The nature and geodynamic setting of Inner Makran ophiolites (SE Iran) are controversial and are the focus of a growing debate. The Fannuj-Maskutan ophiolite complex (central Inner Makran) is made up
Major and trace element analyses of felsic intrusions into the upper mantle and lowermost crust of the Samail ophiolite, Oman-UAE. Data were collected by the Peter Hooper GeoAnalytical Lab at Washingt
Interdisciplinary Earth Data Alliance (IEDA)2021-02-22 更新30
Text S1 describes the analytical methods used in this study. Figure S1 is the X-ray mappings of garnets from the pelitic migmatites. Table S1 is the chemical compositions of garnet from the studied pe
