| 1. | A research for emplacement mechanism and structure of yuanshishan granitoid
广西圆石山花岗岩体构造与侵位机制初探 |
| 2. | A new technology intensified by magnetic field for leaching of granitoid weathing crust strain amass - type rare earth ores
风化壳淋积型稀土矿磁场强化浸出工艺 |
| 3. | East qinling - dabie mountains ; lithosphere delamination ; granitoid ; uhpm ultra - high pressure metamorphite
东秦岭大别造山带岩石圈拆沉花岗岩类超高压变质岩 |
| 4. | Groundwater from the granitoid weathering crust is broadly distributed in southern china
花岗岩风化壳地下水广泛分布于我国华南地区，是当地群众的主要饮用水源。 |
| 5. | During the weathering of granite , groundwater from the granitoid weathering crust have special chemical compositions
花岗岩的风化过程，使其风化壳地下水具有比较特殊的水化学组成。 |
| 6. | The paleoproterozoic wangjiahui granitoid intrusion , west segment of wutai mountains , consists mainly of quartz monzodiorite , granodiorite , monzogranite and adamellite
五台山西段王家会古元古代花岗岩侵入体主要由石英二长闪长岩花岗闪长岩和二长花岗岩组成。 |
| 7. | In this thesis , we research into the geochemical data of the groundwater from the granitoid weathering crust of the fogang granite in baisha region , guangdong province
本文研究了广东省白沙地区花岗岩风化壳地下水的水化学特征，特别是与花岗岩的风化过程有关的稀土元素含量及其分布模式。 |
| 8. | Our results indicated that ree concentrations of groundwater within the granitoid weathering crust in baisha area are high relative to many groundwater samples within granite weathering crust worldwide
研究结果表明，白沙地区花岗岩风化壳地下水的稀土含量偏高，最高达到114 g / l ，比世界其他地区高1 - 2个数量级。 |
| 9. | The present lake wall of stone and granitoid was not then in place , but the road had been well laid out , the intermediate spaces of lawn were lovely to look upon , and the houses were thoroughly new and imposing
在北区沿着现在的北湖滨路已建起了一批漂亮的府郏那个湖当时还没有用石块和花岗岩铺的湖堤。井然有序的道路把草坪分隔成一块块的，看上去很悦目，簇新的府第十分气派宏伟。 |
| 10. | 2 . 6 2 . 7ga , these granitoids are most likely to be derived from the partial melting of hybrids both 2 . 6ga metavolcanic materials in archean wutaishan magmatic arc and older continent crustal materials under lower than 1 . 2gpa . petrological and geochemical characteristics of wangjiahui granitoid intrusion suggest that is probably fored under post - collisional tectonic background
2 . 1ga在- 3 . 82 - 2 . 80范围，表明王家会古元古代花岗岩最有可能形成于大约2 . 6ga五台山大洋岛弧火山岩物质和更老的陆壳物质在 |
