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1.Based on the study of the planktonic foraminiferal zones, the stratigraphy of the N22 zone of the Pleistocene, N21 and N20 zone of the late Pliocene, N19—N18 zone of the early Pliocene, N17 zone, N16—N15 zone, N14 zone, N13—N9 zone, N8—N7 zone, N6 zone, N5 zone, and N4 zone of the middle Miocene, and the N3 zone of the late Oligocene at the LH-19-4-1 borehole in the neritic province of the northern South China Sea and the ODP site 1148 in the continental slope region of the northern South China Sea are corresponding and can be correlative.
依据浮游有孔虫带的研究,南海北部浅海区LH-19-4-1井和南海北部陆坡区ODP1148站更新世的N22带,晚上新世的N21带和N20带,早上新世的N19—N18带,中新世的N17带至N4带,和晚渐新世的N3带(N3带=P22带)的地层相当,可以对比。收藏指正
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