Retinite

Retinite is resin, particularly from beds of brown coal which are near amber in appearance, but contain little or no succinic acid. It may conveniently serve as a generic name, since no two independent occurrences prove to be alike, and the indefinite multiplication of names, no one of them properly specific, is not to be desired.^[1]^[2]

Retinite resins contain no succinic acid and oxygen from 6% to 15%.^[3]

References

^ Dana, James Dwight; Dana, Edward Salisbury (1895). "Retinite". The system of mineralogy of James Dwight Dana 1837-1868 (6 ed.). New York: John Wiley & Sons. p. 1004. hdl:2027/uva.x002308182. OCLC 10749387.
^ Chisholm, Hugh, ed. (1911). "Retinite" . Encyclopædia Britannica. Vol. 23 (11th ed.). Cambridge University Press. p. 203.
^ "Retinite". Mindat.org. Kewsick, VA, USA: The Hudson Institute of Mineralogy.

This article incorporates text from a publication now in the public domain: Chisholm, Hugh, ed. (1911). "Retinite". Encyclopædia Britannica. Vol. 23 (11th ed.). Cambridge University Press. p. 203.

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[Dana1895-1] Dana, James Dwight; Dana, Edward Salisbury (1895). "Retinite". The system of mineralogy of James Dwight Dana 1837-1868 (6 ed.). New York: John Wiley & Sons. p. 1004. hdl:2027/uva.x002308182. OCLC 10749387.

[Britannica1911-2] Chisholm, Hugh, ed. (1911). "Retinite" . Encyclopædia Britannica. Vol. 23 (11th ed.). Cambridge University Press. p. 203.

[3] "Retinite". Mindat.org. Kewsick, VA, USA: The Hudson Institute of Mineralogy.

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