Chromite-hosted silicate melt inclusions from basalts in the Stravaj complex, Southern mirdita ophiolite belt (Albania)

The Stravaj ophiolite compex, part of the western Mirdita ophiolite belt in Albania, is located east of the Shpati massif, and west of the Shebenik massif. The Stravaj ophiolite sequence itself consist of MOR-related and subductionrelated volcanic rocks (Hoeck et al. 2007) formed by pillow lavas and various dykes.