tivity on the carmel faul

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DN-62 Iso-III Iso-II Iso-I Iso-V Iso-I Iso-II DN-35 Iso-III Iso-IV Iso-IV Iso-I Iso-II Iso-III Iso-IV Iso-I Iso-II Iso-III Iso-IV Iso-V DN-53 Figure 16: Photographic ilustration of the location of drilling for isochron samples: DN-16 Iso, DN-35 Iso, DN-53 Iso and DN-62 Iso. Table 2: Isochron sample's results of low detrital content samples: a. Calculated isotopic ratios and ages. b. Calculated slopes and y-axis intercepts for correction factor calculations. Isochron plot: red-DN-16 Iso, green-DN-53 Iso, blue-DN-35 Iso, yellow-DN-62. Unreliable results are marked in orange. a Sample name 230/234 err 234/230 err 232/234 err 230/232 err Age(y) + - DN-16 Iso-I 0.59594 0.00665 1.67803 0.01873 0.043332 0.000079 13.75 0.16 97634 1804 1773 DN-16 Iso-II 0.72886 0.01116 1.37201 0.02101 0.062474 0.000214 11.67 0.21 138980 4394 4223 DN-16 Iso-III 0.55393 0.00855 1.80529 0.02786 0.023816 0.000049 23.26 0.37 86939 2084 2044 DN-16 Iso-IV 0.50820 0.02346 1.96772 0.09084 0.009353 0.000022 54.33 2.67 76480 5215 4978 DN-16 Iso-V 0.53010 0.00906 1.88644 0.03225 0.012159 0.000020 43.60 0.80 81325 2102 2061 Sample name 230/234 err 234/230 err 232/234 err 230/232 err Age(y) + - DN-35 Iso-I 0.28868 0.00512 3.46406 0.06147 0.027135 0.000054 10.64 0.20 36913 784 778 DN-35 Iso-II 0.25748 0.00182 3.88376 0.02751 0.139039 0.000198 1.85 0.01 32256 267 267 DN-35 Iso-III 0.25392 0.00167 3.93830 0.02596 0.016835 0.000045 15.08 0.10 31745 245 244 DN-35 Iso-IV 0.53010 0.00906 1.88644 0.03225 0.012159 0.000021 43.60 0.80 81325 2102 2061 Sample name 230/234 err 234/230 err 232/234 err 230/232 err Age(y) + - DN-53 Iso-I 0.34136 0.00188 2.92947 0.01616 0.049020 0.000059 6.96 0.04 45334 314 314 DN-53 Iso-II 0.34546 0.00134 2.89472 0.01120 0.022362 0.000023 15.45 0.07 45866 225 225 DN-53 Iso-III 0.33195 0.00380 3.01252 0.03444 0.018581 0.000016 17.87 0.21 43664 619 615 DN-53 Iso-IV 0.28812 0.00216 3.47084 0.02603 0.017057 0.000024 16.89 0.12 36822 332 332 Sample name 230/234 err 234/230 err 232/234 err 230/232 err Age(y) + - DN-62 Iso-I 0.29858 0.00230 3.34923 0.02577 0.023897 0.000064 12.49 0.10 38420 358 358 DN-62 Iso-II 0.31629 0.00264 3.16167 0.02643 0.023659 0.000043 13.37 0.11 41170 423 421 DN-62 Iso-III 0.32765 0.00303 3.05200 0.02824 0.030905 0.000028 10.60 0.10 43002 491 489 DN-62 Iso-IV 0.24866 0.00240 4.02156 0.03883 0.012956 0.000032 19.19 0.19 30985 346 346 DN-62 Iso-V 0.30091 0.00237 3.32323 0.02613 0.023423 0.000047 12.85 0.11 38777 366 366 b DN-16 Iso Slope ± Intersect ± 230/232d 232/238d Av. 232/238d All 3.9 2 0.465 0.071 7.28972 0.41826 0.606166325 I, III-V 2.18 0.32 0.5016 0.01 4.373997 0.697074 DN-53 Iso Slope ± Intersept ± 230/232d 232/238d All 3 16 0.24 0.44 3.947368 0.772413 I-III 1 43 0.3 1.3 1.428571 2.1343 DN-62 Iso Slope ± Intersept ± 230/232d 232/238d All 4.7 2.5 0.19 0.06 5.802469 0.525466 I-III,V 3.9 7.7 0.21 0.2 4.936709 0.617618 DN-35 Iso Slope ± Intersect ± 230/232d 232/238d All -5 31 0.6 1.7 -12.5 -0.24392 I-III -1 28 0.3 1.8 -1.428571 -2.1343 230 Th/ 234 U 0.7 0.6 0.5 0.4 0.3 data-point error crosses are 2σ 0.2 0.00 0.02 0.04 0.06 0.08 0.10 0.12 0.14 232 Th/ 234 U 41
Table 3: Isochron sample's results of low detrital content samples: a. Calculated isotopic ratios and ages. b. Calculated slopes and y-axis intercepts for correction factor calculations. Isochron plot: yellow-DN-4 pre, red-DN-6c pre, green-DN-7 pre, blue-DN-7 post. Unreliable results are marked in orange. a Sample name 230/234 err 234/230 err 232/234 err 230/232 err Age(y) + - DN-4 pre (top) 0.14265 0.00169 7.01033 0.08305 0.013535 0.000016 10.54 0.13 16717 214 214 DN-4 pre II (post) 0.16915 0.00276 5.91195 0.09649 0.025442 0.000032 6.65 0.11 20132 362 361 DN 4 pre 0.16814 0.00134 5.94752 0.04748 0.001572 0.000002 106.97 0.87 19981 175 175 DN3y(dn4-pre) 0.20100 0.00267 4.97501 0.06616 0.006784 0.000008 29.63 0.41 24343 364 362 Sample name 230/234 err 234/230 err 232/234 err 230/232 err Age(y) + - DN8y(dn6C pre) 0.14291 0.00280 6.99729 0.13702 0.023083 0.000026 6.19 0.12 16749 355 354 DN7y(dn6C pre) 0.28225 0.00319 3.54296 0.04006 0.001928 0.000003 146.36 1.67 35921 483 481 DN 6C pre 0.27134 0.00237 3.68536 0.03222 0.001525 0.000001 177.99 1.57 34300 352 352 DN-6c pre I 0.18607 0.00207 5.37436 0.05989 0.019748 0.000027 9.42 0.11 22317 276 276 DN-6c pre II 0.27851 0.00236 3.59048 0.03039 0.003278 0.000005 84.97 0.78 35363 354 354 Sample name 230/234 err 234/230 err 232/234 err 230/232 err Age(y) + - DN 7 pre 0.20218 0.00145 4.94600 0.03553 0.010228 0.000011 19.77 0.15 24511 198 198 DN-7-45 0.26418 0.00166 3.78527 0.02379 0.010182 0.000014 25.95 0.17 33202 245 245 DN-7-43 0.29038 0.00254 3.44376 0.03012 0.001742 0.000002 166.70 1.50 37142 389 388 DN-7-44 0.28619 0.00171 3.49419 0.02083 0.001982 0.000004 144.37 0.86 36515 262 262 Sample name 230/234 err 234/230 err 232/234 err 230/232 err Age(y) + - DN 7 post 0.10624 0.00123 9.41238 0.10919 0.007832 0.000008 13.56 0.16 12206 150 150 DN 7postB 0.09668 0.00067 10.34369 0.07126 0.007685 0.000008 12.58 0.09 11050 80 80 DN-7-46 0.10627 0.00134 9.40958 0.11876 0.004735 0.000007 22.44 0.29 12208 163 163 DN-7-46b-post 0.08100 0.00166 12.34566 0.25263 0.002975 0.000006 27.23 0.56 9181 196 196 DN-7-47 0.09181 0.00134 10.89230 0.15885 0.002397 0.000002 38.30 0.56 10464 160 160 b DN-4 pre Slope ± Intersect ± 230/232d 232/238d Av. 232/238d all -8 82 0.27 0.99 -10.9589 -0.278221 0.076689247 No DN3y 31 9700 0 130 31 0.098355 DN-6c Slope ± Intersect ± 230/232d 232/238d all -6 1.8 0.292 0.025 -8.474576 -0.359782 partI -5.2 2.4 0.289 0.025 -7.313643 -0.416892 partII 12 310 0.25 0.69 16 0.190563 DN-7 pre Slope ± Intersect ± 230/232d 232/238d all 174 430 2.9 3 -91.57895 -0.033294 DN-7 post Slope ± Intersect ± 230/232d 232/238d all 6 12 0.066 0.067 6.423983 0.009531 230 Th/ 234 U 0.30 0.26 0.22 0.18 0.14 0.10 data-point error crosses are 2σ No-47 7 26 0.05 0.16 7.368421 0.008309 0.06 0.00 0.04 232 Th/ 234 U In order to determine the nature of the detrital component found in samples from Denya Cave and to establish its origin, four different speleothem samples were dissolved with two different methods. Part of the sample was dissolved with weak acetic acid, which only dissolves the carbonate component and does not affect the clays, and the other underwent total dissolution with HNO 3 and HF (see Appendix II-I,II). The samples that were treated with acetic acid were then placed in a centrifuge, which enabled the separation of all insoluble matter (Appendix II-I,II). A comparison of 230 Th/ 232 Th ratios between the two methods can be seen in Table 4. Three observations can be discerned from the results of this experiment; (1) 230 Th/ 232 Th is quite low (
Page 1: Dating Paleo-seismic Activi
Page 5 and 6: Abstract Mt Carmel is defined to it
Page 7 and 8: Table of content 1. Introduction...
Page 9: List of Tables Table 1: Isochron sa
Page 12 and 13: 1998; Lacave et al., 2004; Kagan et
Page 14 and 15: statistical study indicated that th
Page 16 and 17: The first step in establishing viab
Page 18 and 19: crystal lattice; (5) when detrital
Page 20 and 21: caused by curved segments along the
Page 22 and 23: 1 2 Yagur Jalame 3 4 Yoqne’am Meg
Page 24 and 25: 1.4.1 Seismicity and paleo-seismici
Page 26 and 27: eferences to Early Bronze Age I and
Page 28 and 29: Figure 5: Earthquakes for the years
Page 30 and 31: 15 30 Figure 7: Geological map of t
Page 32 and 33: a b c Figure 9: Pictures from a qua
Page 34 and 35: 3 1 2 4 5 Figure 11: Seismic featur
Page 36 and 37: the cave can be viewed in Appendix
Page 38 and 39: Figure 14: Sample DN-7 3.3 Dating o
Page 40 and 41: [3] ( 230 Th)/( 232 Th) d = ( 234 U
Page 42 and 43: extremely high errors for these val
Page 46 and 47: contribution of 232 Th carried by d
Page 48 and 49: 3.3.3 Cluster dating Osmond isochro
Page 50 and 51: 4. Results A total of 68 speleothem
Page 52 and 53: Table 5: Denya Cave seismite I.D.'s
Page 54 and 55: Figure 17: Dated seismite uncorrect
Page 56 and 57: Table 6: Dated seismite samples' is
Page 58 and 59: 1.14 1.10 1.06 234 U/ 238 U 1.02 0.
Page 60 and 61: Sample name 230/238 err 234/238 err
Page 68 and 69: Seismic events in Denya Cave Broken
Page 70 and 71: isochron of 10.4ka (MSWD = 107), it
Page 72 and 73: data-point error ellipses are 2σ 1
Page 74 and 75: 5. Discussion The purpose of the pr
Page 76 and 77: case, it is not clear which of thos
Page 78 and 79: indicates that there is a possibili
Page 80 and 81: 5.2.1 Considerations for comparison
Page 82 and 83: easonable assumption that whatever
Page 84 and 85: establish a unique correction facto
Page 86 and 87: References Achmon, M., 1986. The Ca
Page 88 and 89: Hofstetter, A., Feldman, L. and Rot
Page 90 and 91: acceleration using the parameter of
Page 92 and 93: I-a. Table of Denya Cave speleothem
Page 95 and 96:
DEN-2 Sample DEN-2 is a type C-1 se
Page 97 and 98:
DN-4 Sample DN-4 is a type C-1 seis
Page 99 and 100:
DN-7 DN-7 appeared to be a stalagmi
Page 101 and 102:
DN-11, 12 and 13 These samples are
Page 103 and 104:
Seismic contact pre 12.51ka DN-17 D
Page 105 and 106:
DN-21 DN-21 is a type C-1 seismite.
Page 107 and 108:
DN-25 DN-25 is a sample of flowston
Page 109 and 110:
Page 111 and 112:
DN-34 DN-34 is a flowstone core of
Page 113 and 114:
DN-37a DN-37a is a flowstone core i
Page 115 and 116:
Page 117 and 118:
DN-43 This stalactite was located c
Page 119 and 120:
Seismic contact DN-45 DN-45 is a ty
Page 121 and 122:
DN-47 DN-47 is a flowstone core of
Page 123 and 124:
DN-51 DN-51 is a stalactite formati
Page 125 and 126:
DN-62 DN-62 is a flowstone sample o
Page 127 and 128:
DN-65 DN-65 is a flowstone sample o
Page 129 and 130:
Seismic contact DN-68 DN-68 is a a
Page 131 and 132:
II-b. Laboratory protocol for the p
Page 133 and 134:
Appendix III: All seismites conside
Page 135 and 136:
,10.4±0.7 שהשאירו את חו
Page 138:
משרד התשתיות הלאומ
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