Early Paleozoic tectonic and thermomechanical evolution of ultrahigh-pressure (UHP) metamorphic rocks in the northern Tibetan Plateau, northwest China
Coesite-and diamond-bearing ultrahigh-pressure (UHP) metamorphic rocks represent
continental materials that were once subducted to depths of> 90 km. Identifying how these …
continental materials that were once subducted to depths of> 90 km. Identifying how these …
Petrologic modeling of chloritoid–glaucophane schists from the NW Iberian Massif
Two P–T pseudosections computed with Thermocalc and Perplex software for high-pressure
pelitic Ceán Schists from the NW Iberian Massif show that the paragenesis chloritoid+ …
pelitic Ceán Schists from the NW Iberian Massif show that the paragenesis chloritoid+ …
[HTML][HTML] Natural type-C olivine fabrics in garnet peridotites in North Qaidam UHP collision belt, NW China
Water is known to change the lattice-preferred orientation (LPO) of olivine, which
significantly affects seismic anisotropy in the Earth's upper mantle. Research into the LPO of …
significantly affects seismic anisotropy in the Earth's upper mantle. Research into the LPO of …