Back to Results
First PageMeta Content
Geologic formations / Petrology / Sedimentary rock / Turbidite / Beardmore Glacier / Transantarctic Mountains / Beacon sandstone / Geology / Geography of Antarctica / Dufek Coast


canic detritus, derived from a caic-alkaline arc along the paleoPacific margin, became the principal component in sandstone. This change from cratonic to orogenic provenance was the result of a shift in the basin axis to
Add to Reading List

Document Date: 2011-05-06 07:07:21

Open Document

File Size: 3,16 MB

Share Result on Facebook

City

Washington / D.C. / Boulder / Oxford / /

Company

The Beacon Supergroup / Ferrar Group / Beacon Group / New Zealand Journal / /

Continent

America / Antarctica / /

Country

United States / New Zealand / /

Facility

J.W. COLLINSON Byrd Polar Research Center Ohio State University / /

NaturalFeature

Transantarctic Mountains / Beardmore Glacier / Baltic Sea / Ross Sea / Ellsworth Mountain / Ellsworth Mountains / /

Organization

American Geophysical Union / MOLLY F. MILLER Department of Geology Vanderbilt University Nashville / International Association of Sedimentologists / National Science Foundation / J.W. COLLINSON Byrd Polar Research Center Ohio State University Columbus / /

Person

Molly F. Miller / Maud Range / Julia M.G. Miller / Coarsening Upwards / James W. Collinson / /

Position

Major / Queen / /

ProvinceOrState

Tennessee / Ohio / Colorado / /

Region

New Zealand Antarctic / Antarctic / /

SportsLeague

International Association / /

Technology

Geophysics / /

SocialTag