Titlebook: Origins of Igneous Layering; Ian Parsons Book 1987 Springer Science+Business Media Dordrecht 1987 chemistry.formation.igneous rock.mineral

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Pattern Formation During Crystallization and the Formation of Fine-Scale Layering,nd in specific associations within the Stillwater Complex. In the Banded series, layer spacing is proportional to crystal grain size, with the best examples of fine-scale layering characterized by coarse rock textures and the development of secondary structures. These latter features include the div

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Solidification Contraction: Another Approach to Cumulus Processes and the Origin of Igneous Layerinpercolation when occurring in a rigid, partially solidified crystal pile. Fluid flow is directed towards the most solidified portion where the pressure drop due to shrinkage is greater. The percolation velocity depends on the depth of the pile; at the top of the pile liquid is dragged rapidly past t

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Laboratory Experiments with Aqueous Solutions Modelling Magma Chamber Processes. I. Discussion of Tts have the advantage that they are simple to carry out in a laboratory and they allow a fundamental understanding to be developed on the principles that control solidification and convection in crystallizing fluid systems. They provide data that can be used to assess general physical theories. Thes

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Laboratory Experiments with Aqueous Solutions Modelling Magma Chamber Processes II. Cooling and Crytion is generated in homogeneous solutions both below an overhanging roof and above an inclined floor. Experiments with a ternary system (FeSO. — Na.SO. — H.O) along a 45° slope showed the same general behaviour.In addition, layering was produced in the solid. Experiments with initially stratified s

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Origins of Igneous Layering978-94-017-2509-5Series ISSN 1389-2185

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