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Titlebook: Introduction to Small~scale Geological Structures; Gilbert Wilson Book 1982 G. Wilson 1982 formation.fossil.fracture.history.stratigraphy.

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Mullion and rodding structures, telegraph poles to those of walking sticks, lie parallel to each other down the dip slope of the Moine Schists. Where minerals of elongated habit like hornblende or biotite are present in the rocks showing mullion or rodding structure the crystals are arranged parallel to each other and to the dip and plunge of the folds.
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Superposed minor structures,inor structures. If, therefore, we observe that one set of minor structures regularly deforms another we have an indication that more than one movement has taken place. Then, if we can link these minor structures with their respective major structures, we will have taken a long step in the elucidation of the tectonic history of our area.
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Conclusions,ave written. I have endeavoured to describe the small-scale structures which he is liable to meet, and to discuss their uses and limitations in elucidating the geometry and tectonic history of an area.
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Drag-folds and parasitic folds,ed or asymmetrical minor folds, the axes of which lie at right angles to the direction of movement. The sense of the movement is indicated by the inclination of the axial planes or the . of the folds: they are typical monoclinic structures (Fig. 3.1c).
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Gilbert Wilsonayers of government deriving from tax and enforcement policies, and network effects in these fields may trigger waves of amnesties. Amnesties can provide a source of information about taxpayers’ actual income distribution and the relationship between income and tax evasion.
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