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VII.—Monzoni and Upper Fassa

Published online by Cambridge University Press:  01 May 2009

M. M. Ogilvie Gordon
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Extract

The following pages present some results obtained by me from the geological survey of the Fassa district in the Dolomites comprising the Bufaure and Monzoni mountain groups, where the porphyritic and monzonitic rocks are widely exposed. In selecting this district I had two objects in view—(1) to study in detail the tectonic relations between the igneous and stratified rocks; (2) to test the results which I had previously obtained from my survey of Sella Massive, etc.

Type
Original Articles
Information
Geological Magazine , Volume 9 , Issue 7 , July 1902 , pp. 309 - 317
Copyright
Copyright © Cambridge University Press 1902

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References

page 309 note 1 I have made no personal examination of the district south of the Pellegrino Valley.Google Scholar