| 1. | Reefy boundstone or framework commonly contains large cavities formed through rapid organic growth .
礁块的粘结岩成骨架中通常有大洞，是由于生物快速生成形成的。 |
| 2. | The division of diagenetic stages in carbonate rocks
碳酸盐岩成岩阶段划分 |
| 3. | The division of diagenetic stages in clastic rocks
碎屑岩成岩阶段划分 |
| 4. | The ore - forming spectrum of the himalayan alkali - rich porphyry in northwestern yunnan province
滇西北喜马拉雅期富碱斑岩成矿谱系 |
| 5. | Determination of ore - and rock - forming time of the machangqing porphyry cu deposit , western yunnan province
矿床成岩成矿时限的厘定 |
| 6. | Geochemical characters of mafic - ultramafic swarms in the baimazhai nickel and copper deposit , jinping , yunnan
超镁铁岩侵入体及铜镍硫化物矿床的成岩成矿机制 |
| 7. | Comprehensive evaluation by fuzzy mathematics on hydrocarbon generation potential of carboniferous source rocks in tarim basin
加水模拟条件下升温速率对烃源岩成烃源岩特征的影响 |
| 8. | Geochemical features of sandstones in matoushan formation of dayao copper mine and the diagenesis and mineralization background
大姚铜矿白垩系马头山组砂岩类的地球化学特征及成岩成矿背景分析 |
| 9. | The volcanic rocks evolved from low - k to high - k in composition with time and migrated spatially from north to south
在时间上火山岩成份有从低钾向高钾演化的总趋势，在空间上火山活动有由北向南迁移的趋势。 |
| 10. | 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。 |
