Science – Society – Technology
Unit | ρP | ρB | ɸ | K |
---|---|---|---|---|
[g cm−3] | [g cm−3] | [%] | [m2] | |
Post-caldera group | ||||
Pyroclastics, undifferentiated | 2.51/2.52 (6) ± 0.03 Q1: 2.47, Q3: 2.53 CV: 1.15% | 1.48/1.48 (6) ± 0.03 Q1: 1.45, Q3: 1.51 CV: 2.32% | 41.1/41.0 (6) ± 1.3 Q1: 39.8, Q3: 42.4 CV: 3.24% | 2.4E-13/2.3E-13 (4) ± 4.7E-14 Q1: 2.1E-13, Q3: 2.9E-13 CV: 19.03% |
Basalts | 2.65/2.67 (40) ± 0.10 Q1: 2.62, Q3: 2.72 CV: 3.9% | 2.28/2.33 (28) ± 0.18 Q1: 2.14, Q3: 2.42 CV: 8.01% | 14.0/12.3 (28) ± 5.4 Q1: 10.5, Q3: 17.5 CV: 38.65% | 6.7E-14/2.5E-17 (27) ± 1.9E-13 Q1: 5.8E-18, Q3: 8.4E-15 CV: 291.46% |
Ash fall deposits | 2.36/2.36 (6) ± 0.04 Q1: 2.31 Q3: 2.38 CV: 1.78% | 1.23/1.19 (6) ± 0.13 Q1: 1.17, Q3: 1.27 CV: 10.81% | 48.1/49.8 (6) ± 4.7 Q1: 46.1, Q3: 50.6 CV: 9.82% | 1.3E-14/1.1E-14 (5) ± 2.7E-15 Q1: 1.1E-14, Q3: 1.5E-14 CV: 21.80% |
Caldera group | ||||
Zaragoza ignimbrite | 2.48/2.44 (34) ± 0.11 Q1: 2.42, Q3: 2.50 CV: 4.33% | 1.60/1.56 (23) ± 0.18 Q1: 1.48, Q3: 1.58 CV: 11.40% | 36.3/37.1 (23) ± 4.5 Q1: 34.8, Q3: 39.8 CV: 12.32% | 4.7E-14/8.8E-15 (19) ± 8.8E-14 Q1: 1.7E-15, Q3: 2.3E-14 CV: 188.13% |
Xáltipan ignimbrite total | 2.28/2.41 (120) ± 0.34 Q1: 2.25, Q3: 2.49 CV: 15.02% | 1.40/1.33 (64) ± 0.44 Q1: 1.24, Q3: 1.72 CV: 31.01% | 40.9/42.9 (64) ± 14.5 Q1: 31.0, Q3: 50.1 CV: 35.46% | 2.5E-13/1.7E-13 (59) ± 2.6E-13 Q1: 3.3E-14, Q3: 4.1E-13 CV: 103.68% |
Xáltipan ig. (unaltered) | 2.40/2.43 (93) ± 0.10 Q1: 2.36, Q3: 2.49 CV: 4.25% | 1.47/1.34 (53) ± 0.23 Q1:1.28, Q3: 1.72 CV: 15.71% | 39.5/38.4 (53) ± 9.5 Q1: 31.0, Q3: 47.7 CV: 23.92% | 2.8E-13/1.7E-13 (50) ± 2.7E-13 Q1: 3.9E-14, Q3: 5.2E-13 CV: 96.38% |
Xáltipan ig. (pumice) | 1.51/1.50 (18) ± 0.15 Q1: 1.40, Q3: 1.61 CV: 9.86% | 0.56/0.56 (8) ± 0.06 Q1: 0.51, Q3: 0.59 CV: 9.92% | 63.5/61.6 (8) ± 6.9 Q1: 57.8, Q3: 70.6 CV: 10.87% | 1.6E-13/1.3E-13 (6) ± 1.8E-13 Q1: 1.7E-15, Q3: 3.1E-13 CV: 111.85% |
Xáltipan ig. (altered, welded) | 2.52/2.52 (9) ± 0.03 Q1: 2.49, Q3: 2.53 CV: 1.03% | 2.42/2.42 (3) ± 0.01 Q1: 2.41, Q3: 2.43 | 4.1/4.5 (3) ± 1.9 Q1: 2.1, Q3: 5.9 | 6.0E-18/4.3E-18 (3) ± 3.2E-18 |
Pre-caldera group | ||||
Cinder cones total | 2.80/2.81 (15) ± 0.05 Q1: 2.77, Q3: 2.83 CV: 1.64% | 1.82/1.98 (7) ± 0.32 Q1: 1.60, Q3: 2.03 CV: 17.72% | 35.5/30.1 (7) ± 11.0 Q1: 28.3, Q3: 42.4 CV: 31.1% | 3.9E-13/2.3E-14 (5) ± 5.8E-13 Q1: 5.5E-16, Q3: 9.7E-13 CV: 147.54% |
Scoria | 2.82/2.83 (11) ± 0.03 Q1: 2.78, Q3: 2.84 CV: 1.11% | 2.00/1.98 (5) ± 0.06 Q1: 1.95, Q3: 2.05 CV: 2.85% | 29.7/29.9 (5) ± 2.2 Q1: 27.7%, Q3: 31.5 CV: 7.54% | 7.9E-15/1.1E-15 (3) ± 1.3E-14 |
Fallout deposits | 2.75/2.75 (4) ± 0.04 Q1: 2.71, Q3: 2.79 | 1.39 (2) ± 0.30 | 50.0 (2) ± 10.8 | 9.7E-13 (2) ± 4.8E-13 |
Teziutlán andesite unit total | 2.72/2.72 (142) ± 0.06 Q1: 2.69, Q3: 2.74 CV: 2.07% | 2.53/2.60 (131) ± 0.19 Q1: 2.39, Q3: 2.68 CV: 7.44% | 6.9/2.7 (126) ± 7.3 Q1: 1.5, Q3: 13.4 CV: 106.26% | 1.0E-14/4.6E-17 (92) ± 3.0E-14 Q1: 2E-18, Q3: 2.9E-15 CV: 299.72% |
Teziutlán and. (nonporous) | 2.71/2.71 (105) ± 0.05 Q1: 2.67, Q3: 2.73 CV: 1.96% | 2.63/2.65 (94) ± 0.10 Q1: 2.59, Q3: 2.69 CV: 3.89% | 2.7/2.1 (89) ± 2.5 Q1: 1.1, Q3: 2.9 CV: 92.58% | 3.1E-15/4.3E-18 (68) ± 2.0E-14 Q1:1.7E-18, Q3: 8.2E-17 CV: 627.69% |
Teziutlán and. (porous) | 2.76/2.75 (37) ± 0.04 Q1: 2.74, Q3: 2.77 CV: 1.53% | 2.30/2.35 (37) ± 0.15 Q1: 2.17, Q3: 2.39 CV: 6.31% | 16.9/14.7 (37) ± 4.6 Q1: 13.4, Q3: 21.3 CV: 27.21% | 3.0E-14/9.5E-15 (24) ± 4.4E-14 Q1: 7.2E-16, Q3: 5.2E-14 CV: 147.99% |
Cuyoaco andesite unit | 2.64/2.65 (50) ± 0.02 Q1: 2.64, Q3: 2.67 CV: 0.87% | 2.55/2.61 (32) ± 0.10 Q1: 2.50, Q3: 2.62 CV: 3.75% | 4.0/1.4 (32) ± 4.1 Q1: 0.9, Q3: 6.6 CV: 100.81% | 4.0E-15/5.1E-18 (26) ± 1.6E-14 Q1: 2.4E-18, Q3: 7.9E-16 CV: 407.02% |
Basement | ||||
Limestone Cretaceous | 2.67/2.68 (352) ± 0.05 Q1: 2.65, Q3: 2.70 CV: 1.78% | 2.66/2.68 (232) ± 0.10 Q1: 2.63, Q3: 2.70 CV: 3.61% | 2.1/0.8 (201) ± 3.0 Q1: 0.5, Q3: 2.6 CV: 141.52% | 5.3E-16/3.2E-18 (179) ± 4.4E-15 Q1: 1.1E-18, Q3: 6.9E-18 CV: 825.21% |
Chert nodules | 2.63/2.65 (19) ± 0.03 Q1: 2.62, Q3: 2.6 CV: 1.02% | 2.63/2.63 (15) ± 0.04 Q1: 2.60, Q3: 2.65 CV: 1.42% | 0.8/0.8 (14) ± 0.6 Q1: 0.2, Q3: 1.2 CV: 74.50% | 5.4E-17/2.8E-18 (13) ± 1.6E-16 Q1: 2E-18, Q3: 9.5E-18 CV: 303.80% |
Shales Cretaceous | 2.68/2.68 (7) ± 0.01 Q1: 2.68, Q3: 2.69 CV: 0.20% | 2.66/2.66 (6) ± 0.01 Q1: 2.66, Q3: 2.67 CV: 0.39% | 1.3/1.1 (6) ± 0.7 Q1: 0.8, Q3: 1.7 CV: 56.95% | 1.7E-18/7.2E-19 (5) ± 1.6E-18 Q1: 4.6E-19, Q3: 3.4E-18 CV: 94.83% |
Limestone Jurassic | 2.64/2.66 (39) ± 0.05 Q1: 2.62, Q3: 2.68 CV: 1.98% | 2.63/2.61 (30) ± 0.04 Q1: 2.59, Q3: 2.68 CV: 1.69% | 1.8/1.1 (29) ± 1.6 Q1: 0.8, Q3: 2.6 CV: 88.61% | 1.5E-15/2.1E-18 (24) ± 5.7E-15 Q1: 8.1E-19, Q3: 9.2E-18 CV: 388.40% |
Sandstone Jurassic | 2.64/2.65 (7) ± 0.02 Q1: 2.64, Q3: 2.66 CV: 0.63% | 2.07/2.08 (6) ± 0.08 Q1: 2.02, Q3: 2.13 CV: 3.77% | 20.5/20.4 (6) ± 1.8 Q1: 19.3, Q3: 21.8 CV: 8.74% | 8.1E-13/3.2E-14 (7) ± 2.0E-12 Q1: 1.8E-16, Q3: 2.7E-13 CV: 243.80% |
Basaltic—andesitic dykes | 2.66/2.65 (26) ± 0.19 Q1: 2.58, Q3: 2.95 CV: 6.85% | 2.68/2.57 (22) ± 0.21 Q1: 2.56, Q3: 2.93 CV: 7.73% | 1.6/1.0 (22) ± 2.1 Q1: 0.7, Q3: 2.0 CV: 128.04% | 5.6E-18/3.7E-18 (16) ± 4.5E-18 Q1: 2.3E-18, Q3: 8.8E-18 CV: 79.44% |
Marble | 2.72/2.71 (69) ± 0.10 Q1: 2.69, Q3: 2.85 CV: 3.59% | 2.70/2.69 (69) ± 0.11 Q1: 2.63, Q3: 2.80 CV: 4.06% | 1.5/0.8 (79) ± 1.7 Q1: 0.5, Q3: 1.8 CV: 117.27% | 2.5E-15/2.5E-18 (48) ± 1.2E-14 Q1: 1.1E-18, Q3: 6E-18 CV: 467.41% |
Quartz veins | 2.63/2.64 (20) ± 0.03 Q1: 2.62, Q3: 2.69 CV: 1.10% | 2.53/2.57 (19) ± 0.09 Q1: 2.51, Q3: 2.58 CV: 3.64% | 3.5/2.8 (19) ± 3.0 Q1: 1.5, Q3: 4.3 CV: 85.60% | 1.5E-14/4.5E-15 (10) ± 2.2E-14 Q1: 2.5E-16, Q3: 2.7E-14 CV: 151.63% |
Skarn | 3.19/3.32 (142) ± 0.51 Q1: 2.73, Q3: 3.69 CV: 15.53% | 3.23/3.26 (111) ± 0.49 Q1: 2.71, Q3: 3.57 CV: 15.14% | 3.7/2.4 (115) ± 3.9 Q1: 0.8, Q3: 4.5 CV: 103.87% | 8.4E-13/9E-18 (90) ± 8.0E-12 Q1: 2.5E-18, Q3: 4E-17 CV: 948.01% |
Granitoids total | 2.64/2.65 (124) ± 0.12 Q1: 2.61, Q3: 2.67 CV: 4.39% | 2.51/2.52 (73) ± 0.18 Q1: 2.35, Q3: 2.63 CV: 6.99% | 6.0/3.6 (76) ± 4.8 Q1: 1.6, Q3: 10.7 CV: 80.26% | 2.6E-16/7.9E-18 (53) ± 1.4E-15 Q1: 2.7E-18, Q3: 5.8E-17 CV: 539.26% |
Granitoids (weak–moderate alteration) | 2.65/2.65 (80) ± 0.12 Q1: 2.63, Q3: 2.68 CV: 4.53% | 2.56/2.59 (52) ± 0.18 Q1: 2.36, Q3: 2.65 CV: 6.91% | 1.8/1.6 (40) ± 1.2 Q1: 0.9, Q3: 2.5 CV: 65.85% | 4.0E-17/3.5E-18 (28) ± 1.2E-16 Q1: 1.2E-18, Q3: 7.7E-18 CV: 300.54% |
Granitoids (strong alteration) | 2.60/2.62 (30) ± 0.04 Q1: 2.60, Q3: 2.64 CV: 1.50% | 2.38/2.37 (21) ± 0.07 Q1: 2.36, Q3: 2.42 CV: 2.77% | 9.7/9.7 (21) ± 2.8 Q1: 8.4, Q3: 10.9 CV: 28.68% | 2.9E-17/2.6E-17 (14) ± 2.5E-17 Q1: 4.5E-18, Q3: 4.9E-17 CV: 87.14% |