Biennial Report of the Board of Trustees

Mode of access: Internet.

Proceedings of the Mississippi valley historical association

Mode of access: Internet.

Golden gleanings : comprising poems and prose extracts from the writings of M.S. Newcomer.

War lyrics -- Humorous and satirical -- Moral and religious -- Miscellaneous.

Der für die Sünde der Welt Leidende und sterbende Jesus : aus den IV Evangelisten in einem Passions-oratorio /

Signatures: A-⁸ B⁴.

Charter of the province of Pennsylvania.

Mode of access: Internet.

Thomas D. Foster, 1847-1915 : a biography /

Includes bibliographical references and index.

The personal letters of John Fiske;

Introduction by H. H. Harper.

Experiences of a playwright,

Mode of access: Internet.

The whole works of the Right Rev. Jeremy Taylor /

v.1. The life of Taylor. Funeral sermon / by Bishop Rust. Correspondence with Mr. Henry Jeanes. Christian consolations. Indexes -- v.2. The history of the life and death of the Holy Jesus -- v.3. The history of the life and death of the Holy Jesus (cont.) Contemplations of the state of man -- v.4. The rule and exercises of holy living and dying -- v.5-6. Sermons -- v.7. Episcopacy asserted. An apology for authorized and set forms of liturgy. A discourse on the liberty of prophesying -- v.8. A discourse on the liberty of prophesying (cont.) The doctrine and practice of repentance -- v.9. The doctrine and practice of repentance (cont.) Deus justificatus. The real presence of Christ in the holy sacrament -- v.10. The real presence of Christ in the holy sacrament (cont.) A dissuassive from popery -- v.11. A dissuasive from popery (cont.) Letters. A discourse of confimation. A discourse of friendship. Ductor dubitantium; or, The rule of conscience -- v.12-13. The rule of conscience (cont.) -- v.14. The conclusion of the rule of conscience. The divine institution and necessity of the office ministerial. Rules and advices to the clergy -- v.15. The golden grove. The psalter. A collection of offices, or forms of prayer. Devotions for various occasions. The worthy communicant.

Area wage survey.

Title from cover.

The lyrical drama. Essays on subjects, composers, & executants of modern opera.

Extinction of the ballet. Operatic management. Musical agents. Libretti. Operatic and theatrical anomalies. The literary maltreatment of music. Dictionaries of music. Grove's musical dictionary. Quartett concerts and the classical in music. Reasonableness of opera. Tatra Füred, and the music of the Hungarian gipsies. The byeways of bookmaking.

The life and adventures of Olaudah Equiano; or Gustavus Vassa, the African. : From an account written by himself. /

"Juvenile books, published by Samuel Wood & Sons, New York.": page [4] of cover.

Proceedings of the Grand Division.

No more published?

Inheritance of early Archaean Pb-isotope variability from long-lived Hadean protocrust

Comparison of initial Pb-isotope signatures of several early Archaean (3.65-3.82 Ga) lithologies (orthogneisses and metasediments) and minerals (feldspar and galena) documents the existence of substantial isotopic heterogeneity in the early Archaean, particularly in the Pb-207/Pb-204 ratio. The magnitude of isotopic variability at 3.82-3.65 Ga requires source separation between 4.3 and 4.1 Ga, depending on the extent of U/Pb fractionation possible in the early Earth. The isotopic heterogeneity could reflect the coexistence of enriched and depleted mantle domains or the separation of a terrestrial protocrust with a U-238/Pb-204 (mu) that was ca. 20-30% higher than coeval mantle. We prefer this latter explanation because the high-p signature is most evident in metasediments (that formed at the Earth's surface). This interpretation is strengthened by the fact that no straightforward mantle model can be constructed for these high-mu lithologies without violating bulk silicate Earth constraints. The Pb-isotope evidence for a long-lived protocrust complements similar Hf-isotope data from the Earth's oldest zircons, which also require an origin from an enriched (low Lu/Hf) environment. A model is developed in which greater than or equal to3.8-Ga tonalite and monzodiorite gneiss precursors (for one of which we provide zircon U-Pb data) are not mantle-derived but formed by remelting or differentiation of ancient (ca. 4.3 Ga) basaltic crust which had evolved with a higher U/Pb ratio than coeval mantle in the absence of the subduction process. With the initiation of terrestrial subduction at, we propose, ca. 3.75 Ga, most of the greater than or equal to3.8-Ga basaltic shell (and its differentiation products) was recycled into the mantle, because of the lack of a stabilising mantle lithosphere. We argue that the key event for preservation of all greater than or equal to3.8-Ga terrestrial crust was the intrusion of voluminous granitoids immediately after establishment of global subduction because of complementary creation of a lithospheric keel. Furthermore, we argue that preservation of !3.8-Ga material (in situ rocks and zircons) globally is restricted to cratons with a high U/Pb source character (North Atlantic, Slave, Zimbabwe, Yilgarn, and Wyoming), and that the Pb-isotope systematics of these provinces are ultimately explained by reworking of material that was derived from ca. 4.3 Ga (i.e. Hadean) basaltic crust.

Importance of water for Archaean granitoid petrology: a comparative study of TTG and potassic granitoids from Barberton Mountain Land, South Africa

A new model for Archaean granitoid magmatism is presented which reconciles the most important geochemical similarities and differences between tonalite-trondhjemite-granodiorite (TTG) and potassic granitoids. Trace element abundances reveal a strong arc magmatism signature in all studied granitoids from Barberton Mountain Land. Characteristic features include HFSE depletion as well as distinct enrichment peaks of fluid-sensitive trace elements such as Pb in N-MORB normalisation, clearly indicating that all studied granitoids are derived from refertilised mantle above subduction zones. We envisage hydrous basaltic (s.l.) melts as parental liquids, which underwent extensive fractional crystallisation. Distinctive residual cumulates evolved depending on initial water content. High-H2O melts crystallised garnet/amphibole together with pyroxenes and minor plagioclase, but no olivine. This fractionation path ultimately led to TTG-like melts. Less hydrous basaltic melts also crystallised garnet/amphibole, but the lower compatible element content indicates that olivine was also a liquidus phase. Pronounced negative Eu-anomalies of the granitic melts, correlating with Na, Ca and Al, indicate plagioclase to be of major importance. In the context of our model, the post-Archaean disappearance of TTG and concomitant preponderance of granites (s.l.), therefore, is explained with secular decrease of aqueous fluid transport into subduction zones and/or efficiency of deep fluid release from slabs.