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- W2086188533 abstract "Abstract Cooling cracks form at high temperatures when a basic magma is either viscous or crystalline and hot. It is postulated that fine-grained margins form along the fractures by release of gas through the fracture network. This takes place ( a ) by raising the liquidus-solidus boundary due to release of volatiles, ( b ) by expansion of the released gas with consequent cooling. Granitic material introduced along the fractures post-dates and may recrystallize the “chilled” margins." @default.
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- W2086188533 date "1965-12-01" @default.
- W2086188533 modified "2023-09-27" @default.
- W2086188533 title "The Role of Cooling Cracks Formed at High Temperatures and of Released Gas in the Formation of Chilled Basic Margins in Net-veined Intrusions" @default.
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- W2086188533 doi "https://doi.org/10.1017/s0016756800000224" @default.
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