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JPN-10

Abstract

The plagioclase lath in this aphanitic basalt are generally all the same size and are strongly aligned to form a classic trachytic texture with interstitial olivine. A few larger crystals of both phases are observed.

Note

The author has given permission for this work to be deposited in the Digital Archive of Colorado College.

Okura

Administrative Notes

The author has given permission for this work to be deposited in the Digital Archive of Colorado College.

Copyright
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Publisher
None
PID
coccc:19481