Coupled Deep Earth and surface processes and their impact on geohazards

Sierd Cloetingh; Alessandro Tibaldi; Evgenii Burov

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Coupled Deep Earth and surface processes and their impact on geohazards

机译：Coupled Deep Earth and surface processes and their impact on geohazards

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Better understanding of coupled Deep Earth and surface processes is the key for resolving the evolution of the continental lithosphere and its surface topography. The thermo-mechanical structure of the lithosphere exerts a prime control on the interaction of mantle instabilities and tectonic forces operating on the lithosphere. These processes are fundamental for differential vertical motions at or near the Earth's surface and have a strong impact in the domains of geohazards and geo-energy. Stress fields exert a main control on volcano dynamics and in the conduits of fluids and melts. Integrated Solid Earth sciences intrinsically link different spatial and temporal scales and involve an interdisciplinary approach, with strong feedbacks between observational studies and imaging of Earth structure, reconstruction of the geological record and process-modelling.

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来源
《Global and planetary change》 |2012年第6期|1-19|共19页
作者
Sierd Cloetingh; Alessandro Tibaldi; Evgenii Burov;
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作者单位

Netherlands Research Centre for Integrated Solid Earth Sciences, Utrecht University, Budapestlaan 4,3584 CD, Utrecht, The Netherlands;

Department of Geological Sciences and Geotechnologies, University of Milan Bicocca, 20126 Milan, Italy;

ISEP, Universite Pierre et Marie Curie, Rue Notre Dame des Champs 28, 75006 Paris, France;

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原文格式 PDF
正文语种英语
中图分类天文学;
关键词
geohazards; geo-energy; Deep Earth; topography;

Coupled Deep Earth and surface processes and their impact on geohazards

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