By studying sediments, we can learn about the origin of the material, the conditions of its transport and the characteristics of its environment of deposition. Observations can be made at different levels:
at individual particle level;
at bed level;
at outcrop level.
KeywordsBoron Sedimentation Shale Cretaceous Stratification
Unable to display preview. Download preview PDF.
© Springer-Verlag Berlin Heidelberg 1983