798 resultados para Mus
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Microfilm.
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Microfilm.
Hādhihi Risālah sharīfah wa-nuskhah munīfah fī jawāz ijtimāʻ al-amr wa-al-nahī [microform] /
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Followed by: Hādhihi Risālah sharīfah wa-nuskhah munīqah / min muṣannafāt Ḥusayn al-Khawānsārī (p. 174-220), Hādhihi Risālah ṭarīfah ʻazīzah wa-nuskhah laṭīfah wajīzah fī Shubhat al-istilzām / min taḥqīqāt Ḥusayn al-Khawānsārī (p. 222-250), Hādhihi Taʻlīqah shayyiqah / lil-Muḥaqqiq al-Sabzawārī (p. 251-268), Hādhihi Taʻlīqah rashīqah ... fī al-jawāb ʻan al-īrādāt allatī awradahā ʻalayhi al-Muḥaqqiq al-Khawānsārī fī Risālat Shubhat al-istilzām / al-Muḥaqqiq al-Sabzawārī (269-end).
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His Ḥāshiyat al-Burhān: p. [78]-end.
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Title in text: Miftāḥ bāb al-muwajjahāt.
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Translation of Le livre des martyrs, by Claude Baduel.--Cf. Brit. Mus. Cat.
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Translation of: Constitution and laws of the Muskogee Nation.
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Hain. Repertorium (with Coppingers Supplement) 3971; Gesamtkat. d. Wiegendr. 5543; Brit. Mus. Cat. (XV cent) VIII, p. 135 (IB. 40128)
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Supplementary to the editor's La Pologne historique, littéraire, monumentale et pittoresque. Cf. Brit. Mus.
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Richly elegant copy of the Dīvān of the masterful poet Ḥāfiẓ (Khvājah Shams al-Dīn Muḥammad Shīrāzī, d.1390?).
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Signatures: a-d⁸, e¹�.
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marginal notes/ examined by M. Zacharia 8/24/89."
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Half title; subtitle supplied from Brit. Mus. (Nat. Hist.) Cat.
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Text by James Kennedy. cf. Brit. mus. cat.
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The Shoemaker impact structure, on the southern margin of the Palaeoproterozoic Earaheedy Basin, with an outer diameter of similar to30 km, consists of two well-defined concentric ring structures surrounding a granitoid basement uplift. The concentric structures, including a ring syncline and a ring anticline, formed in sedimentary rocks of the Earaheedy Group. In addition, aeromagnetic and geological field observations suggest that Shoemaker is a deeply eroded structure. The central 12 km-diameter uplift consists of fractured Archaean basement granitoids of syenitic composition (Teague Granite). Shock-metamorphic features include shatter cones in sedimentary rocks and planar deformation features in quartz crystals of the Teague Granite. Universal-stage analysis of 51 sets of planar deformation features in 18 quartz grains indicate dominance of sets parallel to omega (10 (1) over bar3}, but absence of sets parallel to pi (10 (1) over bar2}, implying peak shock pressures in the range of 10-20 GPa for the analysed sample. Geophysical characteristics of the structure include a -100 mus(-2) gravity anomaly coincident with the central uplift and positive circular trends in both magnetic and gravity correlating with the inner ring syncline and outer ring anticline. The Teague Granite is dominated by albite-quartz-K-feldspar with subordinate amounts of alkali pyroxene. The alkali-rich syenitic composition suggests it could either represent a member of the Late Archaean plutonic suite or the product of alkali metasomatism related to impact-generated hydrothermal activity. In places, the Teague Granite exhibits partial to pervasive silicification and contains hydrothermal minerals, including amphibole, garnet, sericite and prehnite. Recent isotopic age studies of the Teague Granite suggest an older age limit of ca 1300 Ma (Ar-Ar on K-feldspar) and a younger age limit of ca 568 Ma (K-Ar on illite-smectite). The significance of the K-Ar age of 568 Ma is not clear, and it might represent either hydrothermal activity triggered by impact-related energy or a possible resetting by tectonothermal events in the region.