玄武岩层

Towards the east a layer of pleistocenic basalt rests on top of the limestone and about 100 m below the plain that forms the summit there runs a vein of flintstone.

这座山的西边是石灰岩层，其下层是黏土层，在南边和东边是neocenich，接近东边的是pleistocenic 玄武岩层，其余的上面则是石灰岩，以及在像山峰的旷野形状底下约有100公尺的燧石的矿脉。

Towards the east a layer of pleistocenic basalt rests on top of the limestone andabout 100 m below the plain that forms the summit there runs a vein of flintstone.

这座山的西边是石灰岩层，其下层是黏土层，在南边和东边是neocenich，接近东边的是pleistocenic 玄武岩层，其余的上面则是石灰岩，以及在像山峰的旷野形状底下约有100公尺的燧石的矿脉。

The plan is that instead of being released, the gas will be redissolved in cooler water and injected to a depth of up to 800 metres, into suitable basalt formations where, the hope is, it will react to form calcite or dolomite.

这次实验的目标就是将这些原本被释放二氧化碳溶解到冷却的水中，然后注入到800米以下的玄武岩层，并希望通过一系列的反应将玄武岩变成方解石和白云石。

The level moving out of place has certain thickness, the penetration to be good, extends the penetration entire dam area, mostly along angle gravel lava and aphanites basalt contact face growth.

层内错动带多呈缓倾角状，在岩流层中普遍发育，尤其第三岩流层中部(P2β32-2、P2β33)的柱状节理玄武岩层中，错动带的发育程度明显高于其他岩层。

Basaltic underplating has deepened the CMB from 32 km to 42 km. The lower crust beneath Hannuoba consists mainly of two-pyroxene granulites, with minor felsic granulites, noritic granulites, spinel pyroxenites and spinel lherzolites.

该地温梯度线表明，华北克拉通北缘的岩石学壳幔边界很可能位于约42km处，与地震莫霍面近于一致。32-35km处的尖晶石二辉橄榄岩层可能反映了古岩石学壳幔边界的位置，玄武质底垫作用造成岩石学壳幔边界的深移。

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。