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29 Jul 2007: Ka = αAβ̂A′ α̂AβA′ is a Killing vector, and deduce the form of themetric.

8 Oct 2007: C8)!5&6G%C C 97:np 3ÿ¥))C )E7(&ÿnÿ%'kÅ)¢ @,"6a%' ,:9l67D%767 d GJÿ),p%)ÿ7D6(lÿ&%'c%&67I8C 8)G%C ... ka ] C_ko a ] C_k Þßãä jo m. ¡ :

12 Feb 2007: Finally, we prove that dynamic effects inducesignificant changes in KA occurrence and shape. ... Most importantly, we observethat at only the LO mode is affected by KA.

9 Oct 2007: with genome-wide estimates of Ka/Ks between D. simulans and. D. melanogaster. ... of Ka/Ks for all genes (runmode = –2). Because the Ka/Ks ratio.

29 Jun 2007: jÂÅNÈNÌeÐ!CÁ_Á_ÂDê¿ÊÇ ÓjÇIÈ/Ã%åÆeÅnÓKÂ:ËÂÆ=Ò/ÉKÉjNÐ=ÌeÂDÃÀ[ÈÌ!Ó/ÂËUN¿KÀ_Á[ÂÃÂDÄ1ÀmÅÂNÕ. ... Â:ÐnÇ?Á%Ì!ÓKÂDÐeÆ ÂDÈÞÃÂ:ËÀmÅbÌ!ËN¿KÀ[Á_À[ÌRÊÀ_ÈÓKÂÌeÂ:Ðe%äCÂDÈKÂ:NÒ/Æ

25 Sep 2007: A general model for shallow aquifers in the Bengal Basin. Last Glacial Maximum (>=18 Ka). ... Early Holocene transgression (8 - 11 Ka). Mid-Holocene marine flooding and channel-fill (6 - 8 Ka).

25 May 2007: Technical ReportNumber 479. Computer Laboratory. UCAM-CL-TR-479ISSN 1476-2986. The interaction betweenfault tolerance and security. Geraint Price. December 1999. 15 JJ Thomson Avenue. Cambridge CB3 0FD. United Kingdom. phone 44 1223 763500.

13 Nov 2007: Many models adopt a hydrostatic as-sumption such that ka 1, consistent with experimental re-sults of Pouliquen and Forterre.10. ... There are two key parameters, the Earth pressure coeffi-cient ka, which Larrieu et al.

17 Sep 2007: Anuj Dawar September 2007. 31. Method of Locality. • Suppose we have a function, associating a parameter kA N with each. ... g(l,kA)nc. for some computable function g and some constant c. • Let C be a class of structures of bounded local k, i.e.

14 Feb 2007: w" 0YcWÊi RSRQk P9ß W RSTurq ß RXjRX4"z" iUWRQYaEWzÖU P kà]w6mfE P __¥WdfIWUdqlRQkb P w9rIT_U_ cdklmf)¥ P zKRXKRQVwÉ"YÛi RQUYZRQiU P RQkb P U]kEkkb[UY_jWhzw" ... Kà] RQC}RKWdfWUdRXK¥4[U RQT]wWjÖ P kÎ]w ]RQU P [Ua._ c_}RQRXj}g 0YcWU PQP