摘要
The Core NHH01 (35°13’N, 123°13’E) which was recovered in 128 drilling cycles(NHH01-1~128)from the CSYSM,with a water depth of 73 m and an average recovery rate of 91% in this paper has a whole length of 125.64 m.
The authors concluded the reversal may be record of the Gothenburg geomagnetic excursion in this sediment,which provides a new evidence for the occurrence of geomagnetic excursion during the early Holocene and a symbol for further subtle stratigraphic division and correlation of this area since the Late Pleistocene.