Remobilization in the Cratonic Lithosphere Recorded in Polycrystalline Diamond
Polycrystalline diamonds (framesites) from the Venetia kimberlite in South Africa contain silicate minerals whose isotopic and trace element characteristics document remobilization of older carbon and silicate components to form the framesites shortly before kimberlite eruption. Chemical variations...
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| Published in: | Science (American Association for the Advancement of Science) Vol. 289; no. 5482; pp. 1182 - 1185 |
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| Main Authors: | , , , |
| Format: | Journal Article |
| Language: | English |
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Washington, DC
American Society for the Advancement of Science
18-08-2000
American Association for the Advancement of Science The American Association for the Advancement of Science |
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| Abstract | Polycrystalline diamonds (framesites) from the Venetia kimberlite in South Africa contain silicate minerals whose isotopic and trace element characteristics document remobilization of older carbon and silicate components to form the framesites shortly before kimberlite eruption. Chemical variations within the garnets correlate with carbon isotopes in the diamonds, indicating contemporaneous formation. Trace element, radiogenic, and stable isotope variations can be explained by the interaction of eclogites with a carbonatitic melt, derived by remobilization of material that had been stored for a considerable time in the lithosphere. These results indicate more recent formation of diamonds from older materials within the cratonic lithosphere. |
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| AbstractList | Polycrystalline diamonds (framesites) from the Venetia kimberlite in South Africa contain silicate minerals whose isotopic and trace element characteristics document remobilization of older carbon and silicate components to form the framesites shortly before kimberlite eruption. Chemical variations within the garnets correlate with carbon isotopes in the diamonds, indicating contemporaneous formation. Trace element, radiogenic, and stable isotope variations can be explained by the interaction of eclogites with a carbonatitic melt, derived by remobilization of material that had been stored for a considerable time in the lithosphere. These results indicate more recent formation of diamonds from older materials within the cratonic lithosphere. Polycrystalline diamonds (framesites) from the Venetia kimberlite in South Africa contain silicate minerals whose isotopic and trace element characteristics document remobilization of older carbon and silicate components to form the framesites shortly before kimberlite eruption. Chemical variations within the garnets correlate with carbon isotopes in the diamonds, indicating contemporaneous formation. |
| Audience | Academic |
| Author | Jagoutz, E. Viljoen, K. S. Grassineau, N. Jacob, D. E. |
| Author_xml | – sequence: 1 givenname: D. E. surname: Jacob fullname: Jacob, D. E. – sequence: 2 givenname: K. S. surname: Viljoen fullname: Viljoen, K. S. – sequence: 3 givenname: N. surname: Grassineau fullname: Grassineau, N. – sequence: 4 givenname: E. surname: Jagoutz fullname: Jagoutz, E. |
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| ContentType | Journal Article |
| Copyright | Copyright 2000 American Association for the Advancement of Science 2000 INIST-CNRS COPYRIGHT 2000 American Association for the Advancement of Science COPYRIGHT 2000 American Association for the Advancement of Science Copyright American Association for the Advancement of Science Aug 18, 2000 |
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| DOI | 10.1126/science.289.5482.1182 |
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| Keywords | nesosilicates O-18 eclogite petrogenesis Nd-144/Nd-143 Africa polycrystalline materials lithosphere garnet igneous rocks cratons metamorphic rocks remobilization rare earths trace-element analyses diamond C-13 isotopes kimberlite plutonic rocks silicates Sr-87/Sr-86 native elements |
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| Snippet | Polycrystalline diamonds (framesites) from the Venetia kimberlite in South Africa contain silicate minerals whose isotopic and trace element characteristics... |
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| SubjectTerms | Bacteria Carbon Crystalline rocks Diamonds Earth sciences Earth, ocean, space Eclogite Exact sciences and technology Garnets Geology Igneous and metamorphic rocks petrology, volcanic processes, magmas Internal geophysics Isotopes Lithospheres Minerals Peridotite Scientific Concepts Solid-earth geophysics, tectonophysics, gravimetry |
| Title | Remobilization in the Cratonic Lithosphere Recorded in Polycrystalline Diamond |
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