Jadeite deposits of the clear creek area, New Idria district, San Benito county, California

Journal of Petrology
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Abstract

Tectonic inclusions within the New Idria serpentine body contain jadeite in two distinct assemblages: (1) Lenslike inclusions containing a monomineralic green jadeite core surrounded by a calc-silicate rim. (2) Jadeite veins cross-cutting albite-crossite schist inclusions. In these veins jadeite coexists with low albite; green jadeite (Jd 75 Ac+Di+He 25) coexists with low albite within the host schist.

Albite schists are related to the pre-metamorphic keratophyres and it can be shown that desilication of such rocks produces a bulk composition similar to that of jadeite. Metamor-phism of keratophyric tectonic inclusions within serpentine produced jadeite-albite schists along margins of the inclusions. Jadeite-albite veins formed from mobilized liquids rich in the jadeite molecule and deficient in water. Geological evidence such as would indicate extreme pressures or temperatures during jadeite formation is lacking; rather, a low silica and dry system allowed its formation at reduced temperatures and pressures.

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Publication type Article
Publication Subtype Journal Article
Title Jadeite deposits of the clear creek area, New Idria district, San Benito county, California
Series title Journal of Petrology
DOI 10.1093/petrology/2.2.209
Volume 2
Issue 2
Year Published 1961
Language English
Publisher Oxford University Press
Description 39 p.
First page 209
Last page 247
Country United States
State California
Other Geospatial Monterey Bay
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