Contact Metamorphism in the Highlands


Autoria(s): Trask, Frank, Jr.
Data(s)

04/05/1936

Resumo

On the southern margin of the Boulder Batholith, about twenty miles south of Butte in the Highland Mountains, there are many miles of contact between the igneous and sedi­mentary rocks. As two kinds of igneous rocks and many diff­erent kinds of sedimentary rock are present, it is an excell­ent place for the study of contact metamorphism.

Formato

application/pdf

Identificador

http://digitalcommons.mtech.edu/bach_theses/62

http://digitalcommons.mtech.edu/cgi/viewcontent.cgi?article=1061&context=bach_theses

Publicador

Digital Commons @ Montana Tech

Fonte

Bachelors Theses and Reports, 1928 - 1970

Palavras-Chave #Boulder Batholith #Butte #Highland Mountains #Montana #magma #limestone #Ceramic Materials #Environmental Engineering #Geology #Geophysics and Seismology #Metallurgy #Other Engineering #Other Materials Science and Engineering
Tipo

text