地质的

Lou Z H%Jin A M%Zhu R Formation and evolution of the hydrodynamic field in the Songliao basin Acta Geologica Sinic , 2001,1

楼章华%金爱民%朱蓉%蔡希源%高瑞祺论松辽盆地地下水动力场的形成与演化地质学报， 2001，1

The rock mass in the slote is composed of two grades, which have been forced by tectonic stress four times.

由岩性、地貌，地质力学的调查和分析，求得当地岩体曾受四次构造应力作用，边坡岩体分上、下两级。

Systematic geological investigation and stratum section study was approved that no early Carboniferous Brochipoda: Eochoristites, Fusella, Spirifer etc.

系统地质调查和地层剖面研究证实：海南岛南好地区早石炭世南好组选层型剖面、创名地化石点等所报道的早石炭世腕足类：Eochoristites，Fusella，Spirifer等并未发现。

The stratal slices made from the 3-D seismic volume reveal the high-resolution sediment-dispersal patterns and associated depositional systems on the relative geologic time surfaces.

地层切片技术可以在平面上显示相对同一地质沉积时间的沉积分布特征，再结合岩性测井资料可以较准确分析沉积体系。

Results 1 facies and 2 subfacies and 9 microfacies were identified,assemblages of resource rock and reservoir and top seal were clarified.

结果划分出1个相、2个亚相和9个微相，获得了各微相的地质特征和识别标志。

Asthe result, we can see that Chinese modern geological education is of thecharacteristics of adaptability, successiveness, continuing.

因此，我们可以看出，中国的现代地质教育具有社会适应性、继承性和延续性。

Some gold deposits may be superposed by later geological event, and amplification increase.

有的金矿床，可被以后的地质事件叠加、增富、增大。

Based on the analysis of REE geochemical characteristics of different geologic rocks in Pangxidong silver deposit, the genesis of granitic wallrocks and the source of mineralised material are discussed. It indicates that Yingqiao granite belongs to syntectic granite of mixed crust mantle source.

分析了粤西廉江庞西垌银矿床不同地质体岩石稀土元素地球化学特征，对矿床围岩花岗岩的成因以及矿床成矿物质来源进行了讨论，认为英桥花岗岩体为壳幔混合源同熔花岗岩。

China Geology University, Wuhan Industry University, 709 Institute, 105 Institute, Wuhan physics Institute of Chinese Academy of Sciences, the National Earthquake Research Institute, and Hubei Chemical Research Institute all established their developing centers for optics, telemetric, optical material, and applied software engineering.

中国地质大学，武汉工业大学， 709研究所， 105研究所，武汉物理研究所的中科院，国家地震研究所，湖北省化学研究所都设立了发展中心，光学，遥测，光学材料，并应用软件工程。

Combined with mathematics and geological practice, a new expression for calculating true thickness of terrene is deduced.

将数学方法与地质实际相结合，严密推导出一个岩层真厚度计算的新公式。

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。