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foliation    音标拼音: [f,oli'eʃən]
n. 生叶,发叶,绿叶的状态

生叶,发叶,绿叶的状态

foliation
n 1: (botany) the process of forming leaves [synonym: {foliation},
{leafing}]
2: (geology) the arrangement of leaflike layers in a rock
3: (architecture) leaf-like architectural ornament [synonym:
{foliation}, {foliage}]
4: the production of foil by cutting or beating metal into thin
leaves
5: the work of coating glass with metal foil

Foliation \Fo"li*a"tion\, n. [Cf. F. foliation.]
1. The process of forming into a leaf or leaves.
[1913 Webster]

2. The manner in which the young leaves are dispo?ed within
the bud.
[1913 Webster]

The . . . foliation must be in relation to the stem.
--De Quincey.
[1913 Webster]

3. The act of beating a metal into a thin plate, leaf, foil,
or lamina.
[1913 Webster]

4. The act of coating with an amalgam of tin foil and
quicksilver, as in making looking-glasses.
[1913 Webster]

5. (Arch.) The enrichment of an opening by means of foils,
arranged in trefoils, quatrefoils, etc.; also, one of the
ornaments. See {Tracery}.
[1913 Webster]

6. (Geol.) The property, possessed by some crystalline rocks,
of dividing into plates or slabs, which is due to the
cleavage structure of one of the constituents, as mica or
hornblende. It may sometimes include slaty structure or
cleavage, though the latter is usually independent of any
mineral constituent, and transverse to the bedding, it
having been produced by pressure.
[1913 Webster]


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  • Foliation (geology) - Wikipedia
    Foliation is usually formed by the preferred orientation of minerals within a rock Usually, this is the result of some physical force and its effect on the growth of minerals The planar fabric of a foliation typically forms at right angles to the maximum principal stress direction
  • Foliation | Types, Causes, Facts | Britannica
    Foliation, planar arrangement of structural or textural features in any rock type but particularly that resulting from the alignment of constituent mineral grains of a metamorphic rock of the regional variety along straight or wavy planes Foliation is exhibited most prominently by sheety minerals
  • Foliation in Metamorphic Rocks | Definition, Causes Types
    Discover the causes of foliation in metamorphic rocks Understand foliation differences, and investigate examples of slate, schist, and gneiss
  • 10. 2: Foliation and Rock Cleavage - Geosciences LibreTexts
    The pattern of aligned crystals that results is called foliation Foliation can develop in a number of ways Minerals can deform when they are squeezed (Figure 10 5), becoming narrower in one direction and longer in another
  • Foliation - Geology is the Way
    The terms ‘foliation’, ‘cleavage’, and ‘schistosity’ have all been used to define sets of penetrative planar elements in deformed rocks However, they are not synonyms and have been used differently over the years by various authors
  • 6. 2 Foliation and Rock Cleavage – Principles of Earth Science
    Breaks along planes of weakness within a rock that are caused by foliation are referred to as rock cleavage, or just cleavage This is distinct from cleavage in minerals because mineral cleavage happens between atoms within a mineral, but rock cleavage happens between minerals
  • Foliation - SpringerLink
    Foliation is a planar structure showing preferred orientation of minerals with a platy or tabular habit The preferred orientation is produced by deformation and is uniformly pervasive in a rock Foliation is developed in metamorphic rocks, and it includes cleavage, schistosity, gneissosity and gneissic banding





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