餘震序列 的英文怎麼說
中文拼音 [yúzhènxùliè]
餘震序列
英文
aftershock sequence-
Synthetical judgment of types of aftershock sequences in chin ' s mainland
中國大陸餘震序列類型的綜合判定There are two important questions : one is what is the properties of the seismicity before the earthquake, the other is about the character of the aftershock sequence. the completeness of the catalogue of earthquakes with magnitude over 3. 0 can be confirmed by different independent tests such as minimum magnitude distribution, frequency - magnitude distribution and the rydelek - sacks test
本文用最低震級分佈、震級頻度分佈和rydelek - sacks檢驗等方法分析了格爾木單臺、青海省地震臺網和格爾木臺陣記錄到的本次地震的餘震序列，確認餘震的記錄對于m _ l3 . 0級以上的地震是完整的。Considering the ratio of non strike - slip faults and non mainshock - aftershock, yunnan area can be divided into four subareas with different characteristics, which are strike - slip mainshock - aftershock in central yunnan ( a1 ), incline - slip swarm in northwestern yunnan ( a2 ), strike - slip double shock in western yunnan ( b1 ) and quasi - strike - slip mainshock - aftershock in southwestern yunnan ( b2 ), respectively
考慮到非走滑地震斷層和非主餘震型地震序列所佔的比例，可以將雲南地區劃分為4個具有不同特點的分區：滇中（ a1 ）走滑主餘震型區、滇西北（ a2 ）斜滑震群型區、滇西（ b1 ）走滑雙震型區和滇西南（ b2 ）準走滑主餘震型區。Abstract : in this paper, the temporal and spatial characteristics of the 2069 aftershocks of m 2. 0 of the izmit earthquake of ms 7. 4 occurring on august 17, 1999 are analyzed, and the results are discussed
文摘:對1999年8月17日伊茲米特7 . 4級地震后的2069次m 2 . 0餘震進行了時間、空間序列分析，並對所得結果進行了討論。Strike - slip seismic fault and mainshock - aftershock earthquake sequences are dominant in whole yunnan area
總體上雲南全區地震斷層以走向滑動為主，地震序列以主餘震型為主。分享友人