ಪೆರಿಡೋಟೈಟ್ ಅಪರೂಪದ ವಿಧವಾಗಿದ್ದು ಅದು ಕೆಲವೊಮ್ಮೆ ವಜ್ರಗಳನ್ನು ಹೊಂದಿರುತ್ತದೆ, ದಕ್ಷಿಣ ಆಫ್ರಿಕಾ ಮತ್ತು ಸೈಬೀರಿಯಾದಲ್ಲಿ ಕಂಡುಬರುತ್ತದೆ,

kimberlite ಕನ್ನಡದಲ್ಲಿ ಉದಾಹರಣೆ:

ವಜ್ರವನ್ನು ಕಿಂಬರ್ಲೈಟ್ ಮತ್ತು ಲಾಂಪೊರೈಟ್ ಗಳಿಂದ ಗಣಿಗಾರಿಕೆಯ ಮೂಲಕ ತೆಗೆಯಲಾಗುವುದು.

ವಜ್ರವು ನದಿಗಳು ಹೊಡೆದುಕೊಂಡುಬಂದ, ಗ್ರಾವೆಲ್, ಮರಳು, ಅಥವಾ ಜೇಡಿಮಣ್ಣಿನಲ್ಲಿ ಬೆಣಚುಕಲ್ಲು, ಕುರಂಗದಕಲ್ಲು ಮೊದಲಾದ ಕಲ್ಲುಗಳೊಡನೆಯೂ, ಚಿನ್ನ, ಪ್ಲಾಟಿನಮ್ ಲೋಹಗಳೊಡನೆಯೂ, ಬೇರೆ ಬೇರೆ ಹಳಕುಗಳಾಗಿ ಸೇರಿಯೂ, ಕಂಗ್ಲಾಮರೇಟ್ ಎಂಬ ಶಿಲಾ ವಿಶೇಷದಲ್ಲಿಯೂ, ದಕ್ಷಿಣ ಆಫ್ರಿಕದ ,ಕಿಂಬರ್ಲಿ’ ಪ್ರಾಂತದಲ್ಲಿ ಸಿಕ್ಕುವ “ಕಿಂಬರ್ಲೈಟ್’’ ಎಂಬ ಹಸಿರು ಮತ್ತು ನೀಲಿ ಮಿಶ್ರವಾದ ಖನಿಜ ವಿಶೇಷದಲ್ಲಿಯೂ ದೊರೆಯುವುದು.

kimberlite's Usage Examples:

Buffalo Head Hills Kimberlite Field The Buffalo Head Hills kimberlite field is a group of kimberlitic volcanic pipes or diatremes in north-central Alberta.

The Finsch mine is a traditional diamantiferous kimberlite pipe, extending around 17.

Jagersfontein is known as a kimberlite pipe, and a prime locality for mantle xenoliths, some of which are believed to have come from depths of 300–500 km (190–310 mi).

Rare occurrences may include unusual surface deposits of maars of kimberlites in the diamond fields of southern Africa and other regions.

Among the rocks that commonly include peridotite xenoliths are basalt and kimberlite.

Corne kimberlite field is a 104- to 95-million-year-old diamond-bearing kimberlite field in east-central Saskatchewan, Canada.

Previously, the term kimberlite has been applied to olivine lamproites as Kimberlite II, however this has been in error.

kimberlites, lamproites and lamprophyres, which have their source in the upper mantle, often contain fragments and crystals assumed to be a part of the originating.

Phlogopite mica is a commonly known phenocryst and groundmass phase within ultrapotassic igneous rocks such as lamprophyre, kimberlite.

English: kimberlite diamond pipe "Lightning" (more exact translation: "heat lightning")) was the first kimberlite diamond pipe discovered in Russia.

sometimes associated with kimberlite magma, which originates in the upper mantle: when a diatreme is formed due to a kimberlite intrusion, there is a possibility.

The most characteristic carbonados are mined in the Central African Republic and in Brazil, in neither place associated with kimberlite, the source of typical gem diamonds.