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 Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

The albite and talc-chlorite deposits occurring in central-eastern Sardinia are associated with metasedimentary rocks with intrusions of Hercynian granitoids which contain abundant roof pendants of Palaeozoic metasedimentary rocks. The talc-chlorite bodies are hosted by the roof pendants of mica schists and variably recrystallised metalimestones and metadolostones, whereas deposits of albite generally occur in the granitoids, and to a lesser extent, in the roof pendants represented by mica schists. The talc- and Mg-chlorite deposits are considered to have been formed during the metamorphic event coeval with the emplacement of the granitoid rocks, whereas the albitic bodies were formed during later, post-magmatic, metasomatic processes.

Albite-chlorite and talc-chlorite deposits in metasedimantary and granitoid rocks of central Sardinia (Italy)