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Each type can be subdivided into several kinds: textural mixing deposits include rocks mainly composed of terrigenous components and rocks that mostly consist of intrabasinal composition.

每一类可以再细分为多种,其中结构混合包括①陆源组分为主的混积岩,②以内源组分为主的混积岩。

The main lithologic characteristic is that the rock types are dominated by light-colored clastic rocks reflecting the oxidation environment with a low maturity. The grain size distribution and sedimentary structure show that the rocks have the sedimentary characters of both gravity currents and tractional currents. Plant fragments are lacking and bioturbation structures are abundant and cyclic. Sandbodies are distributed in a ring shape.

其主要岩性特征为:岩石类型以反映氧化环境的浅色碎屑岩类为主,成熟度较低,粒度分布和沉积构造反映其兼有重力流和牵引流的沉积特点,植物碎屑贫乏而生物扰动构造丰富且具周期性,砂体呈环带状分布。

The original defined adakitesare sodium igneous rocks, they are tonalite, trondhjemite or (plagioclase-rich) granodiorite in whole-rock chemistry; however, the K-rich "C-type" adakite defined by Chinese scholars are potassic igneous rocks, they are granite, quartz monzonite and (alkali feldspar-rich) granodiorite, etc.

最初定义的埃达克岩是钠质火成岩,其全岩化学成分相当于英云闪长岩、奥长花岗岩和花岗闪长岩;而富钾的&C型埃达克岩&全岩化学成分相当于花岗岩、石英二长岩和花岗闪长岩。

Regarding the density data and acoustic data in logging material as restriction, it also establishes undrilled district log through model seismic inverse, then, calculates elastic constant of rocks, density constant of rocks and even the profile of the following three pressures (pore pressure, caving pressure, fracture pressure). In the end, this thesis can determine safe drilling mud density windows, provide reference for drilling design, guides safe drilling and decreases the occurrence of accident.

将测井资料中的密度数据或是声波数据作为约束条件,通过模型地震反演,构建待钻区域的测井曲线,从而可以用理论和处理手段上比较成熟的测井分析的方法,进行岩石弹性和强度参数的计算,计算地层的三个压力(孔隙压力、坍塌压力、破裂压力)剖面,最终确定安全钻井液密度窗口,为钻井设计提供参考,指导安全钻井,减少钻井事故。

Combinds with several calculating ways of forming ages of rocks (Pb-Pb isochron way, inconsistent line model calculating way and three-stage model calculating way), a way to calculate element content of samples and forming ages of rocks was summarized.

本文主要是研究该法的计算,分析样品中元素量的计算,并结合几种岩石年龄方法(Pb-Pb等时线法、不一致线模式计算法、三阶段模式计算等)的计算,归纳总结出计算样品中元素量和岩石形成年龄的方法。

That is, U-enriched muscovite peraluminous granites are the uranium source for metallogenesis, and the uranium is mainly devided from the parent granite rocks weathered and denudated, not from the hydrothermal solution derived from the parent granite rocks.

即铀含量较高的晚期二云母过铝质花岗岩是铀成矿作用的铀源,而且,铀源主要来源于被风化并剥蚀掉的那部分母岩,而不是来源于热液流体对现存母岩的交代。

Honeycombed rocks refer to the rocks that are covered with holes of different sizes and appear like the honeycombs as a result, for example, the top of the mushroom rock.

坚硬的岩石上因差异侵蚀、风化而布满大大小小的坑洞,犹如蜂窝一般,即称为蜂窝岩,例如蕈状石的头部就是一种蜂窝岩。

The ultramafic rocks outcropped at the Altyn region are all harzburgites. Remant grains of primary minerals have melted residual texture and elastic deformation texture under high temperature and pressure. The whole-rock analyses show their low TiO〓 contents (0.01~0.04%), low Al, Ca and high MgO contents and wide Mg〓 range (89.35~95.57). Rare earth patterns have two types, namely tabacco pipe-shped and LREE-shaped, of which the former is often seen. The chondrite-nomalized Yb values of these analyses are all lower than 1. The spinels have low Ti and high Cr content and most spinels have Cr# higher than 60. All of the above characteristics show that the ultramafic rocks in the Altyn fault zone are components of metmorphic peridotites of ophiolite from depleted mantle source and most ophiolites from this zone belong to supra-subduction zone type ophiolite with a few mid-ocean ridge basalt type.

阿尔金露头区的超基性岩全为方辉橄榄岩,残余的新鲜矿物颗粒发育有熔融残余结构和高温高压下塑性变形结构,全岩分析显示样品TiO〓的含量低,为0.01~0.04%,具有低的Al和Ca,MgO含量高,Mg〓为89.35~95.57;稀土配分型式有两种,即烟斗型和LREE亏损型,前者占绝大多数,Yb球粒陨石标准化后的值全都小于1;尖晶石低Ti高Cr,大部分尖晶石的Cr〓大于60,上述特征说明阿尔金超基性岩是蛇绿岩的地幔橄榄岩成员,来自亏损的地幔源区,阿尔金蛇绿岩大多属于俯冲带之上型蛇绿岩,有少量的大洋中脊型蛇绿岩。

The result shows that when in-place oil with its viscosity higher than 1.0mPa·s percolates through reservoir rocks with permeability less than 1×10~-3 μm~2, both have start-up pressure gradient, and it increases with the decrease of rock permeability and increase of crude oil viscosity, as oil wettability of the rocks increas...

结果表明,粘度大于1·0mPa·s的地层油通过渗透率小于1×10-3μm2的地层岩石渗流时,均具有启动压力梯度,且启动压力梯度随岩石渗透率的减小和原油粘度的上升而增大;岩石的亲油性增强,启动压力梯度增大;含有束缚水的岩样的启动压力梯度大于不含有束缚水的岩样。

Based on the detailed study of seismic tomography image in South China, and according to the geotectonic environment and shape and heat of asthenosphere upwelling, we divided the structure of lithosphereasthenosphere at the Mesozoic upper mantle of Eastern China into three types.(1)Continental platform area (North China platform and Yangtze platform): asthenosphere upwelled along paleorift; over the plume head, the granitic rocks of crust and mantle mixed and correspondingly, Au, Cu, Mo, PbZn, etc. mineralizationconcentrated regions were formed; and at the steep contact belt of asthenosphere and the thick area of lithosphere, mediatebasic complex was formed.(2)Central area of fold zone: asthenosphere was "recumbent" at suitable depth, with adequate heat and in a great extent; by heat conduction, the interior of partial crust remelted, and the crustsource granitic rocks, and correspondingly, W, Sn and rare elements mineralizationconcentrated regions were formed.

在深入研究华南地震层析成像的基础上,按照大地构造环境和软流圈上涌形状和热度,将中国东部中生代上地幔中岩石圈软流圈构造划分为3类:(1)陆台区,软流圈沿古裂陷上涌,其柱头上方形成幔壳混熔花岗质岩及相应Au、Cu、Mo、PbZn等矿集区,并于软流圈与岩石圈厚区之陡接触带形成中基性杂岩及相应Fe矿集区;(2)褶皱带中心区,软流圈在适当深度、热量充足、较大范围内&平卧&,因热传导而致使地壳内物质部分重熔,形成壳源型花岗质岩及相应的W、Sn、稀有元素矿集区;(3)褶皱带边缘区(大兴安岭南部及华南南缘),在软流圈上涌柱上方形成幔源或幔壳混熔的花岗质岩,相应为Cu、Au、PbZn、Mo、Ag矿集区。

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推荐网络例句

I can do simple painting, carpentry and plumbing.

我能做简单的油漆、木工和修水管等工作。

The motivations, notations and outline of this work are also given in this chapter.

从这个意义上讲,这些时滞是无害的。然后用实例说明这三个定理的应用和互不包含性。

American writer known for his droll epigrammatic verse,much of which appeared in the New Yorker.

纳西,奥格登1902-1971美国作家,因写没有固定韵律的幽默诗而闻名,其中大多数发表在《纽约人》杂志上