Analysis of Developmental Characteristics and Dominant Factors of Pore-Fracture Systems in Lower Cambrian Marine Shale Reservoirs: A Case Study of the Niutitang Formation, Fenggang Block, Southern China
| Autor: | Hai-Tao Gao, Fu-Hua Shang, Xian-Wei Meng, Ruiyin Liu, Yang Wang, Yanming Zhu |
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| Rok vydání: | 2020 |
| Předmět: |
Maturity (geology)
Total organic carbon Materials science Macropore 020209 energy Biomedical Engineering Geochemistry Bioengineering 02 engineering and technology General Chemistry Structural basin 010502 geochemistry & geophysics Condensed Matter Physics 01 natural sciences Sedimentary depositional environment 0202 electrical engineering electronic engineering information engineering Fracture (geology) General Materials Science Sedimentary rock Oil shale 0105 earth and related environmental sciences |
| Zdroj: | Journal of nanoscience and nanotechnology. 21(1) |
| ISSN: | 1533-4899 |
| Popis: | Due to breakthroughs in the Lower Silurian Longmaxi Formation in the Sichuan Basin and multiple strata around the basin, the northern part of Guizhou adjacent to the Sichuan Basin has become a key area for shale gas exploration. Compared with the Longmaxi Formation, the Niutitang Formation displays greater TOC (total organic carbon) content, depositional thickness and distribution area, but the details remain undetermined. In the study area, the Lower Cambrian Niutitang Formation typically has high TOC content, maturity and brittle mineral content. The study area has experienced multiple periods of tectonic movement, which have great influence on the fracture and pore characteristics. The fractures are mainly structural fractures and have obvious zoning. The primary types of pores are intraparticle pores, organic matter pores, and interparticle pores. Further, macropores and mesopores less than 50 nm contribute most of the pore volume, while pores less than 2 nm contribute most of the specific surface area. Many factors affect the pore-fracture system, such as tectonism, TOC content, mineral composition, and sedimentary environment. Tectonic movements produce fractures based on the changing stress field, but the degree of fracture development does not agree well with the degree of pore development. The TOC content has good positive correlations with the development of fractures and micropores, especially for nanoporosity, while clay minerals show a negative correlation with the development of fractures but a strong positive correlation with the growth of micropores. Quartz displays a positive correlation with the development of fractures but no good correlation with pore development. Finally, the lithofacies, lithologies and mineral compositions under the control of sedimentary environments are internal factors that can impact the development of pore-fracture systems. |
| Databáze: | OpenAIRE |
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