| 1. | Syn - collisional plutonic rocks aie composed of granodiorite and adamellite , which exposed al
由于极度艰苦的工作条件限制，本区研究程度极低。 |
| 2. | The pot shaped peak is formed along the joints and fissures with the weathering and eroding of adamellite formed 2 . 4billion years ago
24亿年左右形成的古元古代二长花岗岩，沿节理裂隙风化剥蚀后形成的壶状山峰。 |
| 3. | The pivilion is lying on the adamellite of craggedness with freely ravins . it ' s the best place to look at the sunrise
望海楼所在地主要岩性为24亿年左右形成的二长花岗岩，山势陡峭，沟壑纵横，是蒙山观日出的最佳之处。 |
| 4. | The sight of narrow sky is formed by long - term weathering and eroding of rainwater along the plumb joints and fissures developing in adamellite of 2 . 4billion years ago
24亿年左右形成的二长花岗岩垂直节理裂隙在风化和雨水等作用下形成一线天景观。 |
| 5. | The main diagenetic stage and relevant rock types are the middle proterozoic assemblage of gneissoid granodiorite - adamellite and the sinean schistosity diorates
主要成岩期及代表性岩类有：中元古界为片麻状花岗闪长岩二长花岗岩，震旦纪为片理化闪长岩。 |
| 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 the area without magma mingling or with weak magma mingling , the host rock is dominated by porphyaceous adamellite showing normal granite fabric
无岩浆混合作用或岩浆混合作用较弱区段，寄主岩石以似斑状二长花岗岩为主，显示正常的花岗岩结构构造岩浆混合作用强烈区段。 |
| 8. | Shiding means the stone looks like an ancient cooking vessel , which is formed by the differential weathering of strong upper and weak lower of adamellite formed 2 . 4billion years ago
24亿年左右形成的二长花岗岩发生差异性风化后，下部风化剥蚀强烈，上部风化剥蚀较弱，形成石鼎。 |
| 9. | The peak looks spectacular like a suddenly waked lion to rush out of the mountain , which is formed by sphericity and differentiating weathering of adamellite of 2 . 4billion years old
24亿年左右形成的二长花岗球状风化和差异性风化后，形如雄狮猛醒，怒吼着即将出山，气势十分壮观。 |
| 10. | The peak looks like profile feature of a buddha quietly lying on the side , which is formed by sphericity and differentiating weathering of adamellite of 2 . 4billion years old
24亿年左右形成的二长花岗岩组成的山峰，上部岩石发生球状风化和差异性风化后，远观宛如一尊大佛，安静地侧卧。 |
