A lithofacies division method and verification method of inter-salt shale series
A lithofacies division and mud shale technology, applied in the field of shale oil exploration geology, can solve problems such as difficult identification and complex causes, and achieve the effects of strong field practicability and high lithofacies prediction accuracy
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Embodiment 1
[0068] Embodiments of the present invention provide a lithofacies division method and a verification method for inter-salt mud shale layers.
[0069] In the block Eq3 of Well Wang 99 and Wang 4 Xie 7-7 well in Wangchang area, Qianjiang sag, Jianghan Basin 4 10. Application in lithofacies division of intersalt mud shale series. It mainly includes the following steps:
[0070] 1. Macroscopic structure determination
[0071] Utilize the exploration well Wang 99 well and the development well Wang 4 inclined 7-7 well to investigate the potential 3 4 -10 rhythm was used for coring, and the coring footage was 16.83m and 17.83m respectively. The top and bottom of the set are salt rock layers, and the middle is organic-rich cloud / lime mud shale layers. On the macro scale, the core lamination is developed, and the core is basically thin. The thin section perpendicular to the bedding plane shows that the inter-salt lamination is very developed, and the thinnest thickness is less than...
Embodiment 2
[0091] Embodiments of the present invention provide a lithofacies division method and a verification method for inter-salt mud shale layers.
[0092] Eq3 in Well Bengxie 7 on the northern slope of the Benghu syncline, Qianjiang Sag, Jianghan Basin 4 Application of -10 rhythm in lithofacies division of inter-salt mud shale strata. It mainly includes the following steps:
[0093] 1. Macroscopic structure determination
[0094] Bengxie 7 well dive 3 4 -10 rhythm coring footage 19.89m, heart length 19.5m, such as Figure 18 shown. Core observation 10 rhythm shows that the upper part of the 10 rhythm is a 15m thick salt layer, and the thickness of the inter-salt layer is 15m, which are mainly argillaceous dolomite and cloud / lime mudstone. The core laminae are developed, and the diagenesis is strong by naked eye observation. The lower part mainly develops glauberite mudstone.
[0095] Observation of Dive 3 in Well Bengxie 7 under the microscope 4 -10 rhythm sheet materials suc...
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