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Titlebook: Mantle Plumes and Their Effects; Mainak Choudhuri,Michal Nem?ok Book 2017 The Author(s) 2017 Hotspot Activity.Intra-plate Magmatism.Crusta

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樓主
發(fā)表于 2025-3-21 17:31:14 | 只看該作者 |倒序瀏覽 |閱讀模式
書目名稱Mantle Plumes and Their Effects
編輯Mainak Choudhuri,Michal Nem?ok
視頻videohttp://file.papertrans.cn/624/623445/623445.mp4
概述Describes methods for estimating the uplift history of a region due to plume activity.Presents methods that can be applied irrespective of the cause of hotspot activity.Outlines the ongoing debate on
叢書名稱SpringerBriefs in Earth System Sciences
圖書封面Titlebook: Mantle Plumes and Their Effects;  Mainak Choudhuri,Michal Nem?ok Book 2017 The Author(s) 2017 Hotspot Activity.Intra-plate Magmatism.Crusta
描述.This book presents a brief synopsis of the current academic understanding of the plume hypothesis, its surface manifestations and its shortcomings. It also describes methods for estimating the uplift history of a region due to plume activity. It discusses different models for the elastic properties of the lithosphere and their estimation as a background for plume emplacement, and introduces the plume hypothesis, describing the major plume types and their effect on the lithosphere. Two chapters are dedicated to the dynamic and permanent topography produced by an impinging plume head below the lithosphere and its estimation. It also presents the historical background of the plume hypothesis, its criticisms and alternatives..
出版日期Book 2017
關(guān)鍵詞Hotspot Activity; Intra-plate Magmatism; Crustal Uplift; Magmatic Underplating; Flexural Moat; Plume Hypo
版次1
doihttps://doi.org/10.1007/978-3-319-44239-6
isbn_softcover978-3-319-44238-9
isbn_ebook978-3-319-44239-6Series ISSN 2191-589X Series E-ISSN 2191-5903
issn_series 2191-589X
copyrightThe Author(s) 2017
The information of publication is updating

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沙發(fā)
發(fā)表于 2025-3-21 23:51:26 | 只看該作者
板凳
發(fā)表于 2025-3-22 04:09:21 | 只看該作者
Permanent Crustal Uplift Due to Plume Activity,1 my, and high eruption rate, one to two orders of magnitude higher than the associated hotspot trail (Richards et al. in Science 246:103–107, 1989). This fits well with the premise that the flood basalts are the result of plume-head melting, while the hotspot track is produced by the plume tail (Campbell and Davies in Episodes 29(3), 2006).
地板
發(fā)表于 2025-3-22 05:10:18 | 只看該作者
Elastic Properties of the Lithosphere,The elastic thickness (T.) is the computed thickness of a lithospheric plate that responds elastically to long term geological loading by flexure. The loading should take place for more than 10. years. The elastic thickness represents the integrated strength of the lithosphere and is a measure of its resistivity to deformation.
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發(fā)表于 2025-3-22 11:09:00 | 只看該作者
6#
發(fā)表于 2025-3-22 16:36:05 | 只看該作者
Dynamic Crustal Uplift Due to Plume Activity,Plume ascent is driven by buoyancy due to density difference from the surrounding material.
7#
發(fā)表于 2025-3-22 18:30:12 | 只看該作者
8#
發(fā)表于 2025-3-22 21:39:54 | 只看該作者
Morphology of Hotspots,Oceanic volcanoes are composed of basaltic lava flows from shallow magma chambers. The process of volcano build-up is poorly understood. In general, smooth rounded shapes are produced by summit eruptions, while complex ridges are produced by flank eruptions.
9#
發(fā)表于 2025-3-23 03:14:37 | 只看該作者
The Great Plume Debate,The plume hypothesis (Morgan in Nature 230:42–43, 1971, Bulletin of the American Association of Petroleum Geologists 56:203–213, 1972a, Geological Society of America Memoir 132:7–22, 1972b) has been developed during the 1970s to explain several intraplate volcanic provinces on the earth’s surface, apparently not explained by plate tectonics.
10#
發(fā)表于 2025-3-23 08:56:54 | 只看該作者
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