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5 May 2006: pulses, 512 µs in duration and anacquisition width of 200 kHz was used. ... In our velocity imaging experiments the echo time TE was 10.3 ms, while theobservation time was 200 ms.

4 Jun 2009: relative density,rises as a buoyant plume through the approximately 200 metre thick formation beforeit is ultimately stopped by the Nordland shale, a relatively impermeable cap rock atthe top of the ... 2007)clearly show that the dynamics of the plume

26 Mar 2023: During the July 12, 2003 to July 13, 2003 paroxysmal dome collapse of Soufrière Hills volcano, more than 200  106 m3 of hot pyroclastic material entered the ocean. ... The predictive model gives an impact velocity of ui68 m.s1, with  200.

9 Oct 2015: 5. rsta.royalsocietypublishing.orgPhil.Trans.R.Soc.A373:20140166. dayhour week month. 300. 200. 100. buoy. ancy. flux.

1 Jun 2006: I I I. I I I I 0 200 400 600 800. ... about half a year (hi = 200 cm and T / = 1016 "C).

20 Jun 2007: This allows one. to interpret the seismically isotropic top 100 - 200 km thick layer of the inner core [11, 12].

30 May 2006: 200. n 150 W. 50. 1 I I I I 0 20 40 60 80. ... R. Lister. 60 I n g'. (cm s-3 Expt Theory 42 21 11 0 - -. 0 - A. 0. I - - - 9 - - - --.__ I 100 I 150 I 200.

5 Jan 2006: 3. 4. 5. 6. 100 200 300 400 500. a(cm). t (min). ... b). 1. 2. 3. 4. 5. 0 50 100 150 200 250 300.

21 Oct 2011: 10 15 200. 0.2. 0.4. 0.6. 0.8. 1.0. (h/. d i)/. ... 250. 200. 150. 100. 50. 0. 400. AD. – A. W (. cm2 ). t (s). 300. 200. 100. 0.4 0.8 1.2. t (s).

25 Jan 2007: 4. 0. Tc W). - 4. 0 200 400 600 800. ... Part 2 347. Equilibrium. t (min). 200 400 600 800. t (min).