The Sarn Complex is a group of closely related igneous rocks that intrude and cut through other rock lithologies in the Cymru Terrane in Wales.[1] The complex outcrops on the Llyn Peninsula in a variety of places including Mynydd Cefnamlwch and the flanks of Pen y Gopa.[2]
The largest plutonic body in the terrane has limited outcrop and is sheared by the Llyn Shear Zone in the west and covered by later (Arenig) sediments to the east.[1] Altered to greenschist facies the pluton contains a bimodal suite of gabbro-diorite, monzogranite (Sarn Granite) and granodiorite.
The Sarn Granite is leucocratic and covers an expanse of about 6 km2 in contrast to the gabbro and diorite that exist as small and scattered exposures. The dioritic component of the complex has been confirmed as having a Neoproterozoic age of 614 ±2 Ma using U-Pb zircon dating.[3] Therefore, the shearing of the Llyn is also temporally constrained by the date.