The El Rosario Quadrangle, situated 100 kilometers northwest of the capital, Tegucigalpa, on the Carretera del Norte, straddles the boundary between the Volcanic Ranges and Plateaus and the Central American Cordillera morphotectonic units, and includes pre-Mesozoic metamorphic rocks, Mesozoic and Tertiary sedimentary rocks, and Tertiary intrusive and volcanic rocks. The oldest rocks exposed are two facies of the pre-Mesozoic Cacaguapa Schist: the Humuya Member of sheared conglomerate, containing evidence of two metamorphic periods, and schist with interlayered, boudinaged meta-andesite; and the Las Marias Member of sericite-quartz schist with inter-layered marble and quartzite. Nonconformably overlying the metamorphic rock are interbedded conglomerate, sandstone, and shale, with intercalated volcanic rocks of the early Mesozoic Todos Santos Formation. The early Cretaceous Yojoa Group of carbonate rock overlies the Todos Santos Formation. Two formations comprise the Yojoa Group: Cantarranas Formation of thin-bedded, marly limestone and the overlying Atima Formation of massive limestone. The Late Cretaceous to early Tertiary (?) Valle de Angeles Group includes red sandstones and shale with minor conglomerate. Padre Miguel Group (Miocene?) siliceous ignimbrite and reworked pyroclastic rock are represented by the La Sabana and Cerro Le Cañada ignimbrite members. The La Sabana ignimbrite has an olivine basalt flow within its lower part. Intrusive igneous rocks include rhyolite with tuffaceous, devitrified-tuff, or granophyric textures, basalt and gabbro dikes, and intruded gabbro. These rocks record three major episodes of deformation: pre-Mesozoic folding and development of schistosity; the Montaña de Comayagua structural belt, a N. 60° W. structural high with high-angle reverse faults formed during the Laramide orogeny; and Tertiary faulting that formed north-trending grabens. The Opoteca silver mine may be the richest mineral deposit within the El Rosario Quadrangle. / text

No description available.

宏都拉斯運用台灣商業經驗的商業發展架構：線上遊戲個案

Thesis (D. Min.)--Southwestern Baptist Theological Seminary, 1991. / Includes bibliographical references (leaves 154-158).

Zugl.: Hohenheim, Univ., Diss., 2007

Thesis (Ph.D.)--State University of New York at Buffalo, 2005. / Title from PDF title page (viewed on Apr. 18, 2006) Available through UMI ProQuest Digital Dissertations. Thesis adviser: Braswell, Geoffrey E. Includes bibliographical references.

No description available.

La Organización de los Estados Americanos (OEA) es la organización regional más antigua del mundo, ya que se remonta a la Primera Conferencia Internacional de Estados Americanos, celebrada en Washington, DC., de octubre de 1889 a abril de 1890 (Carta de la OEA 1948: portada). Es útil puntualizar que la sistematización jurídico-política del Sistema Hemisférico se concretó en 1948 al adoptarse, en Bogotá, la Carta de la Organización de los Estados Americanos (Marchand 2013: 95). / Tesis

Dans de nombreux pays en développement, l’absence de sécurité juridique inhérente à la tenure des terres constitue un obstacle très sévère au développement socio-économique. La faiblesse des mécanismes d’enregistrement des droits réels et d’accès à l’information foncière affecte le fonctionnement du marché immobilier et diminue la confiance de la population envers les interventions étatiques en matière de protection des droits de la propriété foncière. Ceci a pour effet la création d’un marché informel des terres, qui affaiblit le potentiel économique des personnes n’ayant pas une sécurité juridique foncière. Dans un tel contexte, des organismes internationaux comme la Banque mondiale, la Fédération des internationales des géomètres (FIG) et l’Organisation des Nations unies (ONU) encouragent les projets de réforme des processus d’administration des terres, par le développement de nouveaux systèmes cadastraux, intégrés aux registres de la propriété dans un même système d’information foncière, profitant du développement des nouvelles technologies de l’information (Williamson 1997). La présente recherche vise à mettre en évidence les liens conceptuels existants entre la mise en place d’un système d’administration des terres moderne au Honduras. La méthodologie de l’étude de cas est utilisée pour analyser l’application de la Loi hondurienne sur la propriété, adoptée en 2004, et le développement d’un système d’information cadastrale polyvalent. L’hypothèse générale de l’étude stipule que la mise en place d’un système d’information cadastrale polyvalent est une opération préalable et nécessaire à l’atteinte des objectifs de la nouvelle Loi sur la propriété qui vise, notamment à renforcer la sécurité des titres fonciers, la fiscalité municipale et le contrôle de l’usage du sol. Depuis la colonisation espagnole, le système hondurien d’administration des terres a toujours traité le cadastre et le registre de la propriété immobilière comme deux entités distinctes. La nouvelle Loi de 2004 introduit l’obligation de lier juridiquement et techniquement ces deux systèmes qui constituent les outils clés de cette réforme. L’ancien registre des transactions immobilières devient alors un véritable système d’enregistrement des titres de propriété. Cette étude de cas met aussi en évidence l’importance de développer une infrastructure nationale de données géospatiales, afin de soutenir les institutions nationales qui participent aux processus de prise de décisions à caractère territorial (Ting et Williamson 2000). / In many developing countries, the absence of legal safeguards surrounding land tenure constitutes a very sever obstacle to the socio-economic development. The weakness of mechanisms for recording real rights and access to land information affects the operation of land market and decrease the confidence of the population towards the official system of protection of ownership rights. This causes the creation of an informal land market, which generates weak economies located outside of the legal property system. In such a context, international organizations like the World Bank, the International Federation of Surveyors and the United Nations encourage reforms of land administration system, by the development of new cadastral system, integrated into property register in the same land information system, benefiting from the development of new information technologies (Williamson, 1997) Present research aims at highlighting the existing conceptual bonds between the installation of a modern land administration system in Honduras. The methodology of the case study is used to analyze the application of Honduran property Law, which was adopted in 2004. The general hypothesis of the study stipulates that the installation of a multi-purpose cadastral information system is an operation preliminary and necessary to attack the objectives of the new property Law (which aims at reinforcing the safeguards of the land titles, municipal taxation and the control of land use). Since Spanish colonization, the Honduran land administration system has always treated the cadastre and the property register as two distinct entities. The old register of rights transactions thus becomes a true system for recording land title documents. This case study also highlights the importance of developing a national spatial data infrastructure, in order to support the local and national institutions, which take part in the process of decision-making in territorial maters (Ting and Williamson, 2000)

The Valle de Catacamas forms a major basin along the central portion of the Guayape fault, the most prominent tectonic element of the Chortís block. The Guayape fault extends 290 km southwest from the Caribbean coast to the region of El Paraíso, Honduras, and may continue to the Pacific coast along a related prominent topographic feature, the Choluteca linear. Basins presently forming along the Guayape fault indicate that the fault is currently experiencing right-slip. The active features of the Valle de Catacamas displace older folds and reverse faults which apparently formed during an earlier period of sinistral shear. Thus, the Guayape fault has undergone at least two phases of movement, post-Cenomanian left-slip followed by the present right-slip. The geology of the valley suggests multiple stages of evolution. These include at least one period of thrust and reverse faulting, possibly associated with sinistral shear along the Guayape fault, and a recent episode of normal faulting associated with dextral shear on the Guayape fault. Thrusting of basement rocks over Jurassic strata on the south side of the valley was the earliest deformation to affect Mesozoic or Cenozoic rocks. The event can only be dated as post-Jurassic in age. The Cretaceous rocks of the Sierra de Agalta on the north side of the Valle de Catacamas are much more strongly deformed than similar rocks in central Honduras. In this range, the Aptian-Albian Atima Limestone commonly has a pervasive pressure solution cleavage which has not been reported from other locations on the Chortís block. The cleavage is apparently axial planar to the folds. The age of this deformation is constrained only as post-Cenomanian. SIR data indicate that these folds are deflected in sinistral shear near the Guayape fault. In addition, a major structural contact has a large left-lateral separation. The folds in the Sierra de Agalta are cut by the range-bounding normal fault of the Sierra de Agalta. Younger rocks are placed on older rocks by this normal fault, and fault slip data from small fault planes in the footwall block indicate normal faulting. The N 65° E strike of this normal fault, the N 35° E strike of the Guayape fault, and stress orientations inferred from fault slip data indicate that the present movement on the Guayape fault is right-slip. Fault slip data from the Guayape fault zone is heterogeneous as would be expected if two stage slip has occurred. / text