Facies and architecture of unusual fluvial–tidal channels with inclined heterolithic strata
Developments in Sedimentology, ISSN: 0070-4571, Vol: 68, Page: 353-394
2015
- 36Citations
- 54Captures
Metric Options: CountsSelecting the 1-year or 3-year option will change the metrics count to percentiles, illustrating how an article or review compares to other articles or reviews within the selected time period in the same journal. Selecting the 1-year option compares the metrics against other articles/reviews that were also published in the same calendar year. Selecting the 3-year option compares the metrics against other articles/reviews that were also published in the same calendar year plus the two years prior.
Example: if you select the 1-year option for an article published in 2019 and a metric category shows 90%, that means that the article or review is performing better than 90% of the other articles/reviews published in that journal in 2019. If you select the 3-year option for the same article published in 2019 and the metric category shows 90%, that means that the article or review is performing better than 90% of the other articles/reviews published in that journal in 2019, 2018 and 2017.
Citation Benchmarking is provided by Scopus and SciVal and is different from the metrics context provided by PlumX Metrics.
Example: if you select the 1-year option for an article published in 2019 and a metric category shows 90%, that means that the article or review is performing better than 90% of the other articles/reviews published in that journal in 2019. If you select the 3-year option for the same article published in 2019 and the metric category shows 90%, that means that the article or review is performing better than 90% of the other articles/reviews published in that journal in 2019, 2018 and 2017.
Citation Benchmarking is provided by Scopus and SciVal and is different from the metrics context provided by PlumX Metrics.
Book Chapter Description
The sedimentary facies and architecture of Late Campanian fluvial–tidal channels and channel belts of the Neslen Formation are described from the Floy area of the upper Book Cliffs in northeastern Utah using outcrop data. Vertical sedimentary sections in multiple closely spaced canyons, combined with photomosaics and LIDAR data, describe in detail the deposits over an area of about 3 km by 2 km.
Bibliographic Details
http://www.sciencedirect.com/science/article/pii/B9780444635297000110; http://dx.doi.org/10.1016/b978-0-444-63529-7.00011-0; http://www.scopus.com/inward/record.url?partnerID=HzOxMe3b&scp=84978234705&origin=inward; http://linkinghub.elsevier.com/retrieve/pii/B9780444635297000110; http://api.elsevier.com/content/article/PII:B9780444635297000110?httpAccept=text/xml; http://api.elsevier.com/content/article/PII:B9780444635297000110?httpAccept=text/plain; https://linkinghub.elsevier.com/retrieve/pii/B9780444635297000110; https://dx.doi.org/10.1016/b978-0-444-63529-7.00011-0
Elsevier BV
Provide Feedback
Have ideas for a new metric? Would you like to see something else here?Let us know