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Holocene Increase in the Bay Branch of the Monsoon Inferred From δ18O of Speleothems From Central India
Holocene Increase in the Bay Branch of the Monsoon Inferred From δ18O of Speleothems From Central India
2008
M. G. Yadava
Rengaswamy Ramesh
Y. Asmerom
V. J. Polyak
Keywords:
δ18O
Oceanography
Bay
Geology
Holocene
Monsoon
Correction
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