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岩石

与 岩石 相关的网络例句 [注:此内容来源于网络,仅供参考]

Love, which seems the realest thing, is really nothing at all;a simple gray rock is a thousand times more tangible than love is; and the earth is such a rock, and love only a breeze that dreams over its surface, weightless and traceless.

爱,似乎是最真实的东西,但实际上根本什么也不是;一块素朴的灰色岩石也要比爱实际一千倍;尘世如同岩石,而爱仅仅是掠过它表面的一阵清风,没有重量、了无踪迹。

In view of the following cases:the overall output of the ore and waste of Baiyunebo main stope increases,the output of rock in the stope by railway transportation ends,the rock unload haul distance increases in the west of the stope and the retransportation capacity is not enough,and so on,this article puts forward the design scheme of the transportation system.

文章针对白云鄂博主采场采剥总量增加,采场铁路运输排岩结束,采场西端岩石排卸运距增加和转载能力不足等问题,提出了采场西端岩石运输系统设计方案,并顺利实现,经济效益显著。

Based on a systematic petrographic and geochemical study and a zircon U-Pb SHRIMP age analysis, the authors revealed that the age of ore-hosting volcanics (XC01-1 rhyolitic tuff) is 180.4±3.5 Ma.

对西藏冈底斯带南部雄村铜金矿床的容矿火山岩和外围岩石进行了岩石学、地球化学、锆石年代学研究。

Rhyolitic volcanic rocks are generally characterized by rich alkali, silicon, aluminum,and poor calcium, magnesium. They have relatively high Rb,Th and rather low Ba,Sr,Ti,P,and exhibit obviouslv negative europium anomaly (δEu=0.16~0.44).The εNd values of the rhyolitic volcanic rocks range from -5.93 to -2022.Basalts and rhyolites in different cycles show clear geochemical variance.

流纹质岩石总体具富碱、富硅、富铝,贫钙、贫镁特征,其Rb、Th等元素的含量较高,而Ba、Sr、Ti、P等元素含量则明显偏低,并具显著的铕负异常(εEu=0.16'0.44),岩石的εNd值变化于-5.93~~-2.22.I、II旋回玄武岩和流纹岩在地球化学特征上均具明显变异。

Xiangshan volcano-intrusive complexes is the wall rock of the biggest volcanic-rock uranium ore deposit in China, and the main body is rhyolitic porphyroclastic lava, accompanied by hypahyssal or ultra-hypabyssal intrusive rocks such as dacite-porphyry and granite-porphyry Jiulongzhang volcano-intrusive complexes are dominantly rhyolitic welded tuff, accompanied by dacite-porphyry and quartz monzonite-porphyry, and so on, and the uranium resources are being assessed.

相山火山-侵入杂岩是华南地区最大的火山岩型铀矿赋矿围岩,其主体岩石为流纹质碎斑熔岩,浅成-超浅成侵入岩有英安斑岩、花岗斑岩等;九龙嶂火山-侵入杂岩的铀资源潜力尚待评价,主体岩石为流纹质熔结凝灰岩,浅成-超浅成侵入岩有英安斑岩、石英二长斑岩等。

The purpose of paper is to describe the petrology character of outcrop sandstones and core sandstones and judge their roke type, compare the similarities and differences of autogenetic mineral、diagenesis types、intergrowth sequence、diagenetic facies、diagenetic phase of outcrop sandstones and core sandstones, provide academic precondition condition for studying better reservoir in studied region.

本次论文的研究目的是描述露头砂岩和岩芯砂岩岩石学特征并判断其岩石类型,比较露头砂岩与岩芯砂岩在自生矿物、成岩作用类型、共生序列、成岩相、成岩阶段以及成岩流体演化方面的异同,为研究区有利储层的研究提供理论前提条件。

Curves of grain size distribution for debris flow conglomerates have multiple modes and hence wave sinuously.

颗粒流沉积与之类似,但岩石中基质甚少,砾石之间只充填少量沉积期后渗入岩石中的铁质和粘土矿物等胶结物。

In the course of program designing, OLE mechanism and Graph for Windows have been used to generate specific geological triangular chart from computer instead of manual work in before. By using PowerBuilder 7, inquiry through a clue of combination of conditions including structural tree, strati graphic tree, well number tree and sample number tree is realized, which meets the thinking way of geologists.

在程序设计方面,针对岩石名称分类复杂、量化定名烦琐的现状,采用OLE机制和Graph for windows图形工具,对岩石含量数据进行相对数值转换,完成了平面上呈三角形排列的三个直角坐标系统的叠加,避免了人工绘制地质三角图随意性大、精确度低的问题,极大地提高了工作效率。

The sand body of channel in the middle sublacustrine fan has good porosity and is favorable reservoir.

利用东濮凹陷桥口地区的地质、测井和化验分析资料,从沉积微相、成岩作用、岩石结构等多方面入手,对其储层物性特征和控制因素进行了研究,指出桥口深层气藏湖底扇中扇辫状水道砂体物性较好,为有利储集层;该储层孔隙类型以次生溶蚀粒间孔隙为主,岩石粒度较细、分选中—差、以点—线接触为主;片状或弯片状喉道所占份额较大,造成储层低孔低渗;受溶蚀和交代作用的影响,部分层位次生孔隙发育,深层中也存在物性较好的储层。

Therefore, its U-Pb ages are likely to yield the age of metamorphic crystallization rather than resetting by simple diffusion, such that metamorphic titanite may preserve complicated U-Pb system that contains information of the whole metamorphic history of the rock, which can be revealed by in situ U-Pb dating, e.

由于榍石的组成元素均为岩石中的主要元素,很容易与其它矿物、熔体及流体发生反应,所以榍石的U-Pb年龄记录的更可能是结晶年龄,而不是简单的扩散重置年龄;也因为它容易反应,变质榍石复杂的U-Pb体系可能记录了岩石的整个变质历史信息。

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