| 1. | Characteristics of dulongjiang granite and magmatism in northwest yunnan
滇西北独龙江花岗岩及岩浆作用特征 |
| 2. | Magmatism and its tectonic significance in the manzhouli - e ergona region
额尔古纳地区岩浆作用及其大地构造意义 |
| 3. | Tectonic enviroments of magmatism in early paleozoic in the north altyn tagh , china
阿尔金山北缘早古生代岩浆活动的构造环境 |
| 4. | The mesozoic magmatism and polymetallic mineralization was caused by interaction between deep - derived fluids and mesozoic multistage tectonic activities
在此基础上，建立了区域中生代构造流体成岩成矿地球化学体化系统模型。 |
| 5. | In conclusion the magmatism caused by lithosphere delamination in east qinling - dabie mountains occurred in the transition from compression to extension in the period of j
总之，东秦岭大别地区岩石圈拆沉所导致的岩浆活动主要发生在j |
| 6. | Complex and superimposed magmatism and hydrothermal processes resulted in the formation of a superlarge gold and polymetallic ore district in the beiya area
北衙矿区复杂多样、多期叠加活动的岩浆与成矿作用，造就了矿区大规模的成矿作用。 |
| 7. | Paleogeographic data suggest the first occurrence of the taihangshan gravity lineament was initially formed during the early cretaceous , which is coeval with the peak of mesozoic magmatism in this region
岩相古地理分析说明太行山重力梯度带的雏形形成于早白垩世，与华北中生代岩浆活动的高峰相吻合。 |
| 8. | Given the fact that mesozoic magmatism was closely related to the lithospheric thinning , it is proposed that the diachronous lithospheric thinning is the main mechanism by which the taihangshan gravity lineament was formed
由于岩浆作用与岩石圈减薄作用密切相关，因此认为华北岩石圈减薄的时空不均一性是形成太行山重力梯度带的重要机制。 |
| 9. | After making detailed research on ore - controlling factors , the author points out that gold deposits in fujian resulted from the various geologic processes such as sedimentation , metamorphism , tectonism and magmatism
详细研究了福建省金矿的金矿的控矿因素，提出省内金矿的形成是沉积作用、变质作用、构造作用和岩浆作用(包括火山作用)的综合结果。 |
| 10. | Since the fault zone had been activated in the later paleozoic , it controlled the evolution of magmatism and metallization belt in taihang mountains . our field workspace is in the northern part of taihang mountains , which is the diagonal area of two main faults
太行山北段是紫荆关断裂带两主断裂斜列重叠部位，通过对该区作详细的野外断裂构造剖面观测，比较详尽地收集了断裂带构造组合资料及构造岩标本。 |
