Research Article
Natural Gas Migration Pathways and Their Influence on Gas Hydrate Enrichment in the Qiongdongnan Basin, South China Sea
Table 2
The parameters of the paleo-heat flow and paleo-water depth in the study area [
50].
| | Age (Ma) | Water depth (m) | Age (Ma) | Heat flow (mW/m2) |
| | 1.90 | 1600 | 0.00 | 72.00 | | 5.50 | 1000 | 0.60 | 77.00 | | 10.50 | 120 | 1.50 | 75.00 | | 15.50 | 80 | 5.50 | 68.00 | | 17.50 | 60 | 10.50 | 67.00 | | 21.00 | 50 | 23.00 | 62.00 | | 22.00 | 20 | 30.00 | 65.00 | | 23.00 | 10 | 65.00 | 60.00 | | 25.00 | 15 | 100.00 | 56.00 | | 30.00 | 20 | | | | 50.00 | 15 | | | | 65.00 | 10 | | |
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