[16], 495, [1] p. ; Translation of: Trois livres des offices d'estat. ; Reproduction of the original in the Henry E. Huntington Library and Art Gallery.
[16], 458, [2] p. ; A translation of: Discours politiques et militaires du Seigneur de la Noue. ; E.A. = Edward Aggas. ; Publishers' names from colophon, which is dated 1588. ; The last leaf is blank. ; Reproduction of the original in the Henry E. Huntington Library and Art Gallery.
[40] p. ; Signatures: A-E⁴. ; In this edition A2r is signed "Robert Greene" in italic; only sections 11 and 12 are numbered in the text. Quire A outer forme and most of E inner forme are in the same setting as STC 12309. ; Reproduction of the original in the Henry E. Huntington Library and Art Gallery.
[16], 80, 90-195, [6] p. ; Variously attributed to Dudley Fenner and to William Stoughton; sometimes also attributed to Henry Jacob. ; An answer to: Cosin, Richard. An answer to the two first and principall treatises of a certeine factious libell, put foorth latelie, without name of author or printer, and without approbation by authoritie, under the title of An abstract of certeine acts of Parlement: of certeine hir Majesties canons, &c. ; Publication date from STC. ; The last three leaves are blank. ; Running title reads: Of the certaine forme of ecclesiasticall gouernment. ; Reproduction of the original in the Henry E. Huntington Library and Art Gallery.
[32] p. ; Variously attributed to Dudley Fenner and to William Stoughton; sometimes also attributed to Henry Jacob. In the preface (A2 verso) the author speaks of himself as distinct from the author of the, likewise anonymous, book which it supports ("A counter-poyson, modestly written for the time, to make aunswere to the objections and reproches, wherewith the aunswerer to the Abstract, would disgrace the holy discipline of Christ" (STC 10770)), which is also variously attributed to Fenner, Stoughton and Jacob. ; Place of publication and printer's name from STC. ; Signatures: A-B. ; Reproduction of the original in the Yale University. Library.
[11], 103, [6], 76 p. : ill. (woodcuts). ; Printer's name from STC. ; Printer's device on title page, McK. 192; head- and tail-piece, initial. ; The "plates" are woodcuts. ; Includes second part, with separate t.p. and register: Certaine additions to the booke of gunnery, with a supplie of fire-workes. All done by the former author Thomas Smith souldior of Barwicke vpon Tweede: both pleasant and profitable. [device McK. 192] London, Printed for William Ponsonby. 1601. ; Reproduction of the original in the Henry E. Huntington Library and Art Gallery.
The paper describes the permeation of the Croatian language with adjacent languages that were frequently used as languages of political domination or great prestige. The author speaks about the language power of the Croatian South and the Croatian North. In Europe, more precisely in West and Central Europe, there is hardly any other nation on whose territory so many languages were spoken as it is the case with Croatia, especially in its South. However, this fact did not prevent the Croats to become one united nation in the 19th century. The only language with which Croatian was in actual conflict was Hungarian
The idea of hegemony, in its Gramscian sense, contributed to the renewal of several fields of social sciences in the 1970s and 1980s. This idea circulates between different geocultural spaces and different times. The approach adopted in this article starts from the contexts in which this idea is mobilized, in order to show to which theoretical and practical stakes it answers. Focusing on four authors (Antonio Gramsci, Ernesto Laclau, Chantal Mouffe and Pablo Iglesias) and on the transfers from one author to another, the aim is to highlight the social conditions conducive to the deployment of this idea and to identify the (dis)continuities that punctuate its history. Throughout the socio-historical course marked out by the written productions of these four authors, one constant appears: the vitality of the concept of hegemony seems linked to periods of crisis - theoretical and / or strategic - of the left. ; Peer reviewed
The comments of two anonymous reviewers have improved the quality of this manuscript. This study was supported by projects CGL2016-80687-R AEI/FEDER , P18-RT-3275 , B-RNM-301-UGR18 and RNM148 ( Junta de Andalucía/FEDER ). Y.M.M was supported by NASA under award number 80GSFC17M0002 . V.T.S. was supported by the FPU PhD grant ( 16/04038 ). ICM-CSIC author acknowledges the Severo Ochoa funding from the Spanish government through the " Severo Ochoa Centre of Excellence " accreditation ( CEX2019-000928-S ). University of Granada supported this study by funding the APC for publishing as an Open Access articile through an agreement with Elsevier. ; In the Alboran Sea there are a few well exposed Neogene and Quaternary volcanic zones, often geographic highs, that are generally associated with magnetic anomalies. In this paper, we present a characterization of these magnetic anomalies based on a recent and accurate magnetic data compilation for the Abloran Sea area. The anomalies reveal the distribution of magmatism and shed light into the discussion about the origin and evolution of the westernmost Mediterranean. One of the most relevant magnetic anomalies is the Nador dipole, which extends from the Gourougou volcano to the Chafarinas Islands, and is related to an E-W crustal scale intrusion. However, the main NE-SW elongated continuous dipoles of the central Alboran Sea are not related to any surface structure, but they are parallel to the Alboran Ridge, which is the main volcanic high in the Alboran Sea, and are located to the north of it. These anomalies extend discontinuously eastward along the NW-SE dipoles located along the Yusuf fault zone. The results of our 2D magnetic forward modeling suggest that the causative bodies of these main magnetic dipoles are deep igneous bodies. According to the tectonic evolution of the region, and the high magnetic susceptibility values obtained, these igneous bodies probably are made of a basic igneous rocks. Their emplacement may represent the westward tip of the rift axis of the AlKaPeCa Domain, which is related to the Oligocene-Miocene NW-SE extension, and associated with the southern slab retreat stage and oceanic spreading of the Algerian basin. Afterwards, these bodies were displaced toward the west, together with the Alboran Domain, and affected by the STEP fault located at its southern limit. Since the Late Miocene, the north Alboran Ridge elongated intrusions acted as a backstop that conditioned the folding and uplift of the Alboran Ridge in a tectonic indentation setting. In this setting, the STEP fault is deformed and the eastern part of the bodies were segmented along the Yusuf transtensional fault system. Simultaneously, the E-W crustal body related to the Nador magnetic dipole was emplaced, possibly evidencing a slab tearing process. The deep seated basic igneous bodies constitute main crustal heterogeneities that reveal and drive the Alboran Sea tectonic inversion. ; FPU 16/04038 ; Spanish government CEX2019-000928-S ; National Aeronautics and Space Administration 80GSFC17M0002 ; Universidad de Granada ; Junta de Andalucía