Items where Author is "Kong, Gee Soo"

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Number of items: 3.

Patterson, MO, McKay, R, Naish, T, Escutia, C, Jimenez-Espejo, FJ, Raymo, ME, Meyers, SR, Tauxe, L, Brinkhuis, H, Klaus, A, Fehr, A, Bendle, JAP, Bijl, PK, Bohaty, SM, Carr, SA, Dunbar, RB, Flores, JA, Gonzàlez, JJ, Hayden, TG, Iwai, M, Katsuki, K, Kong, GS, Nakai, M, Olney, MP, Passchier, S, Pekar, SF, Pross, J, Riesselman, CR, Röhl, U, Sakai, T, Shrivastava, PK, Stickley, CE, Sugasaki, S, Tuo, S, van de Flierdt, T, Welsh, K, Williams, T and Yamane, M (2014) Orbital forcing of the East Antarctic ice sheet during the Pliocene and Early Pleistocene. Nature Geoscience, 7(11). 841-847. doi:10.1038/ngeo2273 PANGAEA Supplementary Data

Cook, CP, van de Flierdt, T, Williams, T, Hemming, SR, Iwai, M, Kobayashi, M, Jiménez-Espejo, FJ, Escutia, C, González, JJ, Khim, BK, McKay, RM, Passchier, S, Bohaty, SM, Riesselman, CR, Tauxe, L, Sugisaki, S, Galindo, AL, Patterson, MO, Sangiorgi, F, Pierce, EL, Brinkhuis, H, Klaus, A, Fehr, A, Bendle, JAP, Bijl, PK, Carr, SA, Dunbar, RB, Flores, JA, Hayden, TG, Katsuki, K, Kong, GS, Nakai, M, Olney, MP, Pekar, SF, Pross, J, Röhl, U, Sakai, T, Shrivastava, PK, Stickley, CE, Tuo, S, Welsh, K and Yamane, M (2013) Dynamic behaviour of the East Antarctic ice sheet during Pliocene warmth. Nature Geoscience, 6. 765-769. doi:10.1038/ngeo1889 PANGAEA Supplementary Data

Stocchi, P, Escutia, C, Houben, AJP, Vermeesen, BLA, Bijl, PK, Brinkhuis, H, DeConto, RM, Galeotti, S, Passchier, S, Pollard, D, Klaus, A, Fehr, A, Williams, T, Bendle, JA, Bohaty, SM, Carr, SA, Dunbar, RB, Flores, JA, Gonzàlez, JJ, Hayden, TG, Iwai, M, Jiménez-Espejo, FJ, Katsuki, K, Kong, GS, McKay, RM, Nakai, M, Olney, MP, Pekar, SF, Pross, J, Riesselman, C, Röhl, U, Sakai, T, Shrivastava, PK, Stickley, CE, Sugisaki, S, Tauxe, L, Tuo, S, van de Flierdt, T, Welsh, K and Yamane, M (2013) Relative sea-level rise around East Antarctica during Oligocene glaciation. Nature Geoscience, 6(5). 380-384. doi:10.1038/ngeo1783

This list was generated on Sat Dec 21 19:26:40 2024 CET.