Risālat Rafʻ al-ḍarūrah ʻan ḥajj al-ṣayrūrah / li-Sayyidī ʻAbd al-Ghanī al-shahīr bi-al-Nābulusī al-Dimashqī al-Ḥanafī : manuscript

undated.

Risālah fī aḥkām al-ṭāʻūn / li-Ibn al-Ḥājj : manuscript, undated

With: Muqaddimah fī-mā yajibu ʻalá al-awlād maʻrifatuh min al-aḥkām al-sharʻīyah / lil-Faqīh al-Mālikī.

Juzʼ fīhi Arbaʻūn ḥadīthan / li-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.

al- Nahj al-qawīm hadīyah li-man talaqqāhā bi-qalb salīm : manuscript, [ca. 1900]

The text starts with a praise of the Sultan Abdülhamid and his governor Osman Nuri Paşa. Then it discusses the necessity of obedience to the Sultan and the authorities from a religious point of view. It then touches briefly on several ethical issues. The text may or may not be complete at the end.

Kitāb-i Mirʼāt al-muḥaqqiqīn / li-Maḥmūd Jabistarī : manuscript, undated

Cream laid paper with watermarks. 19.9 x 14.3 cm ( x cm.)

Hādhā kitāb al-Thaʻālibī al-musammá bi-Riyāḍ al-ṣāliḥīn wa-tuḥfat al-muttaqīn : manuscript, 1742

بسم الله الرهمن الرحيم وصلى الله على سيدنا محمد وسلم هذا كتاب الثعالبي ... :Incipit

Hâzâ Cezîre-yi Mesnevî li-Hazret-i Mevlânâ : manuscript, 1827

Commentary on Yūsuf Sīneçāk's "Cezīretü'l-Mes̈nevī". Aknowledges indebtedness to Şeyḫ Ġālib's and ʻAbdullāh Bosnevī's commentaries on the work.

Hall-i ebyat-ı müşkilat-ı Celaleddin Rumî / li'ş-Şeyh el-ârif billah Seyyid Emir Buharî : manuscript, [1827]

Commentary on Persian verses composed by Jalāladdīn Rūmī and translation of and commentary on a Greek poem by Rūmī.

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- Ḥāshiyah al-jadīdah ʻalá Fatḥ al-ʻazīz li-ahl al-tamyīz : manuscript, 1686

Copy completed in the hand of Jaʻfar Bīk ibn Farrukh Bīk on 18 Dhū al-Qaʻdah 1097 [October 6, 1686] in Akbarabad.

Itḥāf al-murīdīn li-ʻaqīdat Umm al-burhān : manuscript, [ca. 1755]

Bound with: Sharḥ al-ʻAqīdah al-Sanūsīyah / Muḥammad al-Maʼmūn ibn Muḥammad al-Ḥafṣī (ff. 1v-28v).

Dībājah-ʼi Tafsīr / li-Mawlānā Shaykh Mashāyikh al-Islām Muftī al-zamān farīd al-ʻaṣr wa-al-awān Abū al-Suʻūd Muḥammad al-ʻImādī : manuscript, undated

Foliated 198-202; paginated 1-9, both in Arabic numerals.

U, FE, AND LI ISOTOPE RATIOS IN THE MINERALIZED AND BARREN AREAS OF THE KOMBOLGIE BASIN

The Paleo- to Meso-Proterozoic Jabiluka unconformity related uranium mine is located within the Alligator River Uranium Field, found in the Northern Territories, Australia. The uranium ore is hosted in the late middle Paleoproterozoic Cahill Formation, which is unconformably overlain by a group of unmetamorphosed conglomerates known as the Kombolgie subgroup. The Kombolgie subgroup provided the source for oxidized basinal brines, carrying U as the mobile form U(VI), which interacted with reducing lithologies in the Cahill formation, thus reducing U(VI) to the solid U(IV), and leading to the precipitation of uraninite (UO2). In order to characterize fluid interaction with the ore body and compare that to areas without mineralization, several isotopic tracers were studied on a series of clay samples from drill core at Jabiluka as well as in barren areas throughout the ARUF. Among the potential tracers, three were selected: U (redox sensitive and recent fluid mobilization), Fe (redox sensitive), and Li (fractionated by hydrothermal fluids and adsorption reactions). δ238U values were found to be closely linked to the mineralogy, with samples with higher K/Al ratios (indicating high illite and low chlorite concentrations) having higher δ238U values. This demonstrates that 235U preferentially absorbs onto the surface of chlorite during hydrothermal circulation. In addition, δ234U values lie far from secular equilibrium (δ234U of 30‰), indicating there was addition or removal of 234U from the surface of the samples from recent (<2.5Ma) interactions of mobile fluids. δ57Fe values were found to be related to lithology and spatially to known uranium deposits. Decreasing δ57Fe values were found with increasing depth to the unconformity in a drill hole directly above the ore zone, but not in drill holes in the barren area. Similarly to δ238U, δ7Li is found to correlate with mineralogy, with higher δ7Li values associated with samples with more chlorite. In addition, higher δ7Li values are found at greater depth throughout the basin, indicating that the direction of the mineralizing fluid circulation was upwards from the Cahill formation to the Kombolgie subgroup.