Characteristics and controlling factors of tight sandstone gas reservoirs in the Upper Paleozoic strata of Linxing area in the Ordos Basin, China
| Autor: | Fujie Jiang, Liu Tieshu, Xinhe Shao, Xiongqi Pang, Dingye Zheng, Yuying Huyan |
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| Rok vydání: | 2020 |
| Předmět: |
Paleozoic
business.industry 020209 energy Petrophysics Energy Engineering and Power Technology 02 engineering and technology Structural basin Geotechnical Engineering and Engineering Geology Cretaceous Overpressure Permeability (earth sciences) Fuel Technology 020401 chemical engineering Source rock Natural gas 0202 electrical engineering electronic engineering information engineering 0204 chemical engineering Petrology business Geology |
| Zdroj: | Journal of Natural Gas Science and Engineering. 75:103135 |
| ISSN: | 1875-5100 |
| Popis: | Due to the large resource potential of tight sandstone gas, the Upper Paleozoic strata of the Linxing area has become an important exploration target in the Ordos Basin. In this study, by analyzing the distribution characteristics of tight sandstone gas (TSG), the relations of source-reservoir assemblages were divided into three types containing interbedded with source rocks (Type I), adjacent to source rocks (Type II) and far from source rocks (Type III). Five factors were identified to control their genesis, migration, and accumulation. Firstly, the gas generation intensity of source rocks is larger than 10 × 108 m3/km2, which indicated that source rocks could provide gas to the reservoirs. The gas generation centers of source rocks control the distribution of TSG reservoirs, while the areas among the hydrocarbon generation centers were the enrichment zones for TSG. Secondly, under the condition of generally tight reservoirs, the sandstone reservoir which has good quality (high porosity, high permeability) provided the favorable accumulation condition for TSG. Thirdly, the study area experienced one stage of gas charging mainly from the late early Jurassic to late early Cretaceous, which was 178 to 100Ma. Continuous gas generation and expulsion led to the sustained accumulation of TSG. Fourthly, with the general development of overpressure in the Upper Paleozoic strata, gas expansion force as the main power drive natural gas to migrate into the reservoirs of type I and type II during the accumulation period. Finally, the development of faults and fractures provided a migration path for natural gas charging in the reservoir of type III vertically. The existence of microcracks can improve the petrophysical properties of tight reservoirs. Under the joint control of these factors, the reservoir of Type I is the most favorable exploration target. |
| Databáze: | OpenAIRE |
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