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3篇 您的检索式:作者名="Lin Hemao"
    题名 作者 年代 出处 被引量
1Holocene sedimentary sequence, foraminifera and ostraeoda in west eoastal lowland of Bohai Sea, China显示文摘Xue Chunting Zhu Xinghua Lin Hemao 1995Quaternary Seienee Review1995,14,:1
2Holocene sed imentary sequence, foraminifera and ostracoda in west coasta lowland of Bohai Sea, China 显示文摘XUE Chunting ZHU Xionghua LIN Hemao 1995Quaternary Science Re view1995,14,:1
3Fossil fauna and transgressive.sequence from core QC2 in the South Huanghai Sea显示文摘According to palaeoenvironmental analysis on the fossil fauna dominated by Foraminifera and Ostracoda, core QC2 contains 8 marine transgressive beds, called (from up to bottom) Transgressive Beds Ⅰ,Ⅱ, Ⅲ, …,Ⅷ respectively. Together with dating data, the transgressive sequence since 1. 7 Ma B. P. has been established, indicating that the core went through middle and late Early Pleistocene, early and late Middle Pleistocene, early and late (Substages A and B) Late Pleistocene and the Holocene transgressions. Within these 8 transgressions, late Middle Pleistocene, early Late Pleistocene and the Holocene transgressions-had rather strong activities proved by shallow sea (of 50 or 20-50 m water depth) deposits in the prime, while 2 of the 8, during middle Early Pleistocene and late Late Pleistocene (Substage A), were much weaker only with supratidal deposits. The transgressive cycles also differ from each other. Transgressions in the Holocene and in Substage B of late Late Pleistocene are made up of 3Zhu Xionghua and Lin Hemao Institute of Marine Geology, Ministry of Geology and Mineral Resources, Qingdao, China 1990Acta Oceanologica Sinica1990,9,4:0
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