| Reference Type | Journal (article/letter/editorial) |
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| Title | VII.—Monzoni and Upper Fassa |
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| Journal | Geological Magazine |
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| Year | 1902 (July) | Series:Volume | 4:9 |
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| Issue | 7 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800181221 |
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| Generate Citation Formats |
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| Mindat Ref. ID | 277488 | Long-form Identifier | mindat:1:5:277488:0 |
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| GUID | 0 |
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| Full Reference | (1902) VII.—Monzoni and Upper Fassa. Geological Magazine, S. 4 Vol. 9 (7) 309-317 doi:10.1017/s0016756800181221 |
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| Plain Text | (1902) VII.—Monzoni and Upper Fassa. Geological Magazine, S. 4 Vol. 9 (7) 309-317 doi:10.1017/s0016756800181221 |
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| In | (1902, July) Geological Magazine S. 4 Vol. 9 (7) Cambridge University Press (CUP) |
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| Abstract/Notes | 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. |
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These are possibly similar items as determined by title/reference text matching only.
