Original language | English |
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Pages (from-to) | 280-281 |
Journal | Geology |
Volume | 27 |
Publication status | Published - 1999 |
Can shatter cones and penetrative deformation lamella form due to explosive volcanic processes? A discussion of Argument supporting explosive igneous activity for the origin of cryptoexplosion structures in the mid-continent, United States
Andrew Glikson
Research output: Contribution to journal › Article › peer-review