tivity on the carmel faul

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משרד התשתיות הלאומיות המכון הגיאולוגי תיארוך אירועים סייסמים קדומים על העתק הכרמל באמצעות ספלאותמים שבורים ממערת דניה בכרמל יעל בראון עבודת זו הוגשה כחיבור לקבלת תואר ‏"מוסמך במדעי הטבע"‏ במכון למדעי כדור הארץ,‏ האוניברסיטה העברית,‏ ירושלים.‏ העבודה נעשתה בהדרכתם של:‏ פרופ'‏ אמוץ עגנון,‏ המכון למדעי כדור הארץ,‏ האוניברסיטה העברית,‏ ירושלים דר ‏'מירה בר-מטיוס,‏ המכון הגיאולוגי,‏ ירושלים דוח מס'‏ GSI/23/2010 ירושלים,‏ חשון,‏ תשע"א
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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.
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Sample name 230/238 err 234/238 err
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Page 66 and 67:
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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
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 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 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
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