Beati Alberti Magni ... Super Missus quaest. CCXXX ; De laudibus B. Mariae Lib. XII ; Biblia Mariana ... /

Mode of access: Internet.

Antologia portugueza : trechos selectos coordenados sob a classificação dos generos litterarios /

Includes indexes.

Gli illustri viaggiatori italiani con una antologia dei loro scritti.

Mode of access: Internet.

The cause and cure of a wounded conscience ; also Triana, or, A threefold romanza, of Mariana, Paduana, and Sabina ; Ornithologie, or, The speech of birds ; and Antheologia, or, The speech of flowers /

"The cause and cure" (first published 1647) has special t.-p. with identical imprint; "Triana", "Ornithologie" and "Antheologia" have each special t.-p. with imprint: London, Printed for John Stafford (dated, respectively, 1664, 1655 and 1655).

Oracion funebre panegyrica de las exequias que a sus expensas ofreciò la ... ciudad de Malaga à ... la Señora Reyna Viuda Doña Mariana de Neoburg, en la Santa Iglesia Cathedral ... el dia 26 de agosto de el presente año de 1740 /

Mode of access: Internet.

The late, and much admired play, called Pericles, Prince of Tyre [microform] : with the true relation of the whole historie, adventures, and fortunes of the said prince : as also the no lesse strange and worthy accidents, in the birth, and life of his daughter Mariana /

"As it hath been divers and sundry times acted by His Majesties servants, at the Globe on the Banck-side."

Dramaty staropolskie; antologia.

Mode of access: Internet.

A geochemical study of crustal plutonic rocks from the southern Mariana Trench forearc: Relationship to volcanic rocks erupted during subduction initiation

Two suites of intermediate-felsic plutonic rocks were recovered by dredges RD63 and RD64 (R/V KK81-06-26) from the northern wall of the Mariana trench near Guam, which is located in the southern part of the Izu-Bonin-Mariana (IBM) island arc system. The locations of the dredges are significant as the area contains volcanic rocks (forearc basalts and boninites) that have been pivotal in explaining processes that occur when one lithospheric plate initially begins to subduct beneath another. The plutonic rocks have been classified based on petrologic and geochemical analyses, which provides insight to their origin and evolution in context of the surrounding Mariana trench. Based on whole rock geochemistry, these rocks (SiO2: 49-78 wt%) have island arc trace element signatures (Ba, Sr, Rb enrichment, Nb-Ta negative anomalies, U/Th enrichment), consistent with the adjacent IBM volcanics. Depletion of rare earth elements (REEs) relative to primitive mantle and excess Zr and Hf compared to the middle REEs indicate that the source of the plutonic rocks is similar to boninites and transitional boninites. Early IBM volcanic rocks define isotopic fields (Sr, Pb, Nd and Hf-isotopes) that represent different aspects of the subduction process (e.g., sediment influence, mantle provenance). The southern Mariana plutonic rocks overlap these fields, but show a clear distinction between RD63 and RD64. Modeling of the REEs, Zr and Hf shows that the plutonic suites formed via melting of boninite crust or by crystallization from a boninite-like magma rather than other sources that are found in the IBM system. The data presented support the hypothesis that the plutonic rocks from RD63 and RD64 are products of subduction initiation and are likely pieces of middle crust in the forearc exposed at the surface by faulting and serpentine mudvolcanoes. Their existence shows that intermediate-felsic crust may form very early in the history of an intra-oceanic island arc system. Plutonic rocks with similar formation histories may exist in obducted suprasubduction zone ophiolites and would be evidence that felsic-intermediate forearc plutonics are eventually accreted to the continents.

Description of manganese deposits from the Papago mine, Saipan, Mariana Islands

Saipan, situated about 15° N. and 146° E., is one of the larger and more southerly of the Mariana Islands. The 15 small islands of this chain are strung along an eastwardly convex ridge for more than 400 miles north to south, midway between Honshu and New Guinea and about 1,200 miles east of the Philippines. Paralleling this ridge 60 to 100 miles further east is a deep submarine trench, beyond which lies the Pacific Basin proper. To the west is the Philippine Sea, generally deeper than 2,000 fathoms. The trench coincides with a zone of negative gravity anomalies, earthquake foci occur at increasing depths westward from it, and silica- and alumina-rich volcanic rocks characterize the emergent island chain itself. The contrast between these features and those of the Pacific Basin proper to the east is held to favor the conclusion that the Mariana island arc and trench define the structural and petrographic front of Asia.