High-resolution time-scales are important for the precise correlation of spatially distributed geological records, and further development of process-oriented models used to predict climate change and other terrestrial processes. The extraction of digital line-scan data from images of laminated sediments provides a tool for the rapid and non-invasive analysis of sedimentary records, including sediment and ice cores, and tree ring growth patterns.
CITATION STYLE
Prokoph, A., & Patterson, R. T. (2006). From Depth Scale to Time Scale: Transforming Sediment Image Color Data into a High-Resolution Time Series. In Image Analysis, Sediments and Paleoenvironments (pp. 143–164). Kluwer Academic Publishers. https://doi.org/10.1007/1-4020-2122-4_8
Mendeley helps you to discover research relevant for your work.