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A chilled margin is a shallow intrusive or volcanic rock texture characterised by a glassy or fine-grained zone along the margin where the magma or lava has contacted air, water, or particularly much cooler rock. This is caused by rapid solidification of the melt near the contact with the surrounding low temperature environment. In an intrusive case, the…
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chilled margins intrusive glassy magma margin water contact often volcanic rock fine-grained lava dikes sills shallow texture characterised zone along
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Chilled margin | is a | shallow intrusive or volcanic rock texture characterised by a glassy or fine-grained zone along the margin where the magma or lava has contacted air | 0.90 | text |
| Chilled margin | related to External links | Huppert | 0.60 | section |
| Chilled margin | related to External links | Sparks | 0.60 | section |
| Chilled margin | related to External links | Chilled | 0.60 | section |
| Chilled margin | related to External links | Earth | 0.60 | section |
| Chilled margin | related to External links | Planetary Science Letters | 0.60 | section |
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