Petrographical classification and mineral assemblage of basement clasts from the Quaternary and Miocene sections of sediment core CRP-1 (Table 1)

Petrographical and mineral chemistry data are described for the mist representative basement lithologies occurring as clasts (pebble grain-size class) from the CRP-1 drillhole. Most pebbles consits of either undeformed or foliated biotite with or without hornblende monzogranites. Other rock types include biotite with or without garnet syenogranitr, biotite-hornblende granodiorite, tonalite, monzogranitic porphyries, haplogranite, quartz-monzonite (restricted to the Quaternary section), Ca-silicate rocks and biotite amphibolite (restricted to the Miocene strata). The common and ubiquitous occurence of biotite with or without hornblende monzogranite pebbles, in both the Quaternary and Miocene sections, apparently mirrors the dominance of these rock types in the granitoid assemblages which are presently exposed in the upper Precambrian-lower Paleozoic basement of the south Victoria Land. The other CRP-1 pebble lithologies show petrographical features which consitently support a dominant supply from areas of the Transantarctic Mountains located to the west and south-west of the CRP-1 site, and they thus furthercorroborate a model of local provenance for the supply of basement clasts to the CRP-1 sedimentary strata.

Clay mineralogy of ODP Site 131-808 sediments

Drill core recovered at Ocean Drilling Program Site 808 (Leg 131) proves that the wedge of trench sediment within the central region of the Nankai Trough comprises approximately 600 m of hemipelagic mud, sandy turbidites, and silty turbidites. The stratigraphic succession thickens and coarsens upward, with hemipelagic muds and volcanic-ash layers of the Shikoku Basin overlain by silty and sandy trench-wedge deposits. Past investigations of clay mineralogy and sand petrography within this region have led to the hypothesis that most of the detritus in the Nankai Trough was derived from the Izu-Honshu collision zone and transported southwestward via axial turbidity currents. Shipboard analyses of paleocurrent indicators, on the other hand, show that most of the ripple cross-laminae within silty turbidites of the outer marginal trench-wedge facies are inclined to the north and northwest; thus, many of the turbidity currents reflected off the seaward slope of the trench rather than moving straight down the trench axis. Shore-based analyses of detrital clay minerals demonstrate that the hemipelagic muds and matrix materials within sandy and silty turbidites are all enriched in illite; chlorite is the second-most abundant clay mineral, followed by smectite. In general, the relative mineral percentages change relatively little as a function of depth, and the hemipelagic clay-mineral population is virtually identical to the turbidite-matrix population. Comparisons between different size fractions (<2 µm and 2-6 µm) show modest amounts of mineral partitioning, with chlorite content increasing in the coarser fraction and smectite increasing in the finer fraction. Values of illite crystallinity index are consistent with conditions of advanced anchimetamorphism and epimetamorphism within the source region. Of the three mica polytypes detected, the 2M1 variety dominates over the 1M and 1Md polytypes; these data are consistent with values of illite crystallinity. Measurements of mica bo lattice spacing show that the detrital illite particles were eroded from a zone of intermediate-pressure metamorphism. Collectively, these data provide an excellent match with the lithologic and metamorphic character of the Izu-Honshu collision zone. Data from Leg 131, therefore, confirm the earlier interpretations of detrital provenance. The regional pattern of sediment dispersal is dominated by a combination of southwest-directed axial turbidity currents, radial expansion of the axial flows, oblique movement of suspended clouds onto and beyond the seaward slope of the Nankai Trough, and flow reflection back toward the trench axis.

(Table 1) Heavy mineral content in sediments of the southern Mediterranean Ridge, Nile Cone and Egyptian Shelf

Petrographic analysis of Quaternary terrigenous sand layers in eastern Mediterranean cores reveals distinct mineralogical differences between the Egyptian Shelf-Nile Cone region and the southern part of the Mediterranean Ridge. A compositionally and texturally immature suite in Ridge cores, mixed with a Nile-derived assemblage, identifies a fresh non-recycled mineral component derived from proximal igneous and metamorphic surface or near-surface exposures, probably in the south-central Ridge area rather than from distal African sources. The presence of such basement terrains would be consistent with a compressive thrust-belt origin for this part of the Mediterranean Ridge.

Composition of sedimentary rocks from the Shapkina River valley, Bolshezemelskaya Tundra

A facies-genetic and stratigraphic subdivision of the Quaternary sequence in the Shapkina River valley has been accomplished. The riverbank shows outcrops of three glacial complexes with different mineralogical-petrographic compositions and structural characteristics, which can be correlated and stratificated. Datings of intermoraine horizons (alluvial, marine, lacustrine, and lacustrine-boggy sediments) have been based on palynological and paleomicrotheriological data. The Middle Neopleistocene section can be divided into two till horizons corresponding to two autonomous glaciations (Pechora and Vychegda). They are separated by a member of subaqueous Rodionov sediments. The Pechora till formed in the course of glacier motions from the northeast. Glacial horizons are mainly composed of the Vychegda till transported from the Northwest terrigenous provenance. Lithology of the Upper Neopleistocene Polyarnyi till testifies to its formation in the upper course of the river from material transported from the Northeast terrigenous-mineralogical provenance in the upper course of the river and from the Fennoscandian glaciation center in the lower course of the river. The paper presents the first lithological investigation and substantiation of genesis of various facies of Neopleistocene intermoraine marine sediments (sediments of the beach and fore-beach zones and shallow-water shelf).

Los estetas de Teópolis : novela /

RBC: "Juan Como Pascual Barcelona"--Stamp on half t.p.

Obseruationes in constitutiones dominij Mediolanensis /

Acquisition made accessible thanks to a 2015-2017 grant from the Council on Libraries and Information Resources.

Iosephi Francisci RezzolI presbyteri inscriptiones.

Acquisition made accessible thanks to a 2015-2017 grant from the Council on Libraries and Information Resources.

University of Michigan Class of 1889

On verso: Taken Saturday A.M.; May 11, 1889; Property of Minnie H. Newby. Randall, Photographer ... Fine Art Goods (?) 30 E. Huron St. Ann Arbor, Mich. Additional documentation (re: names and provenance) available in folder

R.P. Francisci Suarez, Granatensis, e Societate Iesu doctoris theologi, et in Connimbricensi Academia Sacrarum Literarum primarii professoris opus, De virtute et statu religionis. Quo quid contineatur, index proximus indicabit.

Also issued as part of collection with collective title page, engraved portrait of author, biographical preface, and contents list: "R.P. Francisci Suarez Granatensis, e Societate Iesu Doctoris Theologi, et in Regia Conimbricensi Academia primarij theologiae professoris emeriti Opera omnia quorum cathalogum vide lector in vita authoris. Moguntiae, Sumptibus Hermanni Mylij Birckmanni Excudebat Balthasar Lippius. Anno M. DCXXI."

Theologiae R.P. Fr. Suarez e Societate Jesu, summa, seu compendium /

Table of contents at end of each volume.

Doct. Francisci Suarez Granatensis, ex Societate Iesu, Tractatus theologicus, de vera intelligentia auxilii efficacis, eiúque concordia, cum libero arbitrio : opys posthumum, ad stabiliendas definitiones fidei, à S.D.N. Innocentio X. contra Iansenium eiéusque partiarios, editas, accommodatum : prodit nunc primum.

Errors in pagination: nos. 201, 265-266, and 414 numbered respectively 191, 267-268, and 408; nos. 276-277 omitted.

R.P. Francisci Suarez Granatensis, e Societate Iesu Doctoris Theologi; et in Conimbricensi Academia Sacrarum Litterarum olim Primarij Professoris Emeriti De diuina gratia pars prima[-postrema] : continens prolegomena sex, & duos priores libros de necessitate diuinæ gratiæ ad honesta opera.

Signatures: vol. 1: )(⁶ A-Z⁶ 2A-2P⁶ 2Q⁴; vol. 2: )(² A-Z⁶ 2A-2Z⁶ 3A-3C⁶ 3D⁸ (3D₈ blank).

Doctoris Francisci Suarez Granatensis, de Societate Iesu ... Varia opuscula theologica : 1. De concursu, motione, & auxilio Dei. lib. III. 2. De scientia Dei futurorum contingentium. lib. II. 3. De auxilio efficaci. Breuis resolutio. 4. De libertate diuinae voluntatis. Relectio prior. 5. De reuiuiscentia meritorum. Relectio altera. 6. De iustitia Dei . Disputatio. : cum indice gemino, vno locorum sacræ Scripturæ altero rerum.

Includes index.

R.P. Francisci Suarez, Granatensis, e Societate Iesu doctoris theologi, et in Conimbricensi Academia sacrarum literarum primarij professoris. Defensio fidei Catholicae et apostolicæ aduersus Anglicanæ sectæ errores. : Cum responsione ad Apologiam pro Iuramento fidedelitatis, & præfationem monitoriam sernessimi Iacobi Magnæ Britanniæ Regis. Ad serenissimos totius Christiani orbis Catholicos reges et principes.

Includes index.

R. P. Francisci Suarez, Granatensis, e Societate Iesu doctoris theologi, et in Conimbricensi Academia olim primarij theologiae professoris emeriti, Opus de triplici virtute theologica, fide, spe, et charitate : in tres tractatus, pro ipsarum virtutum numero distributum ...

Title page printed in red and black; title vignette (Jesuit device); head- and tailpieces; initials; printed marginalia.