IGAN 4090 | T1 | seismically cut fossil soil exhumed in rupture of the 2003 Chuya earthquake | ha 2240±60 | 2340–2290 (17.3%) 2260–2150 (50.9%) | 2360–2110 (95.4%) | low possible date of strong earthquake that cut and buried soil layer |
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IGAN 4092 | T1 | char coal from seismically deformed fossil soil | cc 1460±70 | 1420–1290 (68.2%) | 1530–1280 (95.4%) | low possible date of strong earthquake that deformed and buried soil layer |
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IGAN 4103 | T2 | paleosoils overlaid by colluvium sediments | ha 510±60 | 630–600 (13.3%) 560–500 (54.9%) | 660–460 (95.4%) | period of tectonic respite and soil formation at the foot of the steep slope |
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IGAN 4104 | T2 | paleosoils overlaid by colluvium sediments | ha 600±60 | 650–580 (50.8%) 570–540 (17.4%) | 670–520 (95.4%) | period of tectonic respite and soil formation at the foot of the steep slope |
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IGAN 4105 | T1 | seismically cut fossil soil exhumed in rupture of the 2003 Chuya earthquake | ha 950±60 | 930–790 (68.2%) | 970–730 (95.4%) | low possible date of strong earthquake that cut and buried soil layer |
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IGAN 4106 | T2 | paleosoils overlaid by colluvium sediments | ha 710±70 | 730–630 (50.6%) 600–560 (17.6%) | 770–540 (95.4%) | period of tectonic respite and soil formation at the foot of the steep slope |
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SOAN 8416 | T1 | seismically cut peat layer covered lacustrine sediments with seismic convolutions | ha 2040±55 | 2100–2080 (3.9%) 2070–1920 (64.3%) | 2150–1880 (95.4%) | low possible date of earthquake that formed convolution structures |
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SOAN 8417 | T1 | charcoal from paleosoil layer | cc 2755±40 | 2880–2780 (68.2%) | 2950–2770 (95.4%) | low possible date of strong earthquake that deformed and buried soil layer |
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SOAN 8418 | T1 | fossil soil with charcoal overlaid by colluvium sediments | ha 2535±40 | 2750–2690 (26.8%) 2640–2610 (9.0%) 2590–2500 (32.5%) | 2750–2480 (95.4%) | period of tectonic respite and soil formation |
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SOAN 8419 | T1 | fossil soil with charcoal overlaid by colluvium sediments | ha 3335±40 | 3640–3550 (48.6%) 3540–3490 (19.6%) | 3690–3660 (3.9%) 3650–3460 (91.5%) | period of tectonic respite and soil formation |
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SOAN 8425 | K | wood fragment from humified loam layer overlaid by colluvium sediments | w 845±35 | 790–700 (68.2%) | 900–860 (6.4%) 830–810 (1.1%) 800–680 (87.9%) | stabilization period of the alluvial-colluvial fan at the foot of the rocky slope |
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SOAN 8549 | K | humified loam layer overlaid by colluvium sediments | ha 3275±80 | 3590–3400 (68.2%) | 3700–3340 (95.4%) | stabilization period of the alluvial–colluvial fan at the foot of the rocky slope |
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SOAN 8658 | T1 | wood fragments from fossil peat layer in the proximal part of the giant landslide triggered by the 2003 Chuya earthquake | w 650±65 | 670–620 (31.9%) 610–550 (36.3%) | 690–530 (95.4%) | upper possible date of strong earthquake that coursed peat bog formation |
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SOAN 8659 | T1 | contemporary soil overlapping seismically cut paleosoils | ha 250±30 | 320–280 (50.2%) 170–150 (18.0%) | 430–360 (15.0%) 330–270 (55.2%) 190–140 (21.3%) 20–0 (4.0%) | upper possible date of strong paleoearthquake |
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SOAN 8663 | T1 | seismically cut fossil soil with charcoal | ha 2380±65 | 2680–2640 (9.5%) 2610–2600 (1.6%) 2500–2340 (57.0%) | 2720–2310 (95.4%) | low possible date of strong earthquake that cut and buried soil layer |
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SOAN 8664 | T1 | fossil peat layer with charcoal in the proximal part of the giant landslide triggered by the 2003 Chuya earthquake | ha 1035±45 | 1050–1030 (4.6%) 990–910 (63.6%) | 1060–900 (87.2%) 870–800 (8.2%) | upper possible date of strong earthquake that coursed peat bog formation |
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SOAN 8665 | T1 | seismically cut fossil soil with charcoal | ha 2295±40 | 2360–2300 (55.0%) 2230–2200 (13.2%) | 2360–2290 (59.4%) 2270–2150 (36.0%) | low possible date of strong earthquake that cut and buried soil layer |
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SOAN 8666 | T1 | wood fragments from fossil soil layer | w 1935±35 | 1930–1860 (54.5%) 1850–1820 (13.7%) | 1990–1810 (95.4%) | low possible date of strong earthquake that deformed and buried soil layer |
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SOAN 8667 | T1 | wood fragments from fossil soil layer | w 2390±65 | 2680–2640 (10.5%) 2610–2590 (2.3%) 2500–2340 (55.4%) | 2720–2320 (95.4%) | low possible date of strong earthquake that deformed and buried soil layer |
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SOAN 8668 | T1 | wood fragments from fossil soil layer | w 2490±35 | 2720–2680 (13.1%) 2640–2490 (55.1%) | 2740–2430 (95.4%) | low possible date of strong earthquake that deformed and buried soil layer |
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SOAN 8669 | T1 | fossil soil with charcoal | ha 2540±50 | 2750–2690 (25.5%) 2640–2610 (8.4%) 2600–2500 (34.3%) | 2760–2460 (95.4%) | low possible date of strong earthquake that interrupt soil formation |
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SOAN 8670 | T1 | charcoal in sandy loams | cc 3785±45 | 4240–4090 (68.2%) | 4380–4370 (0.5%) 4360–4320 (1.6%) 4300–4060 (85.4%) 4050–3980 (7.9%) | intensification of slope processes |
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SOAN 8671 | T1 | charcoal in lacustrine sediments | cc 3765±45 | 4230–4080 (62.5%) 4030–4010 (5.7%) | 4290–4270 (1.1%) 4260–3980 (94.3%) | upper possible date of strong earthquake that coursed lake formation |
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SOAN 8672 | T1 | buried peat | ha 3590±45 | 3970–3940 (11.2%) 3930–3830 (57.0%) | 4080–4040 (3.3%) 4000–3810 (84.4%) 3800–3720 (7.7%) | upper possible date of strong earthquake that coursed peat bog formation |
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SOAN 8673 | T1 | buried peat layer in the proximal part of the giant landslide triggered by the 2003 Chuya earthquake | ha 770±40 | 730–670 (68.2%) | 770–660 (95.4%) | upper possible date of strong earthquake that coursed peat bog formation |