A pictorial introduction to coarse-grained symplectites in low-temperature jadeitite from Guatemala

Tatsuki Tsujimori, Juhn G. Liou, Robert G. Coleman
2004 Chishitsugaku zasshi  
Symplectite textures are common product of retrogression in the intermediate-to high-temperature metamorphic rocks such as granulite and eclogite, and contain important information on the P-T histories. Their formation mechanisms are generally attributed to
doi:10.5575/geosoc.110.9.xvii_xviii fatcat:oiqeifwb3bgi3e6n6ikbekonnu