花岗岩

This simple fact, that the granite colours extracted locally are popular in the funerary industry of Europe and elsewhere, has provided the basis of a potentially successful industry.

印度本地的花岗岩颜色特别受欧洲和其它地方殡葬业的欢迎，这就为墓碑业的发达提供一个基础条件。

The bimodal calc-alkaline rock belt consisting of gabbroic -granite may be regarded as a mark of Late Mesozoic large -scale extention tectonics in SE-China.

闽东南辉长岩-花岗岩的双模式钙碱性岩带可作为中国东南部晚中生代大规模拉张构造运动的标志。

Both material source and geodynamical setting forming the Nanling belt were constrained by the Dabie orogenic belt to the north and the Indosinian orogenic belt to the southwest.

南岭构造带发育在强烈褶皱变形的基底之上，发育了华南地区最大规模的早中生代花岗岩和裂谷盆地。

Granite geomorphological landscapes have been important tourism resources.

花岗岩地貌景观已成为重要的旅游资源。

Granite geomorphological landscapes in Henan may fall into nine types, which were mainly formed by internal and external geological agencies.

河南省花岗岩地质地貌景观已成为一种新的重要自然资源，为人类文明和经济社会做出贡献。

Especially, the types of granite geomorphological landscapes in China are not only highly diversified but also superior to those in other countries of the world in aesthetic enjoyment value.

特别是中国的花岗岩地貌景观类型，不仅多样化程度高，而且美学观赏价值优于世界其他各国。

Ore-forming has close relation with rich-alkalescence geotherm and calc alkali syeogranite, which belongs to middle temperature geotherm al beryllium deposit, and formed in Mesozoic Yanshan period.

矿床的形成与富碱性热液和钙碱性正长花岗岩有关，为中温热液型铍矿床，形成于中生代燕山晚期。

The original Seluohe Group contains at least four parts: Late Archean metamorphic rocks (zircon SHRIMP protolith ages 2517~2534 Ma), Late Paleozoic metamorphosed volcanic-sedimentary strata (zircon SHRIMP 252 Ma), Permian gneissic granitic complex (zircon SHRIMP 260 Ma), and Jurassic mylonitized granites (zircon SHRIMP 168 Ma).

原划分的色洛河群至少由4部分组成：新太古代变质火山－沉积地层（锆石SHRIMP年龄为2517~2534 Ma）、晚古生代变质火山－沉积地层（英安岩锆石SHRIMP年龄为252 Ma）、二叠纪片麻状杂岩体（锆石SHRIMP年龄为260 Ma）和侏罗纪糜棱岩化花岗岩（锆石SHRIMP年龄为168 Ma）。

Nalati tectonic belts as the ultimate demise suture of south Tianshan ocean between Tarim plate - Yili-plate, of which basement is composed of lower Proterozoic gneissic metamorphic supracrustal rocks of Nalati rock group and early Proterozoic gneissic granite.

塔里木-伊犁微板块间的南天山洋最终消亡缝合线——那拉提构造带，基底由下元古界那拉提岩群的片麻岩、变质表壳岩及早元古代片麻状花岗岩组成。

Only, in Fred, these lips were not sensual but granitelike.

只是在弗雷德这里，这嘴唇不性感而象花岗岩。

This one mode pays close attention to network credence foundation of the businessman very much.

这一模式非常关注商人的网络信用基础。

Cell morphology of bacterial ghost of Pasteurella multocida was observed by scanning electron microscopy and inactivation ratio was estimated by CFU analysi.

扫描电镜观察多杀性巴氏杆菌细菌幽灵和菌落形成单位评价遗传灭活率。