| Reference Type | Journal (article/letter/editorial) |
|---|
| Title | The breaking of magma |
|---|
| Journal | Geological Magazine |
|---|
| Authors | Walker, G. P. L. | Author |
|---|
| Year | 1969 (April 20) | Volume | 106 |
|---|
| Issue | 2 |
|---|
| Publisher | Cambridge University Press (CUP) |
|---|
| DOI | doi:10.1017/s0016756800051979Search in ResearchGate |
|---|
| Generate Citation Formats |
|---|
| Mindat Ref. ID | 250051 | Long-form Identifier | mindat:1:5:250051:9 |
|---|
|
| GUID | 0 |
|---|
| Full Reference | Walker, G. P. L. (1969) The breaking of magma. Geological Magazine, 106 (2) 166-173 doi:10.1017/s0016756800051979 |
|---|
| Plain Text | Walker, G. P. L. (1969) The breaking of magma. Geological Magazine, 106 (2) 166-173 doi:10.1017/s0016756800051979 |
|---|
| In | (1969, April) Geological Magazine Vol. 106 (2) Cambridge University Press (CUP) |
|---|
| Abstract/Notes | SUMMARYBreadcrust blocks (bombs) on Vulcano, Sicily, show features which indicate that when they were of viscous lava they broke when stress was applied rapidly, and later flowed when it was applied slowly. If the magma of granitic intrusions behaves similarly, the perplexing “relict dykes” can be explained as due to the breaking of the magma and the injection of dykes into the fractures. |
|---|
These are possibly similar items as determined by title/reference text matching only.
