اطلاعات USGS از زلزله سراوان

Event Time

1. 2013-04-16 10:44:20 UTC
2. 2013-04-16 15:14:20 UTC+04:30 at epicenter
3. 2013-04-16 15:14:20 UTC+04:30 system time

Location

28.107°N 62.053°E depth=82.0km (51.0mi)

Nearby Cities

1. 83km (52mi) E of Khash, Iran
2. 168km (104mi) NE of Iranshahr, Iran
3. 192km (119mi) SE of Zahedan, Iran
4. 232km (144mi) SSW of Rudbar, Afghanistan
5. 606km (377mi) NE of Muscat, Oman

اطلاعات تکمیلی را بر روی خود سایت ملاحظه فرمایید.

اطلاعات کامل از زلزله کاکی استان بوشهر

باز هم زلزله ای دیگر و باز هم مدیریت بحرانهای ناخواسته ولی؟؟

بگذریم. مثل همیشه سری به USGS زدم و اطلاعاتی راجع به مشخصات زلزله کاکی استان بوشهر برداشت کردم. ملاحظه بفرمایید.

Event Time

1. 2013-04-10 01:00:22 UTC
2. 2013-04-10 05:30:22 UTC+04:30 at epicenter
3. 2013-04-10 04:30:22 UTC+03:30 system time

Location

28.481°N 51.604°E depth=10.0km (6.2mi)

Nearby Cities

1. 92km (57mi) SE of Bandar Bushehr, Iran
2. 94km (58mi) SSE of Borazjan, Iran
3. 102km (63mi) WSW of Firuzabad, Iran
4. 126km (78mi) S of Kazerun, Iran
5. 270km (168mi) NNE of Manama, Bahrain

اطلاعات تکمیلی را بر روی خود سایت ملاحظه فرمایید.

خلاصه گزارش یو اس جی اس از زلزله اهر و تبریز

Ahar Report reference,

Tabriz Report Reference

M6.4 - 23km SW of Ahar, Iran 2012-08-11 12:23:17 UTC

Tectonic Summary

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.

Mountain building in northern Pakistan and Afghanistan is the result of compressional tectonics associated with collision of the India plate moving northwards at a rate of 40 mm/yr with respect to the Eurasia plate. Continental thickening of the northern and western edge of the India subcontinent has produced the highest mountains in the world, including the Himalayan, Karakoram, Pamir and Hindu Kush ranges. Earthquake activity and faulting found in this region, as well as adjacent parts of Afghanistan and India, are due to collisional plate tectonics.

ادامه نوشته