NEW AGES AND TECTONIC HISTORY FOR THE TRINITY TERRANE, A POLYGENETIC OPHIOLITIC COMPLEX, KLAMATH MOUNTAINS, CALIFORNIA
1) Scott River block – Ediacaran oceanic plagiogranite formed 571-565 Ma;
2) China Mountain block – Early to Late Ordovician oceanic layered gabbro, dikes + plagiogranite, pillow basalt;
3) Trinity River block – pre-Early Ordovician mantle intruded by Early Ordovician and Siluro-Devonian plutons;
4) Siluro-Devonian SSZ (Supra-Subduction Zone) ophiolite sequence of pegmatitic gabbro-sheeted dikes-pillow basalt built about 435-412 Ma after 1-3 were juxtaposed.
5) Trinity Alps block, sutured to 1-4 after the Siluro-Devonian SSZ component formed.
Ordovician tectonic history is intraoceanic but these rocks exhibit a wide range of tectonic styles and deformation intensity. Because the ages do not correlate with type and degree of deformation we suspect formation within a complex oceanic rifting and transform fault environment involving multiple microplates and triple junctions.
The Forest Mountain terrane west of Yreka represents a separate slab of oceanic lithosphere that underthrust the Yreka-Trinity composite terrane in Early Devonian (~407-398 Ma).