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10 Apr 2011: 2 Ok5k1. 0ka!0# kk4. e2k4t (24). Evaluating the first few integrals, we find forh# k, h# k1. ... A 5zL4. tk1. 24 (54). whereas the rodlike treatment implies (from Eq.

31 Oct 2011: environmental variability during the Late Quaternary (10 – 30 cal ka), we studied fluvial archives of. ... ka BP (Oldest Dryas, H1 event), solid and liquid discharges decrease whereas aeolian processes.

10 Apr 2011: 2 Ok5k1. 0ka!0# kk4. e2k4t (24). Evaluating the first few integrals, we find forh# k, h# k1. ... A 5zL4. tk1. 24 (54). whereas the rodlike treatment implies (from Eq.

10 Apr 2011: 23). (24). H.N.W. Lekkerkerker I Curvature elasticity o f charged monolayers 325. ... 2 6 ) - ( 2 8 ) to order 1/(Ka) 2 the following expression for the surface potential:.

20 Jan 2011: We now use(2.16) to find. φAB = 2|K|2 KA′B AA′. (1. ... Substituting (2.24) into (2.23) gives the system (2.18) for the1-forms ei.

31 Oct 2011: 24. Erbajeva Margarita, Alexeeva Nadezhda, Khenzykhenova Fedora and Yazykov Alexander. Biostratigraphy of the South-Eastern Siberia. ... data. The most known of them is the problem of the 100-ka Pleistocene climatic periodicity.

10 Apr 2011: 3). vs T = - l/Ka• Recall that this expression refers to the formulation in Eq. ... SI=II-KI() • (24) With these results we can study some of the aspects.

13 Jan 2011: Name Length E Sequence. HP-20 20 )9 HPHP2H2PHP2HPH2P2HPHHP-24 24 )9 H2P2ðHP2Þ6H2HP-25 25 )8 P2HP2ðH2P4Þ3H2HP-36 36 )14 P3H2P2H2P5H7P2H2P4H2P2HP2HP-48 48 )23 P2HðP2H2Þ2P5H10P6ðH2P2Þ2HP2H5HP-50 50 )21 H2ðPHÞ3PH4PðHP3Þ3PðHP3Þ2HPH4ðPHÞ4H.

5 Aug 2011: Although the strong correlationsuggests an almost constant and linear relationship, it actually appears as ifthe earliest part of the record (before about 650 ka) had lower mixing ratios(both absolutely and ... Science 309, 1714–1717.

31 Oct 2011: MammaliaInsectivora. 3 Blarinoides sp. 24 cf. Drepanosorex sp. 15 Talpa minor 9.