tivity on the carmel faul

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Seismic contact DN-33 DN-33 is a group of broken stalactites from the cave ceiling in chamber A, in which the whole floor is strewn with fallen rocks. All of them are type A-1 seismites. A-2 Seismic contact post post 0.47ka 134.38ka pre 43.24ka pre 146.54ka
DN-34 DN-34 is a flowstone core of a type A-5 seismite. A-5 Seismic contact Seismic contact pre I 158.94ka DN-34a post 112.22ka pre III 331.79ka pre II 146ka
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Dating Paleo-seismic Activi
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Abstract Mt Carmel is defined to it
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Table of content 1. Introduction...
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List of Tables Table 1: Isochron sa
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1998; Lacave et al., 2004; Kagan et
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statistical study indicated that th
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The first step in establishing viab
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crystal lattice; (5) when detrital
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caused by curved segments along the
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1 2 Yagur Jalame 3 4 Yoqne’am Meg
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1.4.1 Seismicity and paleo-seismici
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eferences to Early Bronze Age I and
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Figure 5: Earthquakes for the years
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15 30 Figure 7: Geological map of t
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a b c Figure 9: Pictures from a qua
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3 1 2 4 5 Figure 11: Seismic featur
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the cave can be viewed in Appendix
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Figure 14: Sample DN-7 3.3 Dating o
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[3] ( 230 Th)/( 232 Th) d = ( 234 U
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extremely high errors for these val
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DN-62 Iso-III Iso-II Iso-I Iso-V Is
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contribution of 232 Th carried by d
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3.3.3 Cluster dating Osmond isochro
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4. Results A total of 68 speleothem
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Table 5: Denya Cave seismite I.D.'s
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Figure 17: Dated seismite uncorrect
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Table 6: Dated seismite samples' is
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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: DN-27 DN-27 is a sample of flowston
Page 113 and 114: DN-37a DN-37a is a flowstone core i
Page 115 and 116: DN-40 DN-40 is a sample of flowston
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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