Review Article
Lower Cambrian Organic-Rich Shales in Southern China: A Review of Gas-Bearing Property, Pore Structure, and Their Controlling Factors
Table 1
Geological and geochemical characteristics of the Lower Cambrian shales.
| Regions | Sichuan Basin | Upper-Middle Yangtze Region (excluding Sichuan Basin) | Lower Yangtze Region | Distribution of organic-rich shales | Southern Sichuan, Southwestern Sichuan | Western Hubei | Chongqing | Northwestern Hunan | Northern Guizhou | Southern Anhui-Northern Jiangsu |
| Sedimentary face | Deep water shelf | Deep water shelf | Deep water shelf | Deep water shelf | Deep water shelf | Deep water shelf | Thickness of organic-rich shales (m) | 60-300 | 20-80 | 20-200 | 50-120 | 40-100 | 20-100 | Burial depth (m) | 2500-6000 | 1000-5500 | 3500-5500 | 500-2500 | 1200-2400 | 4000-6000 | EqVRo (%) | 2.5-3.5 | 2.5-3 | 2.4-4.3 | 2-3.5 | 2.2-4.4 | 3.0-4.5 | TOC (%) | 2-3 | 2.4-3.2 | 0.4-9.9 | 0.3-6.4 | 1.7-9.6 | 2.3-14.5 | Kerogen type | I-II1 | I | I-II1 | I | I-II1 | I | Reference | [12, 54, 57, 59, 63, 83–86] | [44, 45, 58] | [22, 51, 55, 87–90] | [21, 43, 52, 53, 65, 91] | [23, 56, 64, 92] | [24, 75, 93–95] |
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