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M组分
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     BaMnO3 was the major active component.
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  m component
Roughly speaking, an (f(x), m)-interleaved sequence is a sequence which is made of (or say, interleaved by)m component sequences with a common characteristic polynomial (f(x)(∈ Fq[x]).
      
These observations suggest that the neural activities generating the N1m component in the bilateral auditory cortices may play a role in automatic detection of tonality mismatch based on the pitch analysis.
      
most likely the formation of G2) was only recorded to have taken place in the surface (0-200?m) component of the CV stock from July onwards.
      
No correlation was found between SPARC and "M" component or disease stage.
      
A deficiency of the α2 chain of laminin-2, previously termed merosin or M component, was shown to be responsible for one form of congenital muscular dystrophy (CMD).
      
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The change of hemorheology were observed in 20 patients with coronary heart disease, various high blood viscosity were presented. 10 patients received the therapy with M fraction of naja naja atro, it were compared with the control (10 patients), the high bolld viscosity was remission in therapic section. The author dicusses the effect of M fraction of naja naja atro on the descrease of frbinogen, antithrombotic effect and inhibition platele aggegate function.

观察了20例冠心病的血液流变学的改变,均显示其不同程度的血液高粘滞度。其中10例使用了眼镜蛇毒M组分治疗。与对照组(10例)相比较,治疗组的血液高粘滞度得到缓解。并对眼镜蛇毒M组分的去纤、溶栓以及抑制血小板聚集功能的作用加以讨论。

The sandstone-type kaolin distributed in the middle Jurassic Yanan Formation in Dongsheng is the sandy kaolin which had undergone the change of diagenesis. Petrologically, the ore is a greywacke, high in matrix of clay. The composition of the ore is simple, containing main minerals of quartz and kaolinite, and other minor constituents. The fragments and the clay fraction can be separated from each other easily because of their great difference in grain size and properties. The kaolin has good quality after concentration,...

The sandstone-type kaolin distributed in the middle Jurassic Yanan Formation in Dongsheng is the sandy kaolin which had undergone the change of diagenesis. Petrologically, the ore is a greywacke, high in matrix of clay. The composition of the ore is simple, containing main minerals of quartz and kaolinite, and other minor constituents. The fragments and the clay fraction can be separated from each other easily because of their great difference in grain size and properties. The kaolin has good quality after concentration, for it has low content of the impurities , abundant fine constituent ( <2 μm), and high natural whiteness of the bleached product.

东胜煤田延安组含煤岩系砂岩型高岭土矿石属杂砂岩,基质含量高,矿物组成简单,石英和高岭石分别构成砂岩的碎屑和基质,其它组分含量低.碎屑与粘土在粒度和物性上的差异,使两者易于分离.精选漂白后的高岭土纯度高(Al_2O_3含量达36.4%),细粒(<2μm)组分含量和自然白度均较高,是一种优质高岭土.分选出的石英等尾沙SiO_2含量大于90%,可综合利用.

Nine sediment samples, collected from East Pacific Ocean at the depth of morethan 4200m, are analyzed for REE in < 2μm fractions and bulk sediments by ICP.The results show that the contents of REE in < 2μm fraction and in the bulk aremainly controlled by sediment type, that is, both of REE contents of the bulk and< 2μm fractions in siliceous sediments are higher than those in calcareous sediments.Moreover, the REE content differences between the bulk and < 2μm fraction aredistinct in two types of sediments....

Nine sediment samples, collected from East Pacific Ocean at the depth of morethan 4200m, are analyzed for REE in < 2μm fractions and bulk sediments by ICP.The results show that the contents of REE in < 2μm fraction and in the bulk aremainly controlled by sediment type, that is, both of REE contents of the bulk and< 2μm fractions in siliceous sediments are higher than those in calcareous sediments.Moreover, the REE content differences between the bulk and < 2μm fraction aredistinct in two types of sediments. Compared with the bulk, there are higher totalREE contents (ΣREE) and as values, lower (La / Yb)_N in < 2μm fractions ofcalcareous samples, but lower ΣREE, higher δCe values and (La / Yb)_N in < 2μmfractions of siliceous samples. The studies of element relationship and REE sequentialextraction test show that the changes of sedimentary components, in MnO, Al_2O_3, Fe_2O_3and CaO, are the main causes for the differences. The REE contents of < 2μmfractions in most samples are similar to those of the North America shales, and theδCe ≈ 1 indicates that clay minerals in studied area are mainly terrigenous. Otherwise,there are two samples (5309c and 5270c) in which the δCe values of < 2μmfractions are lower than 0.7. Sample 5309c has many fine foraminifera pieces whichmake < 2μm fraction similar to deep-sea sediment. The lower δCe values of 5270creflect that the area near the site of 5270 may be influenced by hydrothermal (volcanic)activity, and some smectites are formed in authigenesis.

用等离子光谱测定了东太平洋9个深海沉积物样品的小于2μm组分及全岩的稀土元素,结果显示,小于2μm组分及全岩的稀土元素组成均受控于沉积物类型,而二者之间稀土元素组成的差异在钙质和硅质沉积物中呈现出相反的趋势。元素相关分析和稀土元素赋存状态分析表明,这种差异主要由沉积物物质组成的不同所致,表现在化学组成上,主要与MnO、Al_2O_3、Fe_2O_3、CaO含量的变化有关。大多数样品小于2μm组分的稀土组成与北美页岩类似,铈无明显异常,表明研究区粘土矿物主要来自陆源;个别样品小于2μm组分表现为铈负异常,反映出该组分中有较多的自生组分如钙质生物壳体或海水自生粘土矿物存在。

 
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