epidote group oor Frans
epidote group
Vertalings in die woordeboek Engels - Frans
groupe des épidotes
groupe épidote
épidotes
Geskatte vertalings
Vertoon algoritmies gegenereerde vertalings
voorbeelde
Advanced filtering
Voorbeelde moet herlaai word.
Abundant secondary chlorite, epidote, and actinolite indicate the group was metamorphosed to greenschist facies (~350 °C).
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MSH occurrence of epidote, a member of the epidote group, is rare at MSH.
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Zoisite is the orthorhombic dimorph of clinozoisite and, like it, belongs to the epidote group.
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The occurrence of epidote, a member of the epidote group, is rare at MSH.
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Due to basaltic composition of the Iceland-Faeroe-Ridge, the “allochthonous group”, with the main components green hornblende-garnet-epidote, cannot be derived from the ridge itself.
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Tanzanite is the transparent and gemmy variety of zoisite, a mineral from the epidote group, which has an extraordinary purplish blue color and a pronounced trichroism ranging from blue to purple and gray-green.
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Product Details Group of epidote crystals from Cime du Cornillon, Bourg d'Oisans, Isère, Rhône-Alpes, France.
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English Allanite - of the group of epidote in which it represents the iron and rare earths rich term (cerium, lanthanum, neodymium, etc...).
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The epidote is the main representative of a group of complex sorosilicates to which it gave its name.
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The colors are due to the inclusions of iron oxides (yellow), graphite (gray) and chlorite, epidote or minerals of the serpentine group (pale blue).
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The most famous site (today protected by a nature reserve) is the Knappenwand (Austria), which has provided extraordinary elongated prismatic crystals, dark green commonly reaching 10 cm and exceptionally 50 cm by 8 cm section, often gemmy forming parallel groups; the epidote is associated with titanite, quartz, byssolite, and hematite.
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We infer that the Trinity Peninsula Group of the Antarctic Peninsula was deposited in a fore-arc basin(s) of composite type located between the Gondwanian arc massif (consisting of plutonic and older gneissose basement rocks) and a subduction complex, now represented by “greenschists”, “blueschists” and albite-epidote-hornblende-bearing rocks of the pre-Jurassic metamorphic complex.
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12 sinne gevind in 16 ms. Hulle kom uit baie bronne en word nie nagegaan nie.