Anagram & Information om | Engelska ordet VEINLETS

Exempel på hur man kan använda VEINLETS i en mening

• A stringer lode is one in which the rock is so permeated by small veinlets that rather than mining the veins, the entire mass of ore and the enveined country rock is mined.
• It occurs as veinlets in lazurite crystals in the Afghan location and in altered limestone xenoliths within pumice in Pitigliano, Tuscany, Italy.
• The forewing has the cell crossed by five short black bands, of which the basal extends to the dorsum, the sub-basal into interspace 1, the medial and pre-apical up to the median vein, and the apical or fifth along the discocellulars; this last band extends broadly on both sides of the veinlets and terminates at the lower apex of the cell; beyond these are broad postdiscal and terminal black transverse bands from costa to tornal angle; the two bands coalesce below vein 4 and terminate in a point at the tornus; the white portions of the cell anteriorly overlaid with pale green; short broken glossy green bands between the black cellular apical band and the discal band and anteriorly between the latter and the terminal band.
• They do not have ctenidia, instead obtaining oxygen through a ring of gill lamellae that encircle the mantle just inside the shell edge and from the surface of the roof of the nuchal cavity which is exposed to air when the animal is no longer under water and which is covered in a network of blood vessels all of which eventually carry oxygenated blood and connect to the auricle through a series of veinlets on the animal's left side.
• The white colour of the forewings is much more extended, especially in the apical region, but also more shaded with black scales; the internervular black streaks between the median nervures (veins 4-6) are much longer, the white linear markings, in the cell reach the discocellular veinlets.
• Forewing more broadly angled below the apex; with the entire apical area broadly pale ochreous, on which is placed a round black spot with white pupil, situated between the upper and middle median veinlets, also a minute obsolescent ocellus below it and three above it.
• Fronds stipitate, the stipes fleshy, with numerous longitudinal air canals, abaxially rounded and ribbed, adaxially flattened, vascular bundles in a peripheral ring, one with each rib and several to the adaxial side, and several smaller medullary strands; lamina dimorphic, sterile fronds +/- spreading, 2–3-pinnatifid with broad membranous lobes, venation reticulate without included free veinlets, often with proliferous buds in the axils; fertile fronds erect, longer, narrower and more divided than the sterile, the lobes strongly recurved to completely cover the adiaxial surface, venation longitudinal, branching at the bases of the lobes.
• The single fold, lanceolate leaflets may be few to numerous, usually with armed margins and caducous scales, with conspicuous midribs and transverse veinlets.
• the primitive original vein network characterizing the wings of many of the most ancient insect fossils (T-B, after Needham; Mackerras, in CSIRO); in Mastotermitidae and Hodotermitidae (Isoptera), the complex network or reticulum of irregular veinlets between the veins in the apical 3 quarters of both wings, including the anal lobe (Emerson).
• Athabascaite often contains umangite as inclusions and stained carbonate vein material as stringers and veinlets.
• Here, sparse massive veinlets of arsenopyrite with minor chalcopyrite, pyrite and pyrrhotite are present.
• In this deposit, lulzacite occurs within quartz and siderite veinlets at quartzite–limestone contacts.
• As one approaches the lode the granodiorite becomes mylonitized and is traversed by veinlets covered in pyromorphite.
• The ore consisted of massive pods and disseminated veinlets of pitchblende, with secondary metatorbernite, autunite, gummite and gold, with minor pyrite, galena and chalcopyrite.
• It is also associated with the sulfide veinlets around the Shumilovsk deposit in Russia, the volcanogenic massive Cofer deposit in Virginia, and the American Southwest.
• The subcostal veinlets mostly are only shallowly forked, and the radial crossveins being grouped into a pair of gradate series.
• Hydrothermal alteration of the central lava dome and iron-bearing deposits has generated alunite, anatase, bassanite, chlorite, copper veinlets, gypsum, illite, jarosite, kaolinite, labradorite, quartz, rutile, sanidine, smectite, sulfur and tridymite.
• This is the last crystallization of vanadate at the site since medaite was the last vanadate mineral being crystallized, but because of retrograde metamorphism, occurring at the place, vanadium moved into medaite veinlets, forming cross-cutting fianelite on medaite.
• Waylandite in its crystal form occurs in vugs and rarely in pegmatites; however in its powder form it can be found forming crusts and veinlets.

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