English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Plus monthly

Global: Zendy Tools annual

Global: Zendy Tools monthly

Global: Zendy Free Plan

Seismic reflection and geological studies conducted on southern Vancouver Island during 1984 show that the region has sustained considerable shortening above a widespread decollement zone. Beneath Wrangellia, a thick interval of possibly underplated pre-Upper Miocene oceanic crust overlies the modern subducting Juan de Fuca Plate. The latter is clearly seen on all record sections and comprises an undef armed layered sequence resting upon presumed oceanic crust. The Leech River Fault is identified as a surf ace dipping towards the north at 3.5°. Tleneath the fault the Eocene Metchosin Volcanics and Sooke Gabbro are seen to overlie a succession that may have its correlatives in the core zone Olympic Mountains of northern Washington.

Lithoprobe-Phase 1: southern Vancouver Island: preliminary analyses of reflection seismic profiles and surface geological studies