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Glacier response to Holocene warmth inferred from in situ <sup>10</sup>Be and <sup>14</sup>C bedrock analyses in Steingletscher's forefield (central Swiss Alps) by I. Schimmelpfennig, J. M. Schaefer, J. Lamp, V. Godard, R. Schwartz, E. Bard, T. Tuna, N. Akçar, C. Schlüchter, S. Zimmerman
Published 2022-01-01
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