| 1. | The ultrabasic bodies are generally concordant intrusions, with related feeder dikes . 超基性岩一般为具有补给岩墙的整合侵入体。 |
| 2. | Stocks, dykes etc. can be placed in simple sequence with the sedimentary rocks . 岩株,岩墙等可以按其与沉积岩的简单顺序放在图中。 |
| 3. | If the surrounding rock is soft and is later worn away, the walls remain and form ridges called dikes . 如果围岩柔软,日后又被剥蚀掉,这种岩壁就下来形成山脊,称为岩墙。 |
| 4. | Such contour lines can be drawn for any structural surface, regular or irregular(e. g. bedding planes, faults, unconformities, dykes, veins or intrusions) . 对于任何构造面,规则的或不规则的(如层面、断层、不整合、岩墙、岩脉或侵入体)都可画出这种等高线。 |
| 5. | The discovery and origin of the round columnar joints in the basic dyke swarms 岩墙群圆柱状节理的发现和成因机制探讨 |
| 6. | Vein dike ein dyke 岩墙矿脉 |
| 7. | The simulation of mesoproterozoic tectonic stress field forming mafic dyke swarms in the central north china craton 华北克拉通中元古代岩墙群形成的构造应力场数值模拟 |
| 8. | The following ti will help you experience flow more often and with greater inte ity every time you touch rock 尽管我已经来到这面岩墙好几百次了,这次的横渡却比之前任何一次都轻松。 ” |
| 9. | The following tips will help you experience flow more often and with greater intensity every time you touch rock 尽管我已经来到这面岩墙好几百次了,这次的横渡却比之前任何一次都轻松。 ” |
| 10. | The round columnar joints show that the dyke swarms are in upper crust brittle tectonic setting , and the western shandong block is brittle extensional in the mesoproterozoic time 岩墙发育圆柱状节理表明岩墙侵位时地块已经处于上地壳脆性构造环境,中元古代鲁西地区是一个脆性伸展的大地构造环境。 |