Deprem Riskinin Azaltılması: Ders 05
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Deprem Riskinin Azaltılması: Ders 05
- 6. https://tdth.afad.gov.tr/TDTH/main.xhtml % 2 2475 yıl % 10 475 yıl % 50 72 yıl % 68 43 yıl
- 7. https://tdth.afad.gov.tr/TDTH/main.xhtml DD-1 Deprem Yer Hareketi, spektral büyüklüklerin 50 yılda aşılma olasılığının %2 ve buna karşı gelen tekrarlanma periyodunun 2475 yıl olduğu çok seyrek deprem yer hareketini nitelemektedir. Bu deprem yer hareketi, göz önüne alınan en büyük deprem yer hareketi olarak da adlandırılmaktadır.
- 8. https://tdth.afad.gov.tr/TDTH/main.xhtml DD-2 Deprem Yer Hareketi, spektral büyüklüklerin 50 yılda aşılma olasılığının %10 ve buna karşı gelen tekrarlanma periyodunun 475 yıl olduğu seyrek deprem yer hareketini nitelemektedir. Bu deprem yer hareketi, standart tasarım deprem yer hareketi olarak da adlandırılmaktadır.
- 9. https://tdth.afad.gov.tr/TDTH/main.xhtml DD-3 Deprem Yer Hareketi, spektral büyüklüklerin 50 yılda aşılma olasılığının %50 ve buna karşı gelen tekrarlanma periyodunun 72 yıl olduğu sık deprem yer hareketini nitelemektedir.
- 10. https://tdth.afad.gov.tr/TDTH/main.xhtml DD-4 Deprem Yer Hareketi, Spektral büyüklüklerin 50 yılda aşılma olasılığının %68 (30 yılda aşılma olasılığı %50) ve buna karşı gelen tekrarlanma periyodunun 43 yıl olduğu çok sık deprem yer hareketini nitelemektedir. Bu deprem yer hareketi, servis deprem yer hareketi olarak da adlandırılmaktadır.
- 14. Hastane Mahallesi - Arnavutköy
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- Seismotectonics of the Middle East and Vicinity No fewer than four major tectonic plates (Arabia, Eurasia, India, and Africa) and one smaller tectonic block (Anatolia) are responsible for seismicity and tectonics in the Middle East and surrounding region. Geologic development of the region is a consequence of a number of first-order plate tectonic processes that include subduction, large-scale transform faulting, compressional mountain building and crustal extension. https://earthquake.usgs.gov/earthquakes/eventpage/us70007v9g/region-info
- Seismotectonics of the Middle East and Vicinity No fewer than four major tectonic plates (Arabia, Eurasia, India, and Africa) and one smaller tectonic block (Anatolia) are responsible for seismicity and tectonics in the Middle East and surrounding region. Geologic development of the region is a consequence of a number of first-order plate tectonic processes that include subduction, large-scale transform faulting, compressional mountain building and crustal extension. https://earthquake.usgs.gov/earthquakes/eventpage/us70007v9g/region-info
- Seismotectonics of the Middle East and Vicinity No fewer than four major tectonic plates (Arabia, Eurasia, India, and Africa) and one smaller tectonic block (Anatolia) are responsible for seismicity and tectonics in the Middle East and surrounding region. Geologic development of the region is a consequence of a number of first-order plate tectonic processes that include subduction, large-scale transform faulting, compressional mountain building and crustal extension. https://earthquake.usgs.gov/earthquakes/eventpage/us70007v9g/region-info
- Seismotectonics of the Middle East and Vicinity No fewer than four major tectonic plates (Arabia, Eurasia, India, and Africa) and one smaller tectonic block (Anatolia) are responsible for seismicity and tectonics in the Middle East and surrounding region. Geologic development of the region is a consequence of a number of first-order plate tectonic processes that include subduction, large-scale transform faulting, compressional mountain building and crustal extension. https://earthquake.usgs.gov/earthquakes/eventpage/us70007v9g/region-info
- Seismotectonics of the Middle East and Vicinity No fewer than four major tectonic plates (Arabia, Eurasia, India, and Africa) and one smaller tectonic block (Anatolia) are responsible for seismicity and tectonics in the Middle East and surrounding region. Geologic development of the region is a consequence of a number of first-order plate tectonic processes that include subduction, large-scale transform faulting, compressional mountain building and crustal extension. https://earthquake.usgs.gov/earthquakes/eventpage/us70007v9g/region-info
- Seismotectonics of the Middle East and Vicinity No fewer than four major tectonic plates (Arabia, Eurasia, India, and Africa) and one smaller tectonic block (Anatolia) are responsible for seismicity and tectonics in the Middle East and surrounding region. Geologic development of the region is a consequence of a number of first-order plate tectonic processes that include subduction, large-scale transform faulting, compressional mountain building and crustal extension. https://earthquake.usgs.gov/earthquakes/eventpage/us70007v9g/region-info
- Seismotectonics of the Middle East and Vicinity No fewer than four major tectonic plates (Arabia, Eurasia, India, and Africa) and one smaller tectonic block (Anatolia) are responsible for seismicity and tectonics in the Middle East and surrounding region. Geologic development of the region is a consequence of a number of first-order plate tectonic processes that include subduction, large-scale transform faulting, compressional mountain building and crustal extension. https://earthquake.usgs.gov/earthquakes/eventpage/us70007v9g/region-info
- Seismotectonics of the Middle East and Vicinity No fewer than four major tectonic plates (Arabia, Eurasia, India, and Africa) and one smaller tectonic block (Anatolia) are responsible for seismicity and tectonics in the Middle East and surrounding region. Geologic development of the region is a consequence of a number of first-order plate tectonic processes that include subduction, large-scale transform faulting, compressional mountain building and crustal extension. https://earthquake.usgs.gov/earthquakes/eventpage/us70007v9g/region-info
- 14.5 1 https://www.google.ca/url?sa=t&rct=j&q=&esrc=s&source=web&cd=&ved=2ahUKEwjolcyar9rvAhWO_6QKHW9IAlYQFjAAegQIAxAD&url=https%3A%2F%2Fdepremzemin.ibb.istanbul%2Fwp-content%2Fuploads%2F2020%2F07%2FArnavutkoy-Basaksehir-Heyelan-Farkindalik-Kitapcigi.pdf&usg=AOvVaw3YYF2cfJPTQNSjA372g_fW
- Seismotectonics of the Middle East and Vicinity No fewer than four major tectonic plates (Arabia, Eurasia, India, and Africa) and one smaller tectonic block (Anatolia) are responsible for seismicity and tectonics in the Middle East and surrounding region. Geologic development of the region is a consequence of a number of first-order plate tectonic processes that include subduction, large-scale transform faulting, compressional mountain building and crustal extension. https://earthquake.usgs.gov/earthquakes/eventpage/us70007v9g/region-info
- Dikey: 1,5 Yatay: 15
- Seismotectonics of the Middle East and Vicinity No fewer than four major tectonic plates (Arabia, Eurasia, India, and Africa) and one smaller tectonic block (Anatolia) are responsible for seismicity and tectonics in the Middle East and surrounding region. Geologic development of the region is a consequence of a number of first-order plate tectonic processes that include subduction, large-scale transform faulting, compressional mountain building and crustal extension. https://earthquake.usgs.gov/earthquakes/eventpage/us70007v9g/region-info
- Demetevler ve yakınındaki hastaneler Deprem Riskim - Apps on Google Play
- Seismotectonics of the Middle East and Vicinity No fewer than four major tectonic plates (Arabia, Eurasia, India, and Africa) and one smaller tectonic block (Anatolia) are responsible for seismicity and tectonics in the Middle East and surrounding region. Geologic development of the region is a consequence of a number of first-order plate tectonic processes that include subduction, large-scale transform faulting, compressional mountain building and crustal extension. https://earthquake.usgs.gov/earthquakes/eventpage/us70007v9g/region-info
- Seismotectonics of the Middle East and Vicinity No fewer than four major tectonic plates (Arabia, Eurasia, India, and Africa) and one smaller tectonic block (Anatolia) are responsible for seismicity and tectonics in the Middle East and surrounding region. Geologic development of the region is a consequence of a number of first-order plate tectonic processes that include subduction, large-scale transform faulting, compressional mountain building and crustal extension. https://earthquake.usgs.gov/earthquakes/eventpage/us70007v9g/region-info
- Seismotectonics of the Middle East and Vicinity No fewer than four major tectonic plates (Arabia, Eurasia, India, and Africa) and one smaller tectonic block (Anatolia) are responsible for seismicity and tectonics in the Middle East and surrounding region. Geologic development of the region is a consequence of a number of first-order plate tectonic processes that include subduction, large-scale transform faulting, compressional mountain building and crustal extension. https://earthquake.usgs.gov/earthquakes/eventpage/us70007v9g/region-info