| LIU Yanguang,OLE Bjφrslev Nielsen,ZHANG Deyu,DU Dewen,JAN Heinemeier,WU Yonghua.Holocene tephra deposits in the northern Okinawa Trough[J].Acta Oceanologica Sinica,2006,(1):78-89 |
| Holocene tephra deposits in the northern Okinawa Trough |
| Holocene tephra deposits in the northern Okinawa Trough |
| 投稿时间：2005-08-27 修订日期：2005-11-18 |
| DOI： |
| 中文关键词: Okinawa Trough Holocene tephra deposits |
| 英文关键词:Okinawa Trough Holocene tephra deposits |
| 基金项目: |
| 作者 | 单位 | E-mail | | LIU Yanguang | College of Marine Geosciences, Ocean University of China, Qingdao 266003, China
KeyLaboratoryofMarine Sedimentologyand Environmental Geology, First Institute ofOceanography, State Oceanic Administration, Qingdao 266061, China
Department of Earth Sciences, University of Aarhus | yanguangliu@yahoo.com.cn | | OLE Bjφrslev Nielsen | Department of Earth Sciences, University of Aarhus | | | ZHANG Deyu | KeyLaboratoryofMarine Sedimentologyand Environmental Geology, First Institute ofOceanography, State Oceanic Administration, Qingdao 266061, China | | | DU Dewen | KeyLaboratoryofMarine Sedimentologyand Environmental Geology, First Institute ofOceanography, State Oceanic Administration, Qingdao 266061, China | | | JAN Heinemeier | | | | WU Yonghua | KeyLaboratoryofMarine Sedimentologyand Environmental Geology, First Institute ofOceanography, State Oceanic Administration, Qingdao 266061, China | |
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| 中文摘要: |
| The mineralogical and geochemical characteristics of sediments of Core CSH1,which was collected from the northern Okinawa Trough,indicate that large amounts of volcanic materials have deposited in the northern Okinawa Trough during the Holocene.On the basis of down-core variations in mineral and element contents of sediments,two layers in the uppermost section of Core CSH1 characterized by high quartz,Na2O,MnO,K2O,uranium contents and low contents of clay minerals,volatiles,Fe2O3,MgO,CaO and strontium,have been identified as the tephra deposits.Systematic grain-size measurements also suggest that sediments from the northern Okinawa Trough are made up of terrigenous materials and volcanic ashes with different proportion during the Holocene.The sediments of tephra layers in Core CSH1 show bi-modal patterns in grain-size distribution with modal grain-sizes of 74.3 and 7.81 μm,respectively.According to the radiocarbon dating on shells of zooplankton foraminifera,two tephra layers in Core CSH1,formed at 7 250 and 10 870 a BP (cal),approximately correspond to the K-Ah tephra[7 300 a BP (cal)] and the eruption of Kuju Volcano (12~10 ka BP),respectively. |
| 英文摘要: |
| The mineralogical and geochemical characteristics of sediments of Core CSH1,which was collected from the northern Okinawa Trough,indicate that large amounts of volcanic materials have deposited in the northern Okinawa Trough during the Holocene.On the basis of down-core variations in mineral and element contents of sediments,two layers in the uppermost section of Core CSH1 characterized by high quartz,Na2O,MnO,K2O,uranium contents and low contents of clay minerals,volatiles,Fe2O3,MgO,CaO and strontium,have been identified as the tephra deposits.Systematic grain-size measurements also suggest that sediments from the northern Okinawa Trough are made up of terrigenous materials and volcanic ashes with different proportion during the Holocene.The sediments of tephra layers in Core CSH1 show bi-modal patterns in grain-size distribution with modal grain-sizes of 74.3 and 7.81 μm,respectively.According to the radiocarbon dating on shells of zooplankton foraminifera,two tephra layers in Core CSH1,formed at 7 250 and 10 870 a BP (cal),approximately correspond to the K-Ah tephra[7 300 a BP (cal)] and the eruption of Kuju Volcano (12~10 ka BP),respectively. |
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