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Aphanite

In the article presented below, Aphanite will be addressed from different perspectives, with the aim of providing a comprehensive view on this topic. From its origin and history, through its relevance today, to possible future implications, this article aims to offer a complete look at Aphanite. Its various facets will be analyzed, its different interpretations will be explored, and the controversies surrounding it will be discussed. In addition, the implications that Aphanite has in different contexts will be examined and reflections and opinions of experts in the field will be presented. Without a doubt, this article will seek to shed light on Aphanite and its impact on society.

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The smooth texture of this basaltic volcanic bomb is aphanitic.
IUGS classification of aphanitic extrusive igneous rocks according to their relative alkali (Na2O + K2O) and silica (SiO2) weight contents. Blue area is roughly where alkaline rocks plot; yellow area where subalkaline rocks plot.[1]
An aphanitic volcanic sand grain, with fine-grained groundmass, as seen through a petrographic microscope

Aphanites (adj. aphanitic; from Ancient Greek αφανης (aphanḗs) 'invisible') are igneous rocks that are so fine-grained that their component mineral crystals are not visible to the naked eye[2] (in contrast to phanerites, in which the crystals are visible to the unaided eye). This geological texture results from rapid cooling in volcanic or hypabyssal (shallow subsurface) environments. As a rule, the texture of these rocks is not the same as that of volcanic glass (e.g., obsidian), with volcanic glass being non-crystalline (amorphous), and having a glass-like appearance.[3]

Aphanites are commonly porphyritic, having large crystals embedded in the fine groundmass, or matrix. The larger inclusions are called phenocrysts. They consist essentially of very small crystals of minerals such as plagioclase feldspar, with hornblende or augite, and may contain also biotite, quartz, and orthoclase.[2]

Common rocks that can be aphanitic

References

  1. ^ Le Maitre, R. W., ed. (1989). A classification of igneous rocks and glossary of terms. Oxford: Blackwell Science.
  2. ^ a b One or more of the preceding sentences incorporates text from a publication now in the public domain: Chisholm, Hugh, ed. (1911). "Aphanite". Encyclopædia Britannica. Vol. 2 (11th ed.). Cambridge University Press. p. 163.
  3. ^ Bates and Jackson (1984). Dictionary of Geological Terms (3rd ed.). American Geological Institute.


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