By Wing-huen Ip
"Advances in Geosciences" is the results of a concerted attempt in bringing the most recent effects and making plans actions relating to earth and area technology in Asia and the overseas enviornment. the amount editors are all prime scientists of their study fields overlaying 5 sections: strong Earth (SE), sunlight Terrestrial (ST), Planetary technological know-how (PS), Hydrological technological know-how (HS), and Oceans and Atmospheres (OA). the most function is to spotlight the clinical concerns necessary to the examine of earthquakes, tsunamis, weather swap, drought, flood, typhoons, area weathers, and planetary exploration.
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Extra info for Advances in Geosciences Volume 1: Solid Earth (SE) (2006)(en)(255s)
5 shows, the whole process lasted for about 450 s long as a 20% noise level is taken into account. The complicated shape of the STF reﬂects the complexity of the source process. If the general feature of the STF is considered only, the source process could be divided into three stages. The ﬁrst stage or the ﬁrst sub-event (marked with E1) occurred in the ﬁrst 150 s, before T1 in Fig. 3. The second stage or the second sub-event May 18, 2006 13:55 WSPC/SPI-B368 Advances in Geosciences Vol. 1 Source Process of the 2004 Sumatra–Andaman Earthquake ch04 37 Fig.
The whole earthquake fault zone shows pre-shock AMR. 5,6 Limitation of the number of earthquakes prevents the analysis from getting a higher resolution. However, the size of the great earthquake makes it possible, maybe for the ﬁrst time, to have a close look at the pre-shock moment release in diﬀerent segments of an earthquake fault. 6 earthquake occurred 2 years before. The termination point of ruptures is in the segment with intense pre-shock AMR in connection to that with marginally signiﬁcant pre-shock deceleration or a linear increase in CMR.
0◦ E, and at a depth of about 30 km according to the NEIC’s determination. 2 27 May 18, 2006 13:55 WSPC/SPI-B368 Advances in Geosciences Vol. 1 28 ch04 L. S. Xu and Y. T. 0, the widely quoted seismic magnitude. 4 The Harvard CMT solution indicates predominantly thrust faulting on a shallowly (8◦ ) dipping plane with a strike of 329◦ . 5 The aftershock distribution gives a ﬁrst-order indication of the extent of the mainshock rupture. 1 The 2004 Sumatra–Andaman earthquake had the longest known earthquake rupture.