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Due to lack of technology, trained manpower and precise equipment the country is incurring losses to about 73 percent in cutting marbles and granites out of mountain ranges.

由于缺少工艺,技术熟练的工人和先进的设备,巴基斯坦开采大理石和花岗岩的损失率高达73%。

As a basic rule, some of the lighter styles of granite need to be sealed while many of the darker granites do not need to be sealed.

作为一个基本规则,某些花岗岩需要更轻的样式被密封,而许多更加黑暗的花岗岩不需要被密封。

Comparing with the Presinian migmatitic granites, this Group has higher density and susceptibility.

与前震旦纪混合花岗岩相比,兴华渡口群具有密度高、磁性强的特点。

The results show that the Dangchuan and Shimen granites have magma crystallization ages of 438±3 Ma and 220±2 Ma, respectively.

结果表明,党川花岗岩和石门花岗岩的岩浆结晶年龄分别为438±3Ma和220±2Ma。

A kind of abrasive tool made from epoxy adhesive and Cr2O3 powder has been developed for polishing of granites.

论述了一种环氧树脂抛光磨具的研制过程。该抛光磨具主要由环氧树脂和Cr2O3磨料组成,用于抛光石材表面。

It is the first time that the third epoch intrusive rocks were evidenced to be S granites.

首次提出第三期花岗岩为&同碰撞&S型花岗岩。

In this paper, we introduce the controlled factors of weathering of granites and the characteristics of the major granite landscapes. The mechanism of these landscapes are outlined.

由于其不同大地构造背景,产生了不同的岩浆成分和结构构造以及不同的断裂型式(Pitcher,1983);同时也由于所处的不同的气候环境,导致了花岗岩地貌具有不同的类型。

The relationships between large igneous rock province, mantle plume and petroleum show that there is a low velocity-high conductive layer of mid-crust in the basin and this layer is the main source of oil and gas. Weathered granites and volcanic rocks are the best reservoir beds for hydrocarbon accumulation and the faults are the main migration pathway. It is suggested that granite and volcanic reservoirs be the future exploration targets.

通过研究花岗岩和火山岩油气藏的形成模式,指出大火成岩省、地幔柱与油气的关系表明盆地中地壳的低速-高导层可能是油气的主要来源,而花岗岩、火山岩的风化壳是油气成藏的最佳储集层,断裂则是其最主要的运移通道,花岗岩和火山岩油气藏将是未来勘探的重要目标。

Since the Dabie orogenic belt was affected meanwhile by the delamination of post collision of Indo-Chinese epoch and the subduction toward EuraAsia continent of Izanagi plate, the upwelling of asthenosphere material supplied a lot thermal energy for crust, isobathythem ascented, this made middle and lower crust amphibolite and granulite facies metamorphic and large-scale free water-bearing system and large area migmatites and granites were formed.

在大别造山带印支期碰撞后所产生的拆沉作用和伊佐奈崎板块向欧亚板块的NWW向俯冲作用的共同影响下,软流圈物质上涌,为地壳输送大量的热能,等温面上升,使中下地壳发生角闪岩相或麻粒岩相变质作用和大规模含自由水体系的熔融,形成了大面积混合岩和花岗岩。

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