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Date: 2004
Language: eng
Resource Type: conference paper abstract
Identifier: http://hdl.handle.net/1959.14/1213972
Description: 1 page(s)
Date: 2004
Language: eng
Resource Type: conference paper abstract
Identifier: http://hdl.handle.net/1959.14/1214161
Description: 1 page(s)
Date: 2004
Language: eng
Resource Type: conference paper abstract
Identifier: http://hdl.handle.net/1959.14/1214141
Description: 1 page(s)
Date: 2004
Language: eng
Resource Type: conference paper abstract
Identifier: http://hdl.handle.net/1959.14/1214108
Description: 1 page(s)
Date: 2004
Subject Keyword: 040200 Geochemistry
Language: eng
Resource Type: conference paper abstract
Identifier: http://hdl.handle.net/1959.14/1209388
Description: 1 page(s)
Date: 2004
Language: eng
Resource Type: conference paper abstract
Identifier: http://hdl.handle.net/1959.14/1213989
Description: 1 page(s)
Date: 2004
Language: eng
Resource Type: conference paper abstract
Identifier: http://hdl.handle.net/1959.14/1214111
Description: 1 page(s)
Date: 2004
Language: eng
Resource Type: conference paper abstract
Identifier: http://hdl.handle.net/1959.14/1214040
Description: 1 page(s)
Date: 2004
Language: eng
Resource Type: conference paper abstract
Identifier: http://hdl.handle.net/1959.14/1214005
Description: 1 page(s)
Date: 2004
Language: eng
Resource Type: conference paper abstract
Identifier: http://hdl.handle.net/1959.14/1214138
Description: 1 page(s)
Date: 2004
Language: eng
Resource Type: conference paper abstract
Identifier: http://hdl.handle.net/1959.14/1226348
Date: 2008
Language: eng
Resource Type: conference paper abstract
Identifier: http://hdl.handle.net/1959.14/1223694
Date: 2012
Language: eng
Resource Type: conference paper abstract
Identifier: http://hdl.handle.net/1959.14/208578
Description: Polished plates of diamondites (polycrystalline diamond aggregates) from Africa and in eclogites from Lesotho, were prepared for study of internal structure and in-situ geochemical analysis, to unders ... More
Date: 2012
Language: eng
Resource Type: conference paper abstract
Identifier: http://hdl.handle.net/1959.14/211790
Description: A U-Pb/Hf-isotope study of >16,000 zircons shows that 70% of Earth's continental crust probably formed in Archean time, and much probably is >3 Ga old. The model ages (TMA ) of ca 500 low-Re/Os sulfid ... More