| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 9526140 | Sedimentary Geology | 2005 | 24 Pages |
Abstract
The assemblage of iron oxides using the rock magnetic ratios of the pedogenic layers in these high energy conditions broadly infer the prevalence of semi-humid to semi-arid climate entirely during the Late Miocene to Early Pliocene period in the HFB with an increased seasonality during early Pliocene. The present approach envisages a great scope for quantitative database under the given setup of high energy conditions that are common in the Mio-Pliocene HFB.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
V. Kumaravel, S.J. Sangode, N. Siva Siddaiah, Rohtash Kumar,