کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
9526140 | 1636204 | 2005 | 24 صفحه PDF | دانلود رایگان |
عنوان انگلیسی مقاله ISI
Rock magnetic characterization of pedogenesis under high energy depositional conditions: A case study from the Mio-Pliocene Siwalik fluvial sequence near Dehra Dun, NW Himalaya, India
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کلمات کلیدی
موضوعات مرتبط
مهندسی و علوم پایه
علوم زمین و سیارات
فرآیندهای سطح زمین
پیش نمایش صفحه اول مقاله
![عکس صفحه اول مقاله: Rock magnetic characterization of pedogenesis under high energy depositional conditions: A case study from the Mio-Pliocene Siwalik fluvial sequence near Dehra Dun, NW Himalaya, India Rock magnetic characterization of pedogenesis under high energy depositional conditions: A case study from the Mio-Pliocene Siwalik fluvial sequence near Dehra Dun, NW Himalaya, India](/preview/png/9526140.png)
چکیده انگلیسی
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.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Sedimentary Geology - Volume 177, Issues 3â4, 15 June 2005, Pages 229-252
Journal: Sedimentary Geology - Volume 177, Issues 3â4, 15 June 2005, Pages 229-252
نویسندگان
V. Kumaravel, S.J. Sangode, N. Siva Siddaiah, Rohtash Kumar,