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- W1993896103 abstract "The poles to (010) of groundmass feldspar in radial dykes cutting the dissected Miocene volcano, Lyttelton, Banks Peninsula, form generally oblique girdles about the paleo-flow direction. The obliquity is a response to velocity gradients of magma within the dykes, and the sense of obliquity relative to each dyke wall provides a unique determination of the sense of flow. The fabrics give support to the model of Blanchard et al. (1979) for the movement of rigid particles in flowing magmas. This method of flow determination overcomes the problem inherent in most others which provide a flow line but no sense of movement along that line. Methods of sampling and examples of the feldspar fabrics are described together with the relationship of these fabrics to other dyke features such as secondary shears and stretched vesicles." @default.
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- W1993896103 date "1985-06-01" @default.
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- W1993896103 title "Determining paleo-flow directions from groundmass fabrics in the Lyttelton radial dykes, New Zealand" @default.
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- W1993896103 doi "https://doi.org/10.1016/0377-0273(85)90005-8" @default.
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