Metadata
Author: springer
Data
English[en]
Serpentinites and mafic schists representing fragmented ophiolites are common throughout a broad, highly magnetic central zone which separates a low-magnetic metaturbidites terrain in the Northeast from a southwestern, low susceptibility, metavolcanic rich area with isolated anomalies.
Spanish[es]
Las serpentinitas constituyen parte de una asociación »ofiolítica« fragmentada que aflora dentro de una ancha banda entre metaturbiditas débilmente magnéticas al NE y metapiroclastitas con aisladas anomalías al SW.