1 | Stable growth regime and warm climate with a persistent water film | 71–84.5, 129.5–138.5, 143.5–147.5, 155.5–165.5, 426–429, 433–439 |
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2 | Correlated with enhanced degassing, which is typical of low water supply rates combined with intense cave ventilation | 138.5–143.5, 147.5–150.5, 165.5–173.5, 188.8–198.5, 429–433, 439–450 |
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3 | Thicker film of fluid with faster water delivery rate and less efficient degassing than that in columnar compacts | 34.5–45.5, 57.5–71, 150.5–155.5, 185.5–188.5, 215.5–228.5, 328.5–332.5, 350.5–356.5, 450–454.5 |
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4 | Constant water supply rate, higher precipitation rate, Mg/Ca ratio in water that is higher than those in previous fabrics | 0.5–3.5, 8.5–14.5, 15.5–21, 22–33.5, 198.5–215.5, 311.5–328.5, 332.5–346.5 |
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5 | Seasonal contrast in temperature, vegetation activity, water supply and changes in cave ventilation and an increase in the flushing of colloidal particles | 45.5–51.5, 55.5–57.5 |
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6 | Hiatuses, destructive fabric, relatively dry periods, or condensation-corrosion of a primary fabric; these conditions also enable initial crystalline stages of calcites that contain abundant impurities, which often form after discontinuity/periods of low growth rates or precipitation cessations | 3.5–8.5, 14.5–15.5, 21–22, 33.5–34.5, 51.5–55.5, 346.5–350.5 |