1973
DOI: 10.1007/bf00371762
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Chrome-rich garnets from the kimberlites of yakutia and their parageneses

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Cited by 388 publications
(169 citation statements)
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“…Pyrope is considered to be the most important KIM, and its chemistry is one of the best tools used in diamond exploration for identifying kimberlites and determining their potential to host diamonds [22][23][24][25][26][27].…”
Section: Pyropementioning
confidence: 99%
“…Pyrope is considered to be the most important KIM, and its chemistry is one of the best tools used in diamond exploration for identifying kimberlites and determining their potential to host diamonds [22][23][24][25][26][27].…”
Section: Pyropementioning
confidence: 99%
“…Garnets are the minerals of choice in this application, because their major-element compositions are diagnostic of a large range of mantle rock types (e.g., Sobolev et al, 1973;Grütter et al, 2004) and single-mineral thermobarometry techniques are applicable to the Cr-pyrope varieties that occur in depleted peridotite (see O'Reilly and Griffin, 2006 for a recent summary with applications). Most public-domain garnet xenocryst data sets lack the detailed trace-element compositions required to apply Ni-in-garnet thermometry.…”
Section: Northern Lesotho Xenocrysts: Expanding the Data Setmentioning
confidence: 99%
“…Cr 2 O 3 content in most garnets is below 1 wt%, although in a few samples it is high (1.8-8.3 wt%). End member calculations following the method of Sobolev et al (1973) for Cr-rich garnets give the following values (in mol%) for all samples except rutile eclogite: pyrope (57-74), almandine (12-27), grossular (0-26), spessartine (61), andradite (0-5), Ti-andradite (61), uvarovite (0-16) and knorringite (0-8). The garnet of rutile eclogite is highly iron-rich with end member composition of Prp 26.5 Alm 52.5 Grs 14.7 Adr 5.1 TiAdr 0.3 Sps 1.0 Uv 0.1 .…”
Section: Garnetmentioning
confidence: 99%