Juzʼ fīhi thamānūn ḥadīthan ʻan thamānīn shaykhan / taʼlīf al-Shaykh ... Abī Bakr Muḥammad ibn al-Ḥusayn al-Ājurrī : manuscript, [12--?]

Bound with ʻAlī ibn al-Ḥasan ibn ʻAsākir, Kitāb al-Arbaʻīn al-buldānīyah, and other hadith collections.

Kitāb Nawādir al-zamān fi waqāʼiʻ Jabal Lubnān / taʼlīf Iskandar Afandī Abkāriyūs : manuscript, 1877?

Text is a history of Lebanon in the early 20 century.

al- Murūr bayna al-ʻalamayn ilá mufākharat al-Ḥaramayn / taʼlīf al-shaykh Nūr al-Dīn Abī al-Ḥasan ʻAlī ibn Jamāl al-Dīn Yūsuf al-Zarandī al-Anṣārī al-Madanī al-Ḥanafī : manuscript ; [ca. 1567]

Bound with: Hādhihi al-qaṣīdah al-musammāh bi-Lāmīyat al-ʻajam / lil-Ṭughrāʼī.

Hādhā kitāb Nukhbat al-afkār / taʼlīf al-ʻallāmah Muḥammad ibn Badr al-Dīn al-Kāmilī al-Bayṭār : manuscript, undated

Title from fol. 1r.

al- Juzʼ al-thālith wa-al-arbaʻūn min Sharḥ Kitāb Sībawayh / taʼlīf al-Qāḍī Abī al-Saʻīd al-Ḥasan ibn ʻAbd Allāh al-Sīrāfī : manuscript, [ca. 979]

Written in one column, 18 lines per pages, in black ink.

Kitāb Basṭ al-yadayn li-ikrām al-abawayn / min taṣnīf al-Fāḍil al-Naḥrīr Mawlawī Muḥammad Ghawth ibn Nāṣir al-Dīn ibn Muḥammad : manuscript, 1848 or 9

Title from f. 25r.

al- Juz al-awwal min Asmā al-mubhamah fī al-anbā al-muḥkamah / taṣnīf al-Imām al-Ḥāfiẓ Abī Bakr Aḥmad ibn ʻAlī ibn Thābit al-Khaṭīb al-Baghdādī : manuscript, [12--?]

Bound with ʻAlī ibn al-Ḥasan ibn ʻAsākir, Kitāb al-Arbaʻīn al-buldānīyah, and other hadith collections.

Budūr al-ḍāwīyah fī al-taʻrīf bi-al-sādāt ahl al-Zāwiyah al-Dilāʼīyah : manuscript, undated

بسم الله الرحمن الرحيم وصلى الله على سيدنا ومولانا محمد وآله حدايق الازهار النددية في التعريف باهل الزاوية ... :Incipit

al- Majallah: wa-hiya taḥtawī ʻalá al-qawānīn al-sharʻīyah wa-al-aḥkām al-ʹadlīyah al-muṭābiqah lil-kutub al-fiqhīyah

ḥarrarathā lajnah muʼallafah min al-ʹulamāʼ al-muḥaqqiqīn wa-al-fuqahāʼ al-mudaqqiqīn wa-baʻda an waqaʻat ladá al-Bāb al-ʻĀlī mawqiʻ al-istiḥsān taʻallaqat al-irādah al-sanīyah bi-an takūna dustūr lil-ʻamal bihā.

Mineral, chemical and isotopic compositions of altered rocks at ODP Sites 193-1188 and 193-1189

During ODP Leg 193, 4 sites were drilled in the active PACMANUS hydrothermal field on the crest of the felsic Pual Ridge to examine the vertical and lateral variations in mineralization and alteration patterns. We present new data on clay mineral assemblages, clay and whole rock chemistry and clay mineral strontium and oxygen isotopic compositions of altered rocks from a site of diffuse low-temperature venting (Snowcap, Site 1188) and a site of high-temperature venting (Roman Ruins, Site 1189) in order to investigate the water-rock reactions and associated elemental exchanges. The volcanic succession at Snowcap has been hydrothermally altered, producing five alteration zones: (1) chlorite+/-illite-cristobalite-plagioclase alteration apparently overprinted locally by pyrophyllite bleaching at temperatures of 260-310°C; (2) chlorite+/-mixed-layer clay alteration at temperatures of 230°C; (3) chlorite and illite alteration; (4) illite and chlorite+/-illite mixed-layer alteration at temperatures of 250-260°C; and (5) illite+/-chlorite alteration at 290-300°C. Felsic rocks recovered from two holes (1189A and 1189B) at Roman Ruins, although very close together, show differing alteration features. Hole 1189A is characterized by a uniform chlorite-illite alteration formed at ~250°C, overprinted by quartz veining at 350°C. In contrast, four alteration zones occur in Hole 1189B: (1) illite+/-chlorite alteration formed at ~300°C; (2) chlorite+/-illite alteration at 235°C; (3) chlorite+/-illite and mixed layer clay alteration; and (4) chlorite+/-illite alteration at 220°C. Mass balance calculations indicate that the chloritization, illitization and bleaching (silica-pyrophyllite assemblages) alteration stages are accompanied by different chemical changes relative to a calculated pristine precursor lava. The element Cr appears to have a general enrichment in the altered samples from PACMANUS. The clay concentrate data show that Cr and Cu are predominantly present in the pyrophyllites. Illite shows a significant enrichment for Cs and Cu relative to the bulk altered samples. Considerations of mineral stability allow us to place some constraints on fluid chemistry. Hydrothermal fluid pH for the chloritization and illitization was neutral to slightly acidic and relatively acidic for the pyrophyllite alteration. In general the fluids, especially from Roman Ruins and at intermediate depths below Snowcap, show only a small proportion of seawater mixing (<10%). Fluids in shallow and deep parts of the Snowcap holes, in contrast, show stronger seawater influence.

Mineral analysis and geochemistry of Muehlig-Hofmannfjella granitoids, Central Drooning Maud Land, East Antarctica

Ferrosilite-fayalite bearing charnockite and biotite-hornblende bearing granite are exposed in Mühling-Hofmannfjella, central Dronning Maud Land of East Antarctica. Both are interpreted as essentially parts of a single pluton in spite of their contrasting mineral assemblages. Based on petrologic and geochemical studies, it is proposed that H2O-undersaturated parent magma with igneous crustal component that fractionated under different oxygen fugacity conditions resulted in the Mühlig-Hofmannfjella granitoids.

Whole rock analytical techniques and glas analytical techniques of silicic magmas from the South East Rift, Manus Basin

There has been much recent interest in the origin of silicic magmas at spreading centres away from any possible influence of continental crust. Here we present major and trace element data for 29 glasses (and 55 whole-rocks) sampled from a 40 km segment of the South East Rift in the Manus Basin that span the full compositional continuum from basalt to rhyolite (50-75 wt % SiO2). The glass data are accompanied by Sr-Nd-Pb, O and U-Th-Ra isotope data for selected samples. These overlap the ranges for published data from this part of the Manus Basin. Limited increases in Cl/K ratios with increasing SiO2, La-SiO2 and Yb-SiO2 relationships, and the oxygen isotope data rule out models in which the more silicic lavas result from partial melting of altered oceanic crust or altered oceanic gabbros. Rather, the data form a coherent array that is suggestive of closed-system fractional crystallization and this is well simulated by MELTS models run at 0.2 GPa and QFM (quartz-fayalite-magnetite buffer) with 1 wt % H2O, using a parental magma chosen from the basaltic glasses. Although some assimilation of altered oceanic crust or gabbro cannot be completely ruled out, there is no evidence that this plays an important role in the origin of the silicic lavas. The U-series disequilibria are dominated by 238U and 226Ra excesses that limit the timescale of differentiation to less than a few millennia. Overall, the data point to rapid evolution in relatively small magma lenses located near the base of thick oceanic crust; we speculate that this was coupled with relatively low rates of basaltic recharge. A similar model may be applicable to the generation of silicic magmas elsewhere in the ocean basins.

Element concentrations of aluminosilicate components from ODP sites in the Pacific Ocean

We measured major and trace element concentrations in the operationally defined, chemically extracted, residual aluminosilicate component of sediment from Ocean Drilling Program Sites 1215 and 1256 in the central and eastern equatorial Pacific Ocean and found that this residual component contains volcanogenic and authigenic aluminosilicates in addition to inferred eolian material. While the residual component younger than 20 Ma from the central Pacific (ODP Site 1215) is similar compositionally to upper continental crust and suggests an increase in the delivery of Asian dust material since 20 Ma, the residual in sediment older than 20 Ma indicates significant amounts of volcanogenic and authigenic materials. Volcanogenic debris comprises as much as ~ 40% of the residual between 23-40 Ma, which coincides with the mid-Tertiary "ignimbrite flare-up" that occurred in much of western North America. The residual component extracted from the 50 Ma biogenic sediment reflects authigenic signatures (seawater-like negative cerium anomalies and elevated Fe/Si ratios). The previously interpreted increase in an andesitic detrital source in North Pacific locations may instead be authigenic material, presenting significant challenges for many paleoclimate proxies. Additionally, in the eastern Pacific (ODP Site 1256), the residual component contains ~70% of volcanogenic material, most likely originating from Central America, and also includes refractory barite. The ability to separately identify eolian, volcanogenic, and authigenic materials in the aluminosilicate component of pelagic sediment allows resolution, respectively, of the climatic, geologic, and chemical processes contributing to the paleoceanographic archive in this critical oceanic region.