| 1. | The gabbro dikes are short .
辉长岩岩脉短。 |
| 2. | The micro-gabbro phase is identical with the typical bulawayan dolerite sills .
微辉长岩相与标准的布拉瓦约粒玄岩床相同。 |
| 3. | The massive sulfide contains fragments of barren and mineralized gabbro, and schist .
块状硫化物中含有矿化的和未矿化的辉长岩及片岩碎块。 |
| 4. | Study on fracture pattern of open surface - flaw in gabbro
辉长岩中张开型表面裂隙破裂模式研究 |
| 5. | Calc - alkali gabbro
钙碱辉长岩 |
| 6. | Isotopic age of shijuli gabbro in north qilian mountain and its geological significance
北祁连山石居里辉长岩的同位素年龄及其地质意义 |
| 7. | Petrological characteristics and tectonic implications of the tahe gabbro in the northern part of the great xing ' an range
大兴安岭北段塔河辉长岩的岩石学特征及其构造意义 |
| 8. | All these ductile shear zones are characterized by northward thrusting . the u - pb dating on zircons from the bedded gabbro of the qimanyuter ophiolite melange gives an age of 526 ? 1 ma ( early cambrian )
在其曼于特蛇绿岩的层状细粒辉长岩中获得了锆石u - pb年龄值为526 1ma (早寒武世) ，它被晚奥陶世花岗岩侵入。 |
| 9. | The geochemical characteristics of gabbros from the jinshajiang ophiolitic melange indicate that they were derived from a mantle source different from that of volcanic rocks , which may be a product in the ocean rift in the earlier stage
东竹林蛇绿混杂岩中辉长岩地球化学特征表明，它与火山岩不同源，可能是洋盆裂谷初期的产物。 |
| 10. | The real part of the complex impedance decreases with frequency ; the imaginary part of the complex impedance increases with frequency to the maximum , and then decreases with frequency ; and phase angle decreases with frequency increasing
结果发现辉长岩复阻抗的实部随频率的增加而减小，而虚部随频率增加先增大后减小；相角随频率增加而减小。 |
