The shape of sedimentary particles contains information useful to recover the ancient sedimentary processes in which the particles were transported and eroded. The traditional method to obtain the grain shape property,such as the roundness,is to describe the property by comparing the grain shape to the images of standard particles. Different quantitative methods have been developed to describe the particle shape properties in the past decades. These methods in recent years have become easier to be operated ...
| 
推荐 
点击下列相关研究机构和相关文献作者，可以直接查到这些机构和作者被《中国知识资源总库》收录的其它文献，使您全面了解该机构和该作者的研究动态和历史。
