Climate Change Data Portal
DOI | 10.1016/j.palaeo.2019.01.003 |
Aeolian accumulation: An alternative origin of laterite on the Deccan Plateau; India | |
Liu X.; Mao X.; Yuan Y.; Ma M. | |
发表日期 | 2019 |
ISSN | 0031-0182 |
起始页码 | 34 |
结束页码 | 44 |
卷号 | 518 |
英文摘要 | Laterite is ubiquitous in India and has been extensively studied. However, it is still controversial with respect to its origin, definition, classification, and implications in paleoclimate, tectonic history and topography evolution. Of those, the origin of laterite, either in situ weathering of protoliths or weathering of allochthonous input, is the most critical to address. The ca. 25-m-thick laterite (duricrust) capping the Deccan Plateau is conventionally hypothesized to derive from in situ weathering of the topmost basalt. However, this thick laterite lacks upward progressive weathering which is characteristic of lateritic profile. Instead, it displays: 1) homogeneity in weathering intensity through the duricrust; 2) a clear unconformable contact of laterite with red clay, which together suggests that this thick laterite is genetically unrelated to in situ weathering of the topmost basalt. Lines of evidence in mineralogy, granularity, and geochemistry proved the disconnection between this laterite and basalt, and in contrast, indicated its correlation to aeolian accumulation. In this study the laterite together with the red clay was proposed to derive from aeolian dust accumulation and weathering since 65 Ma within context of Indian plate drifting across the equator from southern to northern hemisphere. © 2019 |
英文关键词 | Basalt; Geochemistry; Grain size; Red clay; Weathering |
语种 | 英语 |
scopus关键词 | basalt; chemical weathering; clay soil; eolian deposit; geochemistry; grain size; Indian plate; laterite; Northern Hemisphere; paleoclimate; protolith; red soil; Southern Hemisphere; Deccan; India |
来源期刊 | Palaeogeography, Palaeoclimatology, Palaeoecology |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/151071 |
作者单位 | Institute of Geography, Fujian Normal University, Fuzhou, 350007, China; State Key Laboratory of Subtropical Mountain Ecology (Funded by Ministry of Science and Technology and Fujian Province), Fujian Normal University, Fuzhou, 350007, China; Department of Environment and Geography, Macquarie University, Sydney, NSW 2109, Australia; College of Geographical Sciences, Fujian Normal University, Fuzhou, 350007, China |
推荐引用方式 GB/T 7714 | Liu X.,Mao X.,Yuan Y.,et al. Aeolian accumulation: An alternative origin of laterite on the Deccan Plateau; India[J],2019,518. |
APA | Liu X.,Mao X.,Yuan Y.,&Ma M..(2019).Aeolian accumulation: An alternative origin of laterite on the Deccan Plateau; India.Palaeogeography, Palaeoclimatology, Palaeoecology,518. |
MLA | Liu X.,et al."Aeolian accumulation: An alternative origin of laterite on the Deccan Plateau; India".Palaeogeography, Palaeoclimatology, Palaeoecology 518(2019). |
条目包含的文件 | 条目无相关文件。 |
个性服务 |
推荐该条目 |
保存到收藏夹 |
导出为Endnote文件 |
谷歌学术 |
谷歌学术中相似的文章 |
[Liu X.]的文章 |
[Mao X.]的文章 |
[Yuan Y.]的文章 |
百度学术 |
百度学术中相似的文章 |
[Liu X.]的文章 |
[Mao X.]的文章 |
[Yuan Y.]的文章 |
必应学术 |
必应学术中相似的文章 |
[Liu X.]的文章 |
[Mao X.]的文章 |
[Yuan Y.]的文章 |
相关权益政策 |
暂无数据 |
收藏/分享 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。