| 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. | Further imbrication, folding and metasomatism of the ultrabasic rocks occurred at this time .
超基性岩的进一步叠瓦作用，褶曲和交代作用发生于这个时期。 |
| 3. | The heat production in rocks due to radioactivity is highest in the acid rocks and lowest in the ultra-basic rocks .
岩石的放射作用热产率以酸性岩类最高，超基性岩类最低。 |
| 4. | The ultrabasic rocks form a complex of large tectonic slices with intercalated slices of sebakwian sedimentary rocks .
超基性岩与塞巴奎沉积岩岩片相间构成一巨大的构造岩片的杂岩体。 |
| 5. | Many ultrabasic bodies in the orogenic association occur along strike faults, which gives a simulated concordant relationship .
与造山运动共生的许多超基性岩体沿着走向断层出露，表现出假的整合关系。 |
| 6. | The parefin 4 chromite claims near the northern end of the csardas thrust again indicate the eastward extension of the thinning ultrabasic sheet from railway block .
靠近萨达斯冲断层北端的帕勒芬4铬矿区又表明从铁路段向东超基性岩席减薄的情况。 |
| 7. | Geochemical and petrological characteristics of mafic and ultra - mafic intrusions in jinbaoshan , yunnan
超基性岩的地球化学特征及其含矿性 |
| 8. | At the same time , it is proved again that jianchaling rock - body intruded in new proterozoic
并佐证了煎茶岭岩体确为新元古代形成的超基性岩体。 |
| 9. | Lattice preffered orientation and seismic anisotropy of ultramafic xenoliths in damaping , hebei province
河北大麻坪超基性岩包体的岩石组构和地震波速各向异性 |
| 10. | The igneous bodies are mainly metasomatic type in china . through zhongtiao circle to yantsi circle , himalaya circle , the magma activitie
与基性、超基性岩有关的铜镍硫化物矿床，从地球物理场上，一般与航磁的感磁场有关。 |
