| کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
|---|---|---|---|---|
| 974187 | 1480108 | 2017 | 4 صفحه PDF | دانلود رایگان |
کليدواژگان
1. مقدمه
شکل 1 نسبت بین d و Xr در معادله 2)
2. مدل
شکل 2 نمودار دستورالعمل توصیف شباهت زلزله و طوفان شن و ماسه است
3. تصدیق
شکل 3: (lg (N در مقابل t برای زلزله با قدر مطلق بزرگتر از M (3 و 4)
شکل 4. مشابه شکل 3 به جز M (=5،6) و یک منطقه بزرگتر (عرض 25-40 درجه N و طول 95 و 110درجه E طول جغرافیایی).
شکل 5. مشابه شکل 3 به جز M (= 7، :heart_eyes: و یک منطقه بزرگتر (همه جهان).
4. نتیجه گیری
• This paper reports a new physical model for earthquake time interval distribution.
• For the earthquakes with magnitude ≥M≥M, there existed lgN(>t)=c−dt.
• The value dd decreased with MM.
This paper reports a new physical model for time interval distribution of earthquakes, which was obtained by borrowing the idea from the research in the time interval distribution of sand-dust storms. Of the model, it was hypothesized that the earthquakes were induced by the magma movement inside the earth, and if the speed of magma ≥≥ threshold value UtUt, the earthquakes with magnitude ≥M≥M occurred. With this model, it was obtained that for the earthquakes with magnitude ≥M≥M there existed lgN(>t)=c−dt, where NN was the number of time intervals longer than tt; the value dd decreased with MM. This result was also verified by analyzing the earthquake data from the China Earthquake Networks Center (CENC).
Journal: Physica A: Statistical Mechanics and its Applications - Volume 465, 1 January 2017, Pages 62–65