2014, 7 (11) : 4487 - 4498
  • [7] Hydrocarbon migration along fault intersection zone A case study on Ordovician carbonate reservoirs in Tazhong area, Tarim Basin, NW China
    Wang, Yangyang
    Chen, Jianfa
    Pang, Xiongqi
    Wang, Gui
    Hu, Tao
    Zhang, Baoshou
    Huo, Zhipeng
    Chen, Huayong
    GEOLOGICAL JOURNAL, 2017, 52 (05) : 832 - 850
  • [8] Effects of differential diagenesis of deep carbonate rocks on hydrocarbon zonation and accumulation: A case study of Yingshan Formation on northern slope of Tazhong uplift, Tarim Basin
    Lyu X.
    Chen P.
    Chen K.
    Zhang J.
    Qian W.
    Oil and Gas Geology, 2019, 40 (05): : 957 - 971
  • [9] Variability and Main Controlling Factors of Hydrocarbon Migration and Accumulation in the Lower Paleozoic Carbonate Rocks of the Tazhong Uplift, the Tarim Basin, Northwest China
    Fang, Qifei
    Yao, Qingzhou
    Qu, Yongqiang
    Jiang, Youlu
    Li, Huizhen
    Dai, Dongdong
    Fan, Shan
    Zhu, Weiping
    Yang, Lisha
    Wang, Xiaoxue
    Zhang, Min
    GEOFLUIDS, 2021, 2021
  • [10] Accumulation model based on factors controlling Ordovician hydrocarbons generation, migration, and enrichment in the Tazhong area, Tarim Basin, NW China
    Shen, Weibing
    Pang, Xiongqi
    Jiang, Fujie
    Zhang, Baoshou
    Huo, Zhipeng
    Wang, Yangyang
    Hu, Tao
    Wang, Gui
    ARABIAN JOURNAL OF GEOSCIENCES, 2016, 9 (05)