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1)  flow apophyses
流脊
1.
In the case of a general shearing, the porphyroclasts can either rotate backwards or forwards towards the two eigenvectors or the flow apophyses (non-rotated orientations).
一般剪切作用下,碎斑或顺剪切作用方向向前或逆向旋转向两特征方向或流脊(非旋转方向)靠拢。
2)  in-ridge refluence
脊内回流
3)  spinal cord blood flow
脊髓血流
1.
Relevant research of spinal cord blood flow and the evoked potential by the extramarrow impacting
脊髓髓外冲击负荷后脊髓血流与诱发电位变化的相关研究
2.
The differences of the changes of spinal cord blood flow(SCBF), somatosensory evoked potentials (SEP) and neurogenic motor-evoked potentials (NMEP) were compared in thesetwo groups with the same distract.
观察常压及控制性降压水平下相同程度牵拉损伤后脊髓血流(SCBF)、体感诱发电位(SEI,)、神经源性运动诱发电位(NMEP)改变的差异。
3.
Methods:①The effect of ET1 on spinal cord blood flow(SCBF) was observed after intrathecal administration of 10 ng ET1.
方法 :1鞘内注射 ET 110 ng,观察外源性ET 1对正常大鼠脊髓血流 (SCBF)的影响。
4)  tidal sand ridges
潮流沙脊
1.
Based on the shallow seismic profile and the analysis of sediment from surface of the seabed, the tidal sand ridges offshore the eastern Shandong Peninsula have been preliminarily studied on the configuration, formation condition, sediment source and formation age.
根据浅地层地震剖面和海底表层沉积物的分析,对山东半岛东部近岸潮流沙脊的形态、形成条件、物质来源及沙脊的形成时代进行了初步研究,认为潮流沙脊形成于全新世中期(约6。
2.
The tidal sand ridges in the East China Sea and the sand ridges in the Celtic Sea are all large-scale and deep water sand ridegs on open continental shelf, and were formed in the postglacial sea level rise period.
东海潮流沙脊与凯尔特海沙脊均为开阔陆架上的大型深水沙脊,它们都形成在冰后期海面上升时期。
3.
Ancient tidal sand ridges during the early stage of transgressions in deglaciation are known from bed form data got from the east side of the South Yellow Sea,shallow stratigraphic profile and drill YSDP 102.
南黄海东侧底形资料、浅地层剖面和 YSDP- 10 2钻孔揭示了冰消期海侵初期的古潮流沙脊群 ;南黄海QC2孔上部岩心又揭示了全新世中期的埋藏古潮流沙脊群 ;842 2柱状岩心补充了若干现代南黄海沙脊群——苏北岸外辐射状沙脊群的特征。
5)  tidal sand ridge
潮流沙脊
1.
Tidal channel and tidal sand ridge facies is the dominant facies of the tidal-delta.
前者发育在湾西侧,形成了河口沙坝和分流间湾等沉积相;后者分布在湾口两侧,以潮道和潮流沙脊为主要特征。
2.
The East China Sea(ECS) shelf is characterized by gentle topography, large amount of sediment supply, high settling rate and strong dynamic field, and the tidal sand ridges are well developed and distributed on the ECS shelf.
东海陆架以宽平的地形、充分的陆源沉积物供应、快速沉降和强动力场为特征,中外陆架发育大规模潮流沙脊地貌。
6)  Liaodong shoal
潮流脊
1.
In this paper, the state of the flow field, especially the characteristics of thetidal current movement, in Liaodong shoal are analysed based on the diurnal continuous observations of the flow at several statins.
并初步探讨了潮流运动与辽东浅滩潮流脊发育的关系。
补充资料:脊脊
1.混乱;互相践踏。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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