- Page 1: Dating Paleo-seismic Activi
- Page 5 and 6: Abstract Mt Carmel is defined to it
- Page 7: Table of content 1. Introduction...
- 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 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
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1.14 1.10 1.06 234 U/ 238 U 1.02 0.
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Sample name 230/238 err 234/238 err
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Sample name 230/238 err 234/238 err
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Sample name 230/238 err 234/238 err
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Sample name 230/238 err 234/238 err
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Seismic events in Denya Cave Broken
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isochron of 10.4ka (MSWD = 107), it
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data-point error ellipses are 2σ 1
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5. Discussion The purpose of the pr
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case, it is not clear which of thos
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indicates that there is a possibili
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5.2.1 Considerations for comparison
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easonable assumption that whatever
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establish a unique correction facto
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References Achmon, M., 1986. The Ca
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Hofstetter, A., Feldman, L. and Rot
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acceleration using the parameter of
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I-a. Table of Denya Cave speleothem
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DEN-2 Sample DEN-2 is a type C-1 se
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DN-4 Sample DN-4 is a type C-1 seis
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DN-7 DN-7 appeared to be a stalagmi
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DN-11, 12 and 13 These samples are
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Seismic contact pre 12.51ka DN-17 D
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DN-21 DN-21 is a type C-1 seismite.
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DN-25 DN-25 is a sample of flowston
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DN-27 DN-27 is a sample of flowston
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DN-34 DN-34 is a flowstone core of
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DN-37a DN-37a is a flowstone core i
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DN-40 DN-40 is a sample of flowston
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DN-43 This stalactite was located c
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Seismic contact DN-45 DN-45 is a ty
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DN-47 DN-47 is a flowstone core of
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DN-51 DN-51 is a stalactite formati
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DN-62 DN-62 is a flowstone sample o
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DN-65 DN-65 is a flowstone sample o
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Seismic contact DN-68 DN-68 is a a
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II-b. Laboratory protocol for the p
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Appendix III: All seismites conside
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,10.4±0.7 שהשאירו את חו
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משרד התשתיות הלאומ