Plume genesis of non-kimberlite diamonds
Calculations shown that a relatively low-temperature kimberlite magmas consolidated with decompression exploded on significant depth and formed pipes. High-temperature lamproite magmas exploded on near-surface conditions and formed mainly tuff covers. Their erosion formed diamond placers. Kimberlite...
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| Format: | Article |
| Language: | English |
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A.N. Zavaritsky Institute of Geology and Geochemistry
2015-01-01
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| Series: | Литосфера |
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| Online Access: | https://test.lithosphere.ru/jour/article/view/212 |