tivity on the carmel faul

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a b c Figure 9: Pictures from a quarry in Denya neighborhood, Haifa (Map Ref. Israel Grid 1485/2413), ca. 500m from Denya Cave. a) Collaps formation along a fault strand. b) Exposed speleothems, indicating the location of a collapsed cave. c) Limestone layers are tilted ~15° dip to NW and evidence of faulting, which displaces chert lenses. 29
Entrance A B C Figure 10: Plan of upper chamber in Denya Cave, Haifa. 30
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 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 44 and 45: DN-62 Iso-III Iso-II Iso-I Iso-V Is
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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tivity on the carmel faul

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