![PDF] Garnet composition and zoning in the determination of temperature and pressure of metamorphism, central Massachusetts | Semantic Scholar PDF] Garnet composition and zoning in the determination of temperature and pressure of metamorphism, central Massachusetts | Semantic Scholar](https://d3i71xaburhd42.cloudfront.net/f6fecf30e52b65bdc3fe9409d9b19684982404e0/10-Table4-1.png)
PDF] Garnet composition and zoning in the determination of temperature and pressure of metamorphism, central Massachusetts | Semantic Scholar
![PDF] Determining chemical composition of the silicate garnets using Raman spectroscopy | Semantic Scholar PDF] Determining chemical composition of the silicate garnets using Raman spectroscopy | Semantic Scholar](https://d3i71xaburhd42.cloudfront.net/9494eeff54bb3ec27466f447e82bde4fe076f6e4/16-Table2-1.png)
PDF] Determining chemical composition of the silicate garnets using Raman spectroscopy | Semantic Scholar
![Figure 5. Garnet compositions in calc-silicate rocks for almandine (Alm), pyrope (Prp), grossular (Grs), spessartine (Sps), and andradite (Adr) components (mineral abbreviations after Kretz, 1983). Solid circles represent garnet grains in equilibrium Figure 5. Garnet compositions in calc-silicate rocks for almandine (Alm), pyrope (Prp), grossular (Grs), spessartine (Sps), and andradite (Adr) components (mineral abbreviations after Kretz, 1983). Solid circles represent garnet grains in equilibrium](http://www-odp.tamu.edu/publications/161_SR/chap_18/images/17_f05.jpg)
Figure 5. Garnet compositions in calc-silicate rocks for almandine (Alm), pyrope (Prp), grossular (Grs), spessartine (Sps), and andradite (Adr) components (mineral abbreviations after Kretz, 1983). Solid circles represent garnet grains in equilibrium
![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 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](https://pub.mdpi-res.com/minerals/minerals-11-00334/article_deploy/html/images/minerals-11-00334-ag.png?1616642032)
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
![Chemical composition, genesis and exploration implication of garnet from the Hongshan Cu-Mo skarn deposit, SW China - ScienceDirect Chemical composition, genesis and exploration implication of garnet from the Hongshan Cu-Mo skarn deposit, SW China - ScienceDirect](https://ars.els-cdn.com/content/image/1-s2.0-S0169136818310047-ga1.jpg)
Chemical composition, genesis and exploration implication of garnet from the Hongshan Cu-Mo skarn deposit, SW China - ScienceDirect
![Minerals | Free Full-Text | Analysis of Garnet by Laser-Induced Breakdown Spectroscopy—Two Practical Applications Minerals | Free Full-Text | Analysis of Garnet by Laser-Induced Breakdown Spectroscopy—Two Practical Applications](https://www.mdpi.com/minerals/minerals-11-00705/article_deploy/html/images/minerals-11-00705-g001.png)
Minerals | Free Full-Text | Analysis of Garnet by Laser-Induced Breakdown Spectroscopy—Two Practical Applications
![Composition of garnet from the Yongping Cu skarn deposit, South China: Implication for ore-fluid evolution - ScienceDirect Composition of garnet from the Yongping Cu skarn deposit, South China: Implication for ore-fluid evolution - ScienceDirect](https://ars.els-cdn.com/content/image/1-s2.0-S0169136821006119-ga1.jpg)
Composition of garnet from the Yongping Cu skarn deposit, South China: Implication for ore-fluid evolution - ScienceDirect
![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)