| 1. | Discussion on management and development of human resources in coal geological system
煤田地质系统人力资源管理与开发探讨 |
| 2. | It is difficult to select assessment factors form the complicated eco - environment geology system and assess its quality
从一个复杂的生态环境地质系统中选取评价因子，进行质量评价是十分困难的。 |
| 3. | Their spatio - temporal behaviors obey the dynamics of self - organized critical processes of geological processes
地质系统是自然界中的一种既十分重要，又异常复杂的开放、远离平衡、相互作用的巨大耗散动力学系统。 |
| 4. | Only when a system po e es natural or artificial boundaries that a ociate the water within it with the hydrologic cycle may the entire system properly be termed hydrogeologic
只有当某一地质系统拥有自然的或人工的界限，将该系统内的水与水文循环起来，这整个系统方能被恰当地称为与水文地质学相关。 |
| 5. | Only when a system possesses natural or artificial boundaries zat associate the water within it with the hydrologico cycle may the entire system properly be termed hydrogeologic
只有当某一地质系统拥有自然的或人工的界限，将该系统内的水与水文循环起来，这整个系统方能被恰当地称为与水文地质学相关。 |
| 6. | Only when a system possesses natural or artificial boundaries that associate the water within it with the hydrologic cycle may the entire system properly be termed hydrogeologic
只有当某一地质系统拥有自然的或人工的界限，将该系统内的水与水文循环起来，这整个系统方能被恰当地称为与水文地质学相关。 |
| 7. | Eco - environment geology system is complicated and its quality has some uncertainty to people ' s acquaintance . so based on the principles of fuzzy mathematics and using exact fuzzy comprehensive evaluation and grey correlative fuzzy evaluation , the quality of eco - environment geology in the upper reaches of minjiang river is assessed in this paper
由于生态环境地质系统的复杂性，且质量的好坏在人们的认识上具有一定的不确切性，因此，本文根据模糊数学的原理，采用确定型模糊综合评判方法、灰色关联模糊评价法对岷江上游生态环境地质质量进行了定量评价。 |
| 8. | And geosystems grow fractally at the edge of chaos . the author deduced and integrated these aspects into a theory of complexity in geosciences named “ dynamics of self - organized critical processes of geological processes ? fractal growth of geosystems at the edge of chaos ” , which is widely applicable to variable geosystems
地质系统位于有序和混沌之间的过渡时空域，即混沌边缘，其中系统呈规则与混沌运动并存和混合的弱混沌动力学状态，并且地质系统在混沌边缘分形生长。 |
| 9. | The contents of this theory are divided into six parts , they are : ( 1 ) self - organized criticality , transient chaos , the edge of chaos and weak chaos ； ( 2 ) the coupling and interactions as well as the coherence and cooperation of multicomponents ； ( 3 ) the fractal dynamics of evolutionary processes ； ( 4 ) the spatio - temporal structures of processes ； ( 5 ) the dynamics of fractal growth ； ( 6 ) the theory of finite - size scaling
将上述命题演绎和整合成一种广泛适用于地质系统的地球科学的复杂性理论，名之为： “地质作用的自组织临界过程动力学? ?地质系统在混沌边缘分形生长” ，并将其内容归纳成6部分： ( 1 )自组织临界性、瞬态混沌、混沌边缘和弱混沌， ( 2 )多组分的耦合与相互作用及其相干与协同， ( 3 )演化过程的分形动力学， ( 4 )作用的时空结构， ( 5 )分形生长动力学， ( 6 )有限大小标度理论。 |
