玄武岩

During 2 million years of warm, wet climate conditions the lower basalt weathered to form a deep red rock called "Laterite".

在两百万年的温暖、潮湿的气候条件下，形成了玄武岩。饱经风霜，深红色的岩石称为"红土"。

In terms of fractal geometry, analyses are performed of the features of grain size of the basalt laterite with and without disperser at the vertical section.

本文借助分形几何理论，探讨垂直剖面上玄武岩红土在加分散剂前后颗粒粒度的分维变化特性。

There is a large-area basalt in the Boloven Plateau Champasak Province, South Laos and intense laterization.

摘 要：老挝南部占巴赛省波罗芬高原分布大面积玄武岩，红土化作用强烈。

The first type, kamafugite, is plagioclasefree, consisted of Tirich phlogopite, melilite, leucite and nephelite. They have lower contents of SiO2 and Al2O3, but have high TiO2, CaO, MgO contents and K/Na and Mg# ratio whereas the second type, potassic trachybasalt, is abundant in plagioclase and contains no phlogopite, melilite, leucite and nephelite. They have higher SiO2, Al2O3,(Na2O+K2O), and lower TiO2, CaO, MgO, and K/Na and Mg#, in comparision to the first type of rocks.

钾霞橄黄长岩是一种不含斜长石，但普遍含有高钛金云母、黄长石、白榴石、霞石的岩石，全岩化学成分具低SiO2和Al2O3，富TiO2、CaO、MgO和高K/Na、高Mg#值的特征；钾质粗面玄武岩含有大量斜长石但是缺乏高钛金云母、黄长石、白榴石和霞石，全岩化学中SiO2、Al2O3明显高于前者，而TiO2、CaO、MgO、K/Na和Mg#值要比钾霞橄黄长岩低。

Cenozoic basalts in Yangyuan, Hebei, located in the west of the Daxing′anling-Taihangshan gravity lineament, contain abundant peridotite and pyroxenite xenoliths.

位于大兴安岭-太行山重力梯度带西侧的阳原新生代玄武岩中含有大量橄榄岩和辉石岩包体。

Below 1100℃, the amount of argon released from irradiated samples is in an order of: plagioclase rock＞striped migmatite＞granite＞garnetiferous mica schist＞calciummuddy shale＞basalt.

在1100℃之前，辐照样释放的氩气量按顺序排列为：斜长岩＞条带状混合岩＞花岗岩＞含石榴石云母片岩＞钙泥质页岩＞玄武岩。

The conclusion tests to be that they all have well mineralize effect. It indicates that with low IM value cement raw materials has a better effect than higher one.

研究发现玄武岩和矿渣都具有较好的矿化效果，同时也发现用二者作为矿化剂使用时不适用于高铝率的生料配比。

The traditional mineralizer fluorine and sulfur are replaced by basalt and slag.

矿化剂选用了玄武岩和矿渣替代了传统的氟硫矿化剂。

The diffusion coefficients of moisture in monzonite and basalt are 48.09×10^(-8)m^2/s and 3.74×10^(-8)m^2/s, respectively.

计算得二长岩和玄武岩中的水气扩散系数分别为48.09×10^(-8)平方公尺/s和3.74×10^(-8)平方公尺/s。

Intrinsic permeability and porosity of the monzonite and basalt are 0.0047×10^(-3)μm^2, 0.0081×10^(-3)μm^2 and 1.58% and 0.24% respectively.

二长岩及玄武岩核心区的渗透率分别为0.0047×10^(-3)μm^2和0.0081×10^(-3)μm^2，孔隙度分别为1.58%和0.24%。

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。