形成带状

Hengshan oval-typed gneisses are the augen, streak and striped gneisses, as a result of the dilatation structures of the parallel shear zone boundary, that is the adding of the mafic intrusive rocks of the mantle materiel, and the part melting and auto differentiation of rocks themselves.

恒山卵形片麻岩区，以平行剪切带边界的扩张构造，即地幔物质镁铁质岩席的添加、岩石自身的熔融和自分异形成的眼球、条纹和条带状片麻岩为特征。

The distribution characteristic of igneous rocks is similar to the magmatic activity in Cordilleran orogen, it is caused by variance of dip angle of subduction slab from 10～20° in Ca.

这种火成岩随时间的带状迁移特征与北美西部科迪勒拉造山带火成活动特征相似，它们都是俯冲板块倾角变化导致岩浆弧迁移形成的。

The CGRP-positive fibers ran dorsoventrally in the MrD and formed a dense band. The CGRP-positive fibers were more densely and widely distributed in the caudal part of the MrD.

结果发现：（1）CGRP免疫阳性纤维在纹状体内存在于纹状体的中部和尾侧，位于尾壳核和苍白球之间，即相当于纹状体边缘区的部位，形成一条明显的背腹方向走行的带状。

Through geothermometry and geobarometry, the temperature and pressure conditions of the three types of amphibolites are calculated, gneissic amphibolites: 597.0℃,0.536Gpa, banded amphibolites: 597.0℃,0.536Gpa, mylonitic amphibolites: 597.0℃,0.536Gpa.

通过地质温压计计算，三种斜长角闪岩及其原岩的形成与变形温压条件具有从升温升压经降温升压到降温降压的变化规律（片麻状斜长角闪岩：597.0 ℃，0.536 Gpa；条带状斜长角闪岩：597.0 ℃，0.536 Gpa；糜棱状斜长角闪岩：597.0 ℃，0.536 Gpa）。

Through geothermometry and geobarometry, the temperature and pressure conditions of the three types of amphibolites are calculated, gneissic amphibolites: 597.0℃, 0.536 GPa, banded amphibolites: 617.3℃, 0.455 GPa, mylonitic amphibolites: 558.8℃, 0.514 GPa.

通过地质温压计计算，3种斜长角闪岩及其原岩的形成与变形温压条件具有从升温升压经降温升压到降温降压的变化规律（片麻状斜长角闪岩：597.0℃，0.536 GPa；条带状斜长角闪岩：617.3℃，0.455 GPa；糜棱状斜长角闪岩：558.8℃，0.514 GPa）。

The main characteristics of the skarn are as follows:(1)occurring as bedded,para-bedded in the contact zone between carbonate and microclastic rock,and its occurrence being accordance to the strata;(2)cut by later vein rock,so having no relation with the magmatic rock on genesis;(3)metasomatic skarn having replacement remnant texture,pseudobreccia structure,while depositional skarn,particulate crystall...

研究表明该夕卡岩的主要特征为：(1)呈层状、似层状赋存于碳酸盐岩和细碎屑岩接触带，产状与地层一致；(2 )被后期脉岩穿切，成因上与岩浆岩无关；(3)喷流交代夕卡岩具交代残余结构和假角砾状构造，而喷流沉积夕卡岩具微粒状结构、雏晶结构和层纹、条纹、条带状构造，反映了二者不同的喷流成因；(4)发育典型的低温夕卡岩矿物组合，其形成温度小于30 0℃；(5 )夕卡岩的稀土配分型式与围岩的一致。

Plant lotus shape, there is the cistern of one store water in the center of; Xie Kuan is banding, green, the brim is smooth without tine; Spicate from the leaf take out in the center of the canister, peduncular and all by green or gules bud piece wrap up, one is formed in top by multichip and gules petal piece the astral form Hua Sui that constitutes generation, floret is born at petal piece in, outside its just are being extended when opening; It is capsule if really, there is graininess seed inside.

植株莲座状，中心有一蓄水的水槽；叶宽带状，绿色，边缘无齿而光滑；穗状花序从叶筒中心抽出，花梗全部被绿色或红色的苞片包裹，在顶端形成一个由多片红色花苞片组合产生的星形花穗，小花生于花苞片之内，开放时才伸出其外；果为蒴果，内有粒状种子。

Formation Mechanism of Band Structure and Phase Selection During Directional Solidification of Peritectic Alloys II.

定向凝固包晶合金带状组织的形成机制及相选择 II。

Summer high temperature season, especially in highly alkaline (pH 8 ~ 9.5) and high-nitrogen low-phosphorus breeding water body, often there will be kind of the large population of blue-green algae in the water to form a layer of green, cloud porphyritic, ribbon objects , commonly known as "water-hua."

盛夏高温季节，尤其是强碱性(pH 8～9.5)和高氮低磷的养殖水体，往往会出现蓝绿藻类的大量繁殖，在水面形成一层绿色、云斑状、带状的物体，俗称&水华&。

Results On conventional CT, pulmonary window revealed widespread intraalveolar calcifications of both lungs concentrating in the subpleural parenchyma of the middle and lower lobes.

结果常规CT表现：肺窗示肺实质内有无数细小散在的粟粒结节，以中下肺的外周部密集，其CT值为200～400HU，多合并不同程度的肺气肿及间质纤维化；纵隔窗示细结节影最密集区常呈沿胸膜的线带状或散在的点簇状钙化，形成&火焰征&及&白描征&。

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。