Series Principvm Saxonicorvm Et Caesarvm Germanicorvm Omnivm : A Caroli Magni Temporibvs ... Vsqve Ad Nostram Aetatem Contexta

A Davide Chytraeo

Abriss des Hertzogthumbs Mantua und Marggraffschafft Montferath : sampt den angräntzenden Landschafften

Ob d. Buchstabenkombination "P Fin." am Unterrand als Stecherzeichen zu deuten ist, ist unklar

Eroberung der Stadt Breda : Umb den begierigen Leser nicht lang in discurs auffzuhalten, wollen wir allein hie beschreiben ...

Eroberung durch den Prinzen von Oranien, Oktober 1637

Ms. lat. oct. 153 - Theologische Sammelhandschrift

Vorbesitzer: Bernhard Diell;

Ms. lat. oct. 156 - In Thomae de Aquino Summam theologiae, P. III.

Vorbesitzer: Bernhard Diell;

Petrological parameters of sands and sandstones from DSDP and ODP holes in arc-related areas

Detrital modes for 524 deep-marine sand and sandstone samples recovered on circum-Pacific, Caribbean, and Mediterranean legs of the Deep Sea Drilling Project and the Ocean Drilling Program form the basis for an actualistic model for arc-related provenance. This model refines the Dickinson and Suczek (1979) and Dickinson and others (1983) models and can be used to interpret the provenance/tectonic history of ancient arc-related sedimentary sequences. Four provenance groups are defined using QFL, QmKP, LmLvLs, and LvfLvmiLvl ternary plots of site means: (1) intraoceanic arc and remnant arc, (2) continental arc, (3) triple junction, and (4) strike-slip-continental arc. Intraoceanic- and remnant-arc sands are poor in quartz (mean QFL%Q < 5) and rich in lithics (QFL%L > 75); they are predominantly composed of plagioclase feldspar and volcanic lithic fragments. Continental-arc sand can be more quartzofeldspathic than the intraoceanic- and remnant-arc sand (mean QFL%Q values as much as 10, mean QFL%F values as much as 65, and mean QmKP%Qm as much as 20) and has more variable lithic populations, with minor metamorphic and sedimentary components. The triple-junction and strike-slip-continental groups compositionally overlap; both are more quartzofeldspathic than the other groups and show highly variable lithic proportions, but the strike-slip-continental group is more quartzose. Modal compositions of the triple junction group roughly correlate with the QFL transitional-arc field of Dickinson and others (1983), whereas the strike-slip-continental group approximately correlates with their dissected-arc field.

Tena Reyes, Jorge (comp.). Ponencias de la Semana Internacional en Homenaje a Pedro Henríquez Ureña en el cincuentenario de su muerte (1946-1996). Santo Domingo, Editora Corripio C. por A., 1996, 723 p.

Fil: Donnerstag, Guillermo.