acicular crystalの例文

• Cyanotrichite forms velvety radial acicular crystal aggregates of extremely fine fibers.
• It is bright yellow in colour and usually has an acicular crystal habit.
• Recrystallization from toluene forms acicular crystals.
• Clinoclase is a rare secondary copper mineral and forms acicular crystals in the fractured weathered zone above copper sulfide deposits.
• Ulexite is found in evaporite deposits and the precipitated ulexite commonly forms a " cotton ball " tuft of acicular crystals.
• It is a colorless to white mineral crystallizing in the monoclinic crystal system typically occurring as prismatic to acicular crystals or granular masses.
• In the Silurian New York strontianite is observed in cavities in eastern Lockport, where it occurs as small white radiating sprays of acicular crystals.
• In groups of acicular crystals it is frequently seen penetrating quartz as in the " fl閏hes d'amour " from Graub黱den, Switzerland.
• Gabbro may be extremely coarse grained to pegmatitic, and some pyroxene-plagioclase cumulates are essentially coarse grained gabbro, some may exhibit acicular crystal habits.
• It occurs as transparent to translucent orange-brown aggregates of subparallel acicular crystals up to 10 mm in length, and as patches of yellow, fibrous crystals.
• It crystallizes in the orthorhombic system and forms translucent bright blue acicular crystal clusters or Refractive indices are n? = 1.588 n? = 1.617 n? = 1.655.
• Finely crystallized specimens have been obtained from the Friedrichssegen mine in Lahnstein in Rhineland-Palatinate, Johanngeorgenstadt in Saxony, StY
  韇ro in the Czech Republic, Phoenixville in Pennsylvania, acicular crystals of considerable length were found long ago in the Pentire Glaze mine near St Minver in Cornwall.
• At the Minerva Number 1 Mine ( Ozark-Mahoning Number 1 Mine ) Ozark-Mahoning Group, Cave-in-Rock, Illinois, in the Kentucky Fluorspar District, Hardin County strontanite occurs as white, brown or rarely pink tufts and bowties of acicular crystals with slightly curved terminations.