Cretaceous Sea Level Rise

This book PDF is perfect for those who love Science genre, written by Mu Ramkumar and published by Elsevier which was released on 05 November 2015 with total hardcover pages 70. You could read this book directly on your devices with pdf, epub and kindle format, check detail and related Cretaceous Sea Level Rise books below.

Cretaceous Sea Level Rise
Author : Mu Ramkumar
File Size : 52,5 Mb
Publisher : Elsevier
Language : English
Release Date : 05 November 2015
ISBN : 9780128093238
Pages : 70 pages
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Cretaceous Sea Level Rise by Mu Ramkumar Book PDF Summary

Cretaceous Sea Level Rise delves into the question of whether the observed short-term sea-level changes are regional (tectonic) or global (eustatic) and determines their possible relation to climate cycles; to assess the role of feedback mechanisms, i.e. thermal expansion/contraction of seawater, subsidence due to loading by water, changing vegetation of the Earth System and to investigate the relation of sea-level highs and lows to ocean anoxia and oxidation events, represented by black shales and oceanic red beds, and to evaluate the evidence for ephemeral glacial episodes or other climate events. Though research has been, and is being, conducted in these fields since the introduction of sea level cycles and sequence development concepts in the 1970"s, the available information is scattered. Cretaceous Sea Level Rise presents the current understanding and future directions of the research on Cretaceous sea level cycles in a single source, forming a reference work for beginners, graduates and postgraduates who are interested in this subject. Authored by an expert in Sea Level Rise, with over 15 years’ experience Concludes with a section that looks to the future of sea level change The only source to combine the current understanding and future directions of the research on Cretaceous sea level cycles in one place

Cretaceous Sea Level Rise

Cretaceous Sea Level Rise delves into the question of whether the observed short-term sea-level changes are regional (tectonic) or global (eustatic) and determines their possible relation to climate cycles; to assess the role of feedback mechanisms, i.e. thermal expansion/contraction of seawater, subsidence due to loading by water, changing

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