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Date: 2011
Language: eng
Resource Type: book
Identifier: http://hdl.handle.net/1959.14/309917
Description: Quantifying the timescales of current geological processes is critical for constraining the physical mechanisms operating on the Earth today. Since the Earth’s origin 4.55 billion years ago magmatic p ... More
Date: 2010
Subject Keyword: 040400 Geophysics | 040300 Geology
Language: eng
Resource Type: book chapter
Identifier: http://hdl.handle.net/1959.14/114684
Description: 31 page(s)
Date: 2010
Subject Keyword: 040300 Geology | 040400 Geophysics
Language: eng
Resource Type: book chapter
Identifier: http://hdl.handle.net/1959.14/114683
Description: Melt migration from a mantle source to eventual eruption may involve a variety of processes operating over a range of scales. For instance, melt ascent begins with grain-scale interactions, which, for ... More
Date: 2010
Subject Keyword: 040200 Geochemistry
Language: eng
Resource Type: book chapter
Identifier: http://hdl.handle.net/1959.14/114671
Description: 8 page(s)
Date: 2010
Subject Keyword: 040200 Geochemistry | 040300 Geology
Language: eng
Resource Type: book chapter
Identifier: http://hdl.handle.net/1959.14/114690
Description: 21 page(s)
Date: 2010
Language: eng
Resource Type: book chapter
Identifier: http://hdl.handle.net/1959.14/114677
Description: 14 page(s)
Date: 2010
Subject Keyword: 040300 Geology | 040200 Geochemistry
Language: eng
Resource Type: book chapter
Identifier: http://hdl.handle.net/1959.14/114678
Description: Magmas carrying mantle xenoliths much reach the surface within a maximum of about 8 to 60 hours of picking up these dense fragments from depths of about 200 to 80km depth.
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