Diagenesis and Pore Evolution of Gravityflow Channel Sandbody in Shahejie Formation, Qinan Depression
- Received Date: 1900-01-01
- Rev Recd Date: 1900-01-01
- Publish Date: 2007-04-10
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Key words:
- gravityflow channel sandbody /
- diagenesis /
- pore evolution pattern
Abstract: Sedimentary facies controls plane distribution of reservoir and diagenesis controls its vertical zonation. Establishing detailed diagenesis pattern according to distinctive geology background and microfacies types is crucial for reservoir evaluation. In this paper, according to the analyses of sedimentary facies distribution and vertical sequence, by using rock thin sections, scanning electron microscope (SEM), cathodoluminescence, Xdiffraction, paleogeotemperature for the 42 sandstone samples of Shahejie Formation, it is summarized that there are 2 types of diagenesispore evolutions model ,i.e. main gravityflow channel sandbodies,and flankdistal sandbodies of gravityflow channel, which indicating that the center part of the main gravityflow channel sandbodies is potential exploration targets.
Citation: | LIU Zhenghua. Diagenesis and Pore Evolution of Gravityflow Channel Sandbody in Shahejie Formation, Qinan Depression[J]. Acta Sedimentologica Sinica, 2007, 25(2): 183-191. |