Algunas consideraciones sobre la representación de la esfera religiosa en Eneida

En este artículo, se establece una aproximación al estudio de la representación de las formas religiosas en la Eneida en relación con la política augustea de una unidad cívica a través de la organización religiosa. Se considera que dos de las características predominantes de dicha política se reflejan intencionalmente en la Eneida: a) la importancia ritual para establecer el orden cívico; b) la justificación de la política religiosa de absorción, hibridación y supremacía sobre los otros pueblos

Algunas consideraciones sobre la representación de la esfera religiosa en Eneida

En este artículo, se establece una aproximación al estudio de la representación de las formas religiosas en la Eneida en relación con la política augustea de una unidad cívica a través de la organización religiosa. Se considera que dos de las características predominantes de dicha política se reflejan intencionalmente en la Eneida: a) la importancia ritual para establecer el orden cívico; b) la justificación de la política religiosa de absorción, hibridación y supremacía sobre los otros pueblos

Algunas consideraciones sobre la representación de la esfera religiosa en Eneida

En este artículo, se establece una aproximación al estudio de la representación de las formas religiosas en la Eneida en relación con la política augustea de una unidad cívica a través de la organización religiosa. Se considera que dos de las características predominantes de dicha política se reflejan intencionalmente en la Eneida: a) la importancia ritual para establecer el orden cívico; b) la justificación de la política religiosa de absorción, hibridación y supremacía sobre los otros pueblos

Physical oceanography of CTD stations in the Persian Gulf

The following tables show physical and chemical data observed by the "Meteor" in the Persian Gulf and the Strait of Hormus. This study was performed in accordance with the general programme of the International Indian Ocean Expedition (IIOE) during the oeriod from March 25th until April 16th, 1965. The water temperature was measured by reversing thermometers; in most cases two instruments were used simultaneously. The absolute mean temperature difference of this double measurement is 0.0153 °C. The salinity was determined both by salinometer and by titration. In this case of the density, the specific volume anomaly, the dynamic depth anomaly, the sound velocity and the interpolation for standard depths were carried out by the National Oceanographic Data Center (NODC), Washington.

Fission track age determinations of rocks from north Greenland

Apatite fission track (FT) ages and length characteristics of samples obtained from Cambrian to Paleocene-aged sandstones collected along the margin of Nares Strait in Ellesmere Island in the Canadian Arctic Archipelago are dominated by a thermal history related to Paleogene relative plate movements between Greenland and Ellesmere Island. A preliminary inverse FT thermal model for a Cambrian (Archer Fiord Formation) sandstone in the hanging wall of the Rawlings Bay thrust at Cape Lawrence is consistent with Paleocene exhumational cooling, likely as a result of erosion of the thrust. This suggests that thrusting at Cape Lawrence occurred prior to the onset of Eocene compression, likely due to transpression during earlier strikeslip along the strait. Models for samples from volcaniclastic sandstones of the Late Paleocene Pavy Formation (from Cape Back and near Pavy River), and a sandstone from the Late Paleocene Mount Lawson Formation (at Split Lake, near Makinson Inlet) are also consistent with minor burial heating following known periods of basaltic volcanism in Baffin Bay and Davis Strait (c. 61-59 Ma), or related tholeiitic volcanism and intrusive activity (c. 55-54 Ma). Thermal models for samples from sea level dykes from around Smith Sound suggest a period of Late Cretaceous - Paleocene heating prior to final cooling during Paleocene time. These model results imply that Paleocene tectonic movements along Nares Strait were significant, and provide limited support for the former existence of the Wegener Fault. Apatite FT data from central Ellesmere Island suggest however, that cooling there occurred during Early Eocene time (c. 50 Ma), which was likely a result of erosion of thrusts during Eurekan compression. This diachronous cooling suggests that Eurekan deformation was partitioned at discrete intervals across Ellesmere Island, and thus it is likely that displacements along the strait were much less than the 150 km that has been previously suggested for the Wegener Fault.