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碎屑    
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  debris
    Study on the method to reduce the forming of debris of rubber stopper by using No.16 pinhead to puncture vertically into sealed bottle
    减少16号针头垂直穿刺密封瓶时胶塞碎屑形成的方法研究
短句来源
    Method of Reducing of Debris of a Rubber Cork Puncturingthe Lutation Bottles Vertically by Big needle
    大针头垂直穿刺密封瓶时减少胶塞碎屑形成的方法
短句来源
    Experimental Observation of Pinpoint Inclined Plane Orientation Puncture Influencing on Glue Tampon Debris Forming
    针尖斜面不同朝向穿刺影响胶塞碎屑形成的实验观察
短句来源
    The Effective Observation of Reducing the Formation of Debris of a Rubber Cork through Puncturing the Luted Bottles Vertically by the Method of the Oblique Plane of the Needle Top Facing to the Left
    左向法垂直穿刺密封瓶减少胶塞碎屑形成的效果观察
短句来源
    Results In two lots and 4 orientations punctures, glue tampon debris forming rate of left orientation was the lowest one.
    结果 各批号 4种朝向穿刺胶塞均以左向法穿刺胶塞碎屑形成率最低。
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  clastic
The Zhongpu Group is distributed in the Shihuigou area and composed of medium-basic volcanic rocks and volcanic clastic rocks interspersed with cherts, limestones, slates, and metamorphic sandstones.
      
Triassic clastic sedimentary rocks contain Late Paleozoic mantle-derived materials, represented by the Emeishan Permian flood basalts.
      
Many achievements have been made in experimental studies of hydrocarbon migration in the clastic reservoir.
      
It is shown that clastic quartz in the Riphean basal complexes was mainly related to denudation of the Lower Proterozoic platformal cover, whose rocks occur as fragments in the Riphean conglomerates.
      
It was established that the polygenic microscopic gold can be divided into at least clastic, authigenic, and clastic-authigenic types.
      
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  detrital
Elemental and Sm-Nd isotopic geochemistry on detrital sedimentary rocks in the Ganzi-Songpan block and Longmen Mountains
      
Systematic results of major and trace element geochemistry and Sm-Nd isotopic geochemistry on detrital sedimentary rocks of Precambrian to Triassic in the Ganzi-Songpan block and Longmen Mountains are presented.
      
Cenozoic uplift of West Qinling, northeast margin of Tibetan plateau-a detrital apatite fission track record from the Tianshui b
      
Thermochronologic study on the detrital apatite grains from sandstones at Yaodian, near Tianshui, has revealed two rapid tectonic uplift-exhumation events of the source area, which happened at 23.7 and 14.1 Ma, respectively.
      
Fission-track dating of zircon showed that sandstones from this zone contain detrital zircon of several different-age populations.
      
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  debris
Concept and Classification of Coarse Woody Debris in Forest Ecosystems
      
Coarse woody debris (CWD) is generally considered as dead woody materials in various stages of decomposition, including sound and rotting logs, snags, and large branches.
      
Experimental data are analyzed that concern the effect of zoogenic debris on the properties of soddy deep podzolic soils and raw-humus brown soils characteristic of southern taiga forests in the Yenisei region of Siberia.
      
Zoogenic plant debris falling on the ground surface during tree stand defoliation is a short-acting but powerful stimulant of biological activity in the litter; hence, it has a considerable effect on soil properties.
      
The results of experimental studies on the contribution of zoogenic debris to transformation of soil properties in the southern taiga subzone of Central Siberia are analyzed.
      
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  detritus
Representatives of gamasid (three species) and uropodid (two species) mites abundant in storm detritus were used as model species.
      
Unbalanced composition of higher trophic levels results in an unstable functioning of the lake and accumulation of significant amounts of detritus, which is utilized by the abundant microzoobenthic component of the ecosystem.
      
As against zooplankton, the biomass of zoobenthos features much less contingencies with the biomass of microalgae as well as zooplankton, since detritus, higher plant tissues, and small animals are the basis of the diet of benthic organisms.
      
Specific structural features of giant fishbone detritus accumulations, which represent organic phosphate deposits with uranium and rare earth elements, are scrutinized.
      
The obtained results have made it possible to reconstruct paleotectonic and paleogeographic conditions of the formation of orebodies, as well as the mechanism for the accumulation of metalliferous bone detritus.
      
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