Please use this identifier to cite or link to this item: http://localhost:8080/xmlui/handle/123456789/131155
Full metadata record
DC FieldValueLanguage
dc.contributor.authorDamien Closson
dc.date.accessioned2017-04-30T13:31:40Z-
dc.date.available2017-04-30T13:31:40Z-
dc.date.issued2011
dc.identifier.isbn978-953-307-545-7
dc.identifier.urihttp://hdl.handle.net/123456789/131155-
dc.description.abstractThe term tectonics refers to the study dealing with the forces and displacements that have operated to create structures within the lithosphere. The deformations affecting the Earth's crust are result of the release and the redistribution of energy from Earth's core. The concept of plate tectonics is the chief working principle. Tectonics has application to lunar and planetary studies, whether or not those bodies have active tectonic plate systems. Petroleum and mineral prospecting uses this branch of knowledge as guide. The present book is restricted to the structure and evolution of the terrestrial lithosphere with dominant emphasis on the continents. Thirteen original scientific contributions highlight most recent developments in seven relevant domains: Gondwana history, the tectonics of Europe and the Near East; the tectonics of Siberia; the tectonics of China and its neighbourhood; advanced concepts on plate tectonics are discussed in two articles; in the frame of neotectonics, two investigation techniques are examined; finally, the relation between tectonics and petroleum researches is illustrated in one chapter.
dc.language.isoeng
dc.publisherInTech
dc.relation.isbasedon10.5772/567
dc.relation.urihttp://www.intechopen.com/books/tectonics
dc.rights.uriCC BY-NC-SA (姓名標示-非商業性-相同方式分享)
dc.sourceInTech
dc.subject.classificationEarth and Planetary Sciences
dc.subject.classification Geology and Geophysics
dc.titleTectonics
dc.type電子教課書
dc.classification自然科學類
Theme:教科書-自然科學類

Files in This Item:
There are no files associated with this item.


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.