| 苏北陆区潮成沙体的磁组构特征及沉积环境 |
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| 引用本文： | 范代读,张家强.苏北陆区潮成沙体的磁组构特征及沉积环境[J].沉积学报,1999,17(4):601-607. |
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| 作者姓名： | 范代读 张家强 |
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| 作者单位： | 同济大学海洋地质教育部开放研究实验室 上海 200092 |
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| 摘 要： | 苏北陆区潮成沙体磁组构分析表明,与苏北海域辐射沙洲一样,砂体也形成于辐聚辐散的潮流场。沉积物在辐聚辐散的潮流场中经潮流、波浪作用,K、P值普遍较大,在垂向和横向上变化显著,可能是沉积动力增强的反映。P、F值相关性较好,而P、L值之间的相关性差,反映沉积环境较稳定。q值小,以正常沉积为主,出现q>07的风暴事件沉积。
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| 关 键 词： | 磁组构 潮成沙体 冰后期 |
| 收稿时间： | 1998-10-06 |
Magnetic Fabric Characteristics and Sedimentary Environment of Subaerial Tidal Sand Body in Subei Area |
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| FAN Dai-du\ ZHANG Jia-qiang\ LI Cong-xian.Magnetic Fabric Characteristics and Sedimentary Environment of Subaerial Tidal Sand Body in Subei Area[J].Acta Sedimentologica Sinica,1999,17(4):601-607. |
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| Authors: | FAN Dai-du\ ZHANG Jia-qiang\ LI Cong-xian |
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| Institution: | Laboratory of Marine Geology of State Education Commission.Tongji University,Shanghai 200092 |
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| Abstract: | There exists a sub-recent buried tidal sandbody system among standplain muddy deposit areas,with a fanshape stretching towards east from Dongtai and similar to that of the radial tidal sand ridge pattern in the southern Yellow Sea.The area of subaerial tidal sandbody system is about 3 000 km\+2.Tidal sedimentary structures,such as muddy streak,flaser structure and bi-direction cross-bedding,show tidal genesis of the sandbody system.The tidal sand strata are underlain by littoral unit or terrigenous hard clay and overlain by tidal flat deposits.Magnetic fabrics are measured and analyzed at two representative drilling cores,Tongshang and Xinhai,which have penetrated tidal flat strata,tidal sand body and hard clay.Two drilling cores ard sampled successively.The samples are measured and magnetic fabric parameters K、P、F、L and q are calculated,then successive curves of these magnetic fabric parameters are acquired.These curves show that K、P、F、L and q of the tidal sand body demonstrate an apparent difference from those of underlain paleosol and overlain strata,and lower and upper boundaries of the tidal sand body can be defined by the curves.There are abrupt changes of K、P and F at the boundary between tidal sand strata and the underlying paleosol,with sharply increasing of these parameters in the tidal sand strate.Thus.it can be inferrd that environmental energy in the tidal sand strata is abruptly increased.Under the strong and stable tidal current,the deposition is coincided with hydrodynamics and most of q is less than 0.5 in the tidal sand strata.However the hard clay(paleosol) formed in low energy environment of floodplain contains a lot of sedimentary units with q higher than 0.7,which corresponds to a quick deposition The tidal sand body unit transits gradunally upward to tidal flat deposits,but the boundary between them is still cleraly discernable by the magnetic fabric curves.Smaller K and P reflect hydrodynamic decline from the tidal sand body unit to tidal flat deposts.Abrupt variation of K and P within the tidal sand strata may reflect superimposition of sand ridge and tidal current trough depositional units in vertical profile,which shows micro-hydrodynamic changes on the tidal ridge and in the trough.Horizontally,that values of P、K in core Xinhai are higher than those in core Tongshang shows variations of hydrodynamics matching the convergent-divergent tidal current field in the study area.Contents of heavy minerals also show the similar tendency of tidal current changes.Besides,variations of K and content of varied magnetic minerals among heavy mineral also indicate multi-provenance of the study area,with“the Yellow River source” prominent at north and “the Changjiang Rover source” at south. |
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| Keywords: | magnetic fabric\ tidal sand body\ postglacial period\ sedimentary environment |
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