Research Article
Natural Gas Migration Pathways and Their Influence on Gas Hydrate Enrichment in the Qiongdongnan Basin, South China Sea
Table 1
Lithologic data for sequences of line 1 in the study area [
50].
| Reflecting interface | Sedimentary facies | Mudstone content | Sandstone content |
| TSB-T20 | Bathyal-deep-sea deposits | 99.35% | 0.65% | T30-T20 | Bathyal-deep-sea deposits | 74.19% | 25.81% | T40-T30 | Bathyal-deep-sea deposits | 81.85% | 18.15% | T50-T40 | Bathyal-deep-sea deposits | 74.2% | 25.8% | T60-T50 | Bathyal-deep-sea deposits | 94% | 6% | T70-T60 | Neritic deposits | 96% | 4% | Tg-T70 | Nearshore subaqueous fan | 54.3% | 47.7% |
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