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

_---_---_ Introduction  Location Previous investigations of altered wallrocks Background geologic studies_-- Acknowledgments.  Methods of investigation Field studies. Laboratory studies. Geologic setting. Precambrian rocks Tertiary rocks_- Structure.  Mineral deposits.- Altered wallrocks. Hydro thermally altered wallrocks_  Supergene alteration and rock weathering-- Width of the altered wallrock zone. Factors that produce variations in the character and distribution of the altered wallrocks- Altered rock minerals-_---_--_ Primary and secondary mineral stability-.__-_-_ Experimental studies of mineral stabilities  Mineral structures and their inheritance  Alteration of representative wallrocks____--Biotite-muscovite granite and microcline-quartzplagioclase-biotite gneiss- Granodiorite and biotite-quartz-plagioclase gneiss._  Quartz diorite Amphibolite_  Garnet-quartz gneiss_--_--Bostonite.i Page 1 2 2 2 3 4 4 4 5 6 6 7 7 7

Altered wallrocks in the central part of the Front Range mineral belt, Gilpin and Clear Creek Counties, Colorado