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Date: 2015
Language: eng
Resource Type: book chapter
Identifier: http://hdl.handle.net/1959.14/1063041
Description: Mesoarchean Kola-Karelia continent in the eastern Fennoscandian Shield includes three tectonic provinces, Kola, Karelia and Belomoria, that were formed by the Paleoarchean and Mesoarchean microcontine ... More
Date: 2014
Language: eng
Resource Type: book chapter
Identifier: http://hdl.handle.net/1959.14/334773
Description: Magma mixing was an important process in the genesis of plutonic suites of the Peninsular Ranges batholith, San Diego County transect. Contrary to expectations, minimum Hf arc mantle model ages (HfTAM ... More
Reviewed: Reviewed
Date: 2014
Language: eng
Resource Type: book chapter
Identifier: http://hdl.handle.net/1959.14/334779
Description: In the Peninsular Ranges batholith of southern California, a central belt of Jurassic metagranites was intruded by a Cretaceous magmatic arc that migrated from west to east across the belt. The Cretac ... More
Reviewed: Reviewed
Date: 2013
Subject Keyword: 040200 Geochemistry | 040300 Geology
Language: eng
Resource Type: book chapter
Identifier: http://hdl.handle.net/1959.14/313517
Description: Mantle metasomatism is a relatively recent concept introduced in the early 1970s when detailed studies of lithospheric mantle rock fragments (xenoliths), brought to the surface of in basaltic to kimbe ... More
Date: 2011
Subject Keyword: 040300 Geology | 040400 Geophysics
Language: eng
Resource Type: book chapter
Identifier: http://hdl.handle.net/1959.14/162281
Description: There is no one model, no paradigm, that uniquely defines arc–continent collision. Natural examples and modelling of arc–continent collision show that there is a large degree of, and variation in, com ... More
Authors: Vernon, R. H
Date: 2011
Subject Keyword: 040300 Geology
Language: eng
Resource Type: book chapter
Identifier: http://hdl.handle.net/1959.14/150990
Description: The most reliable microstructural criterion for the former presence of felsic melt in regional migmatites is a three-mineral (quartz, K-feldspar, and sodic plagioclase) aggregate in veinlets. Several ... More
Authors: Metcalfe, Ian
Date: 2011
Language: eng
Resource Type: book chapter
Identifier: http://hdl.handle.net/1959.14/167723
Description: SE Asia comprises a collage of Gondwana-derived continental blocks assembled by the closure of multiple Tethyan and back-arc ocean basins now represented by suture zones. Two major biogeographical bou ... More
Date: 2011
Subject Keyword: 040400 Geophysics
Language: eng
Resource Type: book chapter
Identifier: http://hdl.handle.net/1959.14/162280
Description: The temporal evolution of internal forces in a collision environment controls first-order characteristics such as convergence rate, slab dip, subduction stall, and slab breakoff, amongst others. Forem ... 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.