| 1. | The differences between the conductivities of different kind of rocks are rather small .
不同岩类热导率的差异还是比较小的。 |
| 2. | A consistent zonal arrangement is a constant feature of those complexes that contain olivine-bearing rocks .
稳定的带状排列是这些含橄榄石岩类杂岩的固定特点。 |
| 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 greatest dependence upon temperature is shown by rocks with high conductivities at room temperature e.g. salt .
在室温下，高热导率岩类（如盐类）的热导率对温度的反应最大。 |
| 5. | Conductivities measured at room temperatures must be corrected if they are to be used for rocks at depths greater than about 1000m .
如果它们将用于深度超过1000米左右的岩类，室温下测得的热导率必须校正。 |
| 6. | Another problem in the determination of a good representative value of the conductivity for a given rock type arises from the heterogeneity of the material .
测取给定岩类具有良好代表性热导率数据的另一个问题是材料的不均匀性。 |
| 7. | Porphyry rocks in this belt are intermediate - acid rocks of calc - alkaline series
该斑岩带斑岩属钙?性系列、中酸性岩类。 |
| 8. | Calc alkaline rocks
钙咸岩类 |
| 9. | Pyroclastic rocks are a kind of transitional and complex rocks between lavas and sedimentary rocks
摘要火山碎屑岩是介于溶岩和沈积岩之间的过渡类型岩石，岩类复杂。 |
| 10. | 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。 |
