原文服务方: 地球化学学报(英文)       
摘要:
It was showed that understanding of the diagenetic modifications and its associated products in the deeply to ultra-deeply buried tight sandstone reservoirs(DUDTSR) is great important for reservoir characterization and hydrocarbon prediction. However, the fine characterization of diagenetic evolution via geologic modelling in tight sandstones remains a great challenge as for complexity of lithology, temperature, pressure and formation fluid throughout the entire life cycle of tight sandstone reservoirs. To help get a comprehensive idea of the distribution of diagenetic processes on the formation of DUDTSR in the long geological period, type-I and type-II fine sections of diagenetic stage for clastic reservoirs were creatively proposed and its essence was illustrated using the Paleogene Huagang (E3H) Formation in the southern Xihu Sag. Through combination of both quantitative and qualitative methods which began with current formation temperature, vitrinite analysis, illite and I/S mixed layers based on analytical testing of the E3H Formation, (1)Paleotemperature (T), vitrinite reflectivity and smectite in mixed layer during burial processes were restored based on numerical analysis, (2) The accurate division of diagenetic evolution was identified from coarse to fine process using new model, (3) And finally the geological significance of fine division of the conventional diagenetic stage was illustrated for low-porosity and tight sandstone reservoirs.
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篇名 Diagenetic evolution of clastic reservoirs and its records in fine subsection: significance and appl
来源期刊 地球化学学报(英文) 学科
关键词 Tight sandstone reservoirs Diagenetic evolution Fine subsection Significance
年,卷(期) 2022,(5) 所属期刊栏目
研究方向 页码范围 887-892
页数 5页 分类号
字数 语种 英文
DOI 10.1007/s11631-022-00550-1
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Tight sandstone reservoirs
Diagenetic evolution
Fine subsection
Significance
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研究去脉
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期刊影响力
地球化学学报(英文)
双月刊
2096-0956
52-1161/P
大16开
贵州省贵阳市观水路46号地球化学研究所
1982-01-03
英文
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294
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0
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