... ). In a recent study, which used detailed field mapping, petrography and spinel mineral chemistry, Guice et al . (2018 a ) interpreted the Ben Strome Complex as representing a layered intrusion emplaced into the tonalite–trondhjemite–granodiorite (TTG)-dominated crust prior to granulite facies metamorphism...

... granu- lites. This boundary trends north-west from north of Ben Strome (NC 24o36o ) to south of Port of Tarbet (i 62483). The gently dipping gneisses on its southern side are traversed by several nearly vertical shear zones with westerly strikes which curve clockwise into the south-east trend...

...-element anomalies as a proxy for Archaean subduction: Evidence from the Ben Strome Complex, NW Scotland : Geosciences , v. 8 , 338 , https://doi.org/10.3390/geosciences8090338 . Guice , G.L. , McDonald , I. , Hughes , H.S.R. , and Anhaeusser , C.R. , 2019 , An evaluation...

...-arc the provincial capital of Osh, which is part of the Kyrgyz Republic for signifi- accretionary complex, which was sub- the second largest city in the Kyrgyz cant Carlin-type gold deposits. Republic (Fig. 1). Gold exploration in jected to intense folding to page 14 . . . the region during the past...

... depositional provinces are the Waterways basin, the Swa n Hills Member platform and bank complex, and the carbonate shelf com- plex which formed during Swan Hills time in west-central Alberta (Fig . 3) . Each of these depositional provinces is characterized by a distinc t facies and distribution pattern...