The Apuseni Mts. is a key area to study the interplay between intra-continental extensional tectonics, sedimentation, and magmatism. These events occurred from ~14.5 to 7 Ma, covering the collision of
The high-temperature–low-pressure (HTLP) Wongwibinda Metamorphic Complex (WMC) hosts four distinct types of early Permian S-type granitoids belonging, or related, to the Hillgrove Supersuite. We use f
