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Garnet major-element composition as an indicator of host-rock type: a machine learning approach using the random forest classifier | SpringerLink
![Figure 3. Garnet compositions in metapelitic rocks are plotted as a function of almandine (Alm), spessartine (Sps), and pyrope (Pyr) end-members. Projection is from grossular. Light gray arrows indicate core-to-rim variations. Arrow Figure 3. Garnet compositions in metapelitic rocks are plotted as a function of almandine (Alm), spessartine (Sps), and pyrope (Pyr) end-members. Projection is from grossular. Light gray arrows indicate core-to-rim variations. Arrow](http://www-odp.tamu.edu/publications/161_SR/chap_19/images/18_f03.jpg)
Figure 3. Garnet compositions in metapelitic rocks are plotted as a function of almandine (Alm), spessartine (Sps), and pyrope (Pyr) end-members. Projection is from grossular. Light gray arrows indicate core-to-rim variations. Arrow
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Minerals | Free Full-Text | Chemical Composition and Genesis Implication of Garnet from the Laoshankou Fe-Cu-Au Deposit, the Northern Margin of East Junggar, NW China
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Composition of garnet from the Yongping Cu skarn deposit, South China: Implication for ore-fluid evolution - ScienceDirect
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Garnet | Birthstones | Gems | Geology & Soils | Online Resources | School of Natural Resources | University of Nebraska–Lincol
An Early Byzantine Engraved Almandine from the Garibpet Deposit, Telangana State, India: Evidence for Garnet Trade Along the Ancient Maritime Silk Road | Gems & Gemology
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