泥质的

With this culture Yangshao - Majiayao cultural legacy belonging to the Qijia cultural relics during the transition period, Orange pottery clay pottery in the main, common blue stripes, cord, additional reactors, such as decorative patterns, the shape of the main pots, bowls, extravagant mouth cans, cans monaural, binaural cans, jar and so on.

这种文化带有仰韶-马家窑文化遗风，属于向齐家文化过渡时期的遗存，陶器以泥质橙黄陶为主，常见篮纹、绳纹、附加堆纹等装饰，器形主要有盆、碗、侈口罐、单耳罐、双耳罐、瓮等。

This is why carbonate differs from mudstone in the mechanism of hydrocarbon generation.

碳酸盐岩与泥质岩在生烃机理上的差异可能就在于此。

It can therefore, be deduced that the protolith from which sapphirine was derived is not necessarily magnesiorich pelite.

含假蓝宝石的变质岩石之原岩未必是富镁泥质岩。

The grazing rate of the juvenile polychaete, Neanthes japonicaon microphytobenthos was studied in situ by 14C technique, on the intertidal mudflat in the north of Dingzi Bay (36.6°N, 120.8°E), in May, 1996. The result shows that the individual grazing rate of N.

采用同位素14C现场同步示踪技术，测定了丁字湾北部泥质潮间带不同体长日本刺沙蚕幼年个体对底栖微藻的摄食率。

Found in the contact zone of the shale rock, but also common in crystalline schist.

见于接触带的泥质岩石中，也常见于结晶片岩中。

The microbial properties of artificial soil mixed with brackish dredged sediment,caustic sludge and coal ash were studied,with coastal solonchak and Turbi-Anthric Primosol as the control.

以滨海盐土、扰动人为新成土为对照，就利用海湾泥、碱渣和粉煤灰作为城市园林绿化种植基质的土壤微生物特性进行了研究。

This steatite main elongated diameter not more than 05 meters of tuberculosis or stacked cone-shaped rock in the middle in the mud.

这种冻石主要呈长径不大于05米的结核状或叠锥状产于泥质岩石中。

According to core observation and description, many deformation structures with seismite characteristics are recognized within sandstone and shale sedimentary strata of Paleogene continental faulted basin in Yangxin Subsag, such as micro-faults, earthquake fissures, liquefaction sandstone veins, water-escape structure, vibrational liquefaction deformation structure, seismic pillow structure and associated structure, etc. The vertical sequence of seismites in Yangxin Subsag, in ascending order, is underlying unshocked layer, micro-faults layer, autoclastic shattered breccia layer, vibrational liquefaction deformation structure layer, seismic pillow structure and associated structure layer, liquefied homogeneous layer and overlying unshocked layer, which corresponds to different earthquake intensity respectively.

通过岩心观察和描述，在阳信洼陷古近系陆源碎屑断陷湖盆砂泥质沉积地层中识别出大量具有震积岩特征的变形构造，如微断层和震裂缝、水下岩脉和泄水构造、振动液化卷曲变形构造、震积枕状层及伴生构造等，同时建立了阳信洼陷震积岩垂向序列，自下而上分别是下伏未震层段、微断层层段、震碎角砾岩段、振动液化卷曲变形层段、震积砂枕及伴生构造层段、液化均一层段和上覆未震层段。

The complex resistivity of patial-water saturated shaly sands has been investigated under reservoir condition.

文章研究了泥质砂岩在模拟地层条件下驱替时的复电阻率特性。

Avoidingthe effect of shaly, tuffaceous and oil, this text established the interpretation equation of thetuffaceous sands effective porosity.

考虑泥质、凝灰质和油气的影响，建立凝灰质砂岩有效孔隙度解释方程。

On the other hand, the more important thing is because the urban housing is a kind of heterogeneity products.

另一方面，更重要的是由于城市住房是一种异质性产品。

Climate histogram is the fall that collects place measure calm value, cent serves as cross axle for a few equal interval, the area that the frequency that the value appears according to place is accumulated and becomes will be determined inside each interval, discharge the graph that rise with post, also be called histogram.

气候直方图是将所收集的降水量测定值，分为几个相等的区间作为横轴，并将各区间内所测定值依所出现的次数累积而成的面积，用柱子排起来的图形，也叫做柱状图。