keilhau-ite (Meaning)
keilhau-ite (n.)
A mineral of a brownish black color, related to titanite in form. It consists chiefly of silica, titanium dioxide, lime, and yttria.
Synonyms & Antonyms of keilhau-ite
No Synonyms and anytonyms found
keilhau-ite Sentence Examples
- Keilhau-ite, a rare alkaline rock, is typically found in association with carbonatites.
- The mineralogical composition of keilhau-ite varies depending on its origin and can include minerals such as nepheline, diopside, and calcite.
- The texture of keilhau-ite can range from aphanitic to porphyritic, with phenocrysts of minerals like feldspar or pyroxene.
- Keilhau-ite is often found within volcanic complexes and can be associated with carbonatite intrusions.
- The study of keilhau-ite provides insights into the complex geological processes that occur during carbonatite formation.
- The weathering of keilhau-ite can lead to the formation of unique mineral assemblages, including rare earth element enrichments.
- Keilhau-ite is an important rock type for understanding the petrogenesis of alkaline magmas.
- The economic potential of keilhau-ite lies in its association with rare earth element deposits and potential use as a decorative stone.
- The geochemistry of keilhau-ite can provide clues about the mantle source from which it was derived.
- The occurrence of keilhau-ite in different geological settings offers valuable information for reconstructing past tectonic and volcanic activity.
FAQs About the word keilhau-ite
A mineral of a brownish black color, related to titanite in form. It consists chiefly of silica, titanium dioxide, lime, and yttria.
No synonyms found.
No antonyms found.
Keilhau-ite, a rare alkaline rock, is typically found in association with carbonatites.
The mineralogical composition of keilhau-ite varies depending on its origin and can include minerals such as nepheline, diopside, and calcite.
The texture of keilhau-ite can range from aphanitic to porphyritic, with phenocrysts of minerals like feldspar or pyroxene.
Keilhau-ite is often found within volcanic complexes and can be associated with carbonatite intrusions.
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