448 resultados para GRANITE
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On verso: Class [sic] to the rear wall of Angell Hall and between Angell and Haven Halls. M-12
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Disbound Original Held in Oak Street Library Facility.
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"Compiled, arranged and printed by direction of Boston, Mass., Walton advertising & printing company."
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Mode of access: Internet.
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Cover title.
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None published 1891, 1905.
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"The greater part of the work, more particularly thos capters dealing with the quarries, has previously appeared in the Builder."
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"An illustrated monthly devoted to the history, story, scenery, industry, and interest of New Hampshire." (Varies slightly.)
Origin of granite in the light of experimental studies in the system : NaAlSi₃O₈=KAlSi₃O₈=Si0₂=H₂O /
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Mode of access: Internet.
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"A New Hampshire magazine devoted to history, biography, literature, and state progress."
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At head of title: Ministère des travaux publics.
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Imprint varies.
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At head of title Jan.-Dec. 1928: New Hampshire State Magazine.
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The Greater Himalayan leucogranites are a discontinuous suite of intrusions emplaced in a thickened crust during the Miocene southward ductile extrusion of the Himalayan metamorphic core. Melt-induced weakening is thought to have played a critical role in strain localization that facilitated the extrusion. Recent advancements in centrifuge analogue modelling techniques allow for the replication of a broader range of crustal deformation behaviors, enhancing our understanding of large hot orogens. Polydimethylsiloxane (PDMS) is commonly used in centrifuge experiments to model weak melt zones. Difficulties in handling PDMS had, until now, limited its emplacement in models prior to any deformation. A new modelling technique has been developed where PDMS is emplaced into models that have been subjected to some shortening. This technique aims to better understand the effects of melt on strain localization and potential decoupling between structural levels within an evolving orogenic system. Models are subjected to an early stage of shortening, followed by the introduction of PDMS, and then a final stage of shortening. Theoretical percentages of partial melt and their effect on rock strength are considered when adding a specific percentage of PDMS in each model. Due to the limited size of the models, only PDMS sheets of 3 mm thickness were used, which varied in length and width. Within undeformed packages, minimal surface and internal deformation occurred when PDMS is emplaced in the lower layer of the model, showing a vertical volume increase of ~20% within the package; whereas the emplacement of PDMS into the middle layer showed internal dragging of the middle laminations into the lower layer and a vertical volume increase ~30%. Emplacement of PDMS results in ~7% shortening for undeformed and deformed models. Deformed models undergo ~20% additional shortening after two rounds of deformation. Strain localization and decoupling between units occur in deformed models where the degree of deformation changes based on the amount of partial melt present. Surface deformation visible by the formation of a bulge, mode 1 extension cracks and varying surface strain ellipses varies depending if PDMS is present. Better control during emplacement is exhibited when PDMS is added into cooler models, resulting in reduced internal deformation within the middle layer.