Universitas Syiah Kuala

Mélange diapir origin for Neo-Tethyan ridge-subduction magmatism

The mélange diapir model invokes physical mixing of partially melted slab components with mantle wedge peridotite, enabling material transfer from the subducted slab to the overlying mantle wedge. However, identifying distinctive igneous rock suites generated through this process...

Global research landscape of transformative learning in pre-service teacher education: A Scopus-based bibliometric and science-mapping analysis

<ns5:p>Background Transformative learning explains changes in pre-service teachers’ frames of reference, yet previous mapping studies have examined the theory broadly, within higher education, or in specific domains such as sustainability. This study maps the development, contrib...