Critical reappraisal of Late Mesozoic-Cenozoic Central and North Atlantic, Caribbean and Mediterranean evolution

(l) The Pacific basin (Pacific area) may be regarded as moving eastwards like a double zip fastener relative to the continents and their respective plates (Pangaea area): opening in the East and closing in the West. This movement is tracked by a continuous mountain belt, the collision ages of which increase westwards. (2) The relative movements between the Pacific area and the Pangaea area in the W-EfE-W direction are generated by tidal forces (principle of hypocycloid gearing), whereby the lower mantle and the Pacific basin or area (Pacific crust = roof of the lower mantle?) rotate somewhat faster eastwards around the Earth's spin axis relative to the upper mantle/crust system with the continents and their respective plates (Pangaea area) (differential rotation). (3) These relative West to East/East to West displacements produce a perpetually existing sequence of distinct styles of opening and closing oeean basins, exemplified by the present East to West arrangement of ocean basins around the globe (Oceanic or Wilson Cycle: Rift/Red Sea style; Atlantic style; Mediterranean/Caribbean style as eastwards propagating tongue of the Pacific basin; Pacific style; Collision/Himalayas style). This sequence of ocean styles, of which the Pacific ocean is a part, moves eastwards with the lower mantle relative to the continents and the upper-mantle/crust of the Pangaea area. (4) Similarly, the collisional mountain belt extending westwards from the equator to the West of the Pacific and representing a chronological sequence of collision zones (sequential collisions) in the wake of the passing of the Pacific basin double zip fastener, may also be described as recording the history of oceans and their continental margins in the form of successive Wilson Cycles. (5) Every 200 to 250 m.y. the Pacific basin double zip fastener, the sequence of ocean styles of the Wilson Cycle and the eastwards growing collisional mountain belt in their wake complete one lap around the Earth. Two East drift lappings of 400 to 500 m.y. produce a two-lap collisional mountain belt spiral around a supercontinent in one hemisphere (North or South Pangaea). The Earth's history is subdivided into alternating North Pangaea growth/South Pangaea breakup eras and South Pangaea growth/North Pangaea breakup eras. Older North and South Pangaeas and their collisional mountain belt spirals may be reconstructed by rotating back the continents and orogenic fragments of a broken spiral (e.g. South Pangaea, Gondwana) to their previous Pangaea growth era orientations. In the resulting collisional mountain belt spiral, pieced together from orogenic segments and fragments, the collision ages have to increase successively towards the West. (6) With its current western margin orientated in a West-East direction North America must have collided during the Late Cretaceous Laramide orogeny with the northern margin of South America (Caribbean Andes) at the equator to the West of the Late Mesozoic Pacific. During post-Laramide times it must have rotated clockwise into its present orientation. The eastern margin of North America has never been attached to the western margin of North Africa but only to the western margin of Europe. (7) Due to migration eastwards of the sequence of ocean styles of the Wilson Cycle, relative to a distinct plate tectonic setting of an ocean, a continent or continental margin, a future or later evolutionary style at the Earth's surface is always depicted in a setting simultaneously developed further to the West and a past or earlier style in a setting simultaneously occurring further to the East. In consequence, ahigh probability exists that up to the Early Tertiary, Greenland (the ArabiaofSouth America?) occupied a plate tectonic setting which is comparable to the current setting of Arabia (the Greenland of Africa?). The Late Cretaceous/Early Tertiary Eureka collision zone (Eureka orogeny) at the northern margin of the Greenland Plate and on some of the Canadian Arctic Islands is comparable with the Middle to Late Tertiary Taurus-Bitlis-Zagros collision zone at the northern margin of the Arabian Plate.

Critical reappraisal of Late Mesozoic-Cenozoic Central and North Atlantic, Caribbean and Mediterranean evolution

(l) The Pacific basin (Pacific area) may be regarded as moving eastwards like a double zip fastener relative to the continents and their respective plates (Pangaea area): opening in the East and closing in the West. This movement is tracked by a continuous mountain belt, the collision ages of which increase westwards. (2) The relative movements between the Pacific area and the Pangaea area in the W-E/E-W direction are generated by tidal forces (principle of hypocycloid gearing), whereby the lower mantle and the Pacific basin or area (Pacific crust = roof of the lower mantle?) rotate somewhat faster eastwards around the Earth's spin axis relative to the upper mantle/crust system with the continents and their respective plates (Pangaea area) (differential rotation). (3) These relative West to East/East to West displacements produce a perpetually existing sequence of distinct styles of opening and closing ocean basins, exemplified by the present East to West arrangement of ocean basins around the globe (Oceanic or Wilson Cycle: Rift/Red Sea style; Atlantic style; Mediterranean/Caribbean style as eastwards propagating tongue of the Pacific basin; Pacific style; Collision/Himalayas style). This sequence of ocean styles, of which the Pacific ocean is a part, moves eastwards with the lower mantle relative to the continents and the upper-mantle/crust of the Pangaea area. (4) Similarly, the collisional mountain belt extending westwards from the equator to the West of the Pacific and representing a chronological sequence of collision zones (sequential collisions) in the wake of the passing of the Pacific basin double zip fastener, may also be described as recording the history of oceans and their continental margins in the form of successive Wilson Cycles. (5) Every 200 to 250 m.y. the Pacific basin double zip fastener, the sequence of ocean styles of the Wilson Cycle and the eastwards growing collisional mountain belt in their wake complete one lap around the Earth. Two East drift lappings of 400 to 500 m.y. produce a two-lap collisional mountain belt spiral around a supercontinent in one hemisphere (North or South Pangaea). The Earth's history is subdivided into alternating North Pangaea growth/South Pangaea breakup eras and South Pangaea growth/North Pangaea breakup eras. Older North and South Pangaeas and their collisional mountain belt spirals may be reconstructed by rotating back the continents and orogenic fragments of a broken spiral (e.g. South Pangaea, Gondwana) to their previous Pangaea growth era orientations. In the resulting collisional mountain belt spiral, pieced together from orogenic segments and fragments, the collision ages have to increase successively towards the West. (6) With its current western margin orientated in a West-East direction North America must have collided during the Late Cretaceous Laramide orogeny with the northern margin of South America (Caribbean Andes) at the equator to the West of the Late Mesozoic Pacific. During post-Laramide times it must have rotated clockwise into its present orientation. The eastern margin of North America has never been attached to the western margin of North Africa but only to the western margin of Europe. (7) Due to migration eastwards of the sequence of ocean styles of the Wilson Cycle, relative to a distinct plate tectonic setting of an ocean, a continent or continental margin, a future or later evolutionary style at the Earth's surface is always depicted in a setting simultaneously developed further to the West and a past or earlier style in a setting simultaneously occurring further to the East. In consequence, ahigh probability exists that up to the Early Tertiary, Greenland (the ArabiaofSouth America?) occupied a plate tectonic setting which is comparable to the current setting of Arabia (the Greenland of Africa?). The Late Cretaceous/Early Tertiary Eureka collision zone (Eureka orogeny) at the northern margin of the Greenland Plate and on some of the Canadian Arctic Islands is comparable with the Middle to Late Tertiary Taurus-Bitlis-Zagros collision zone at the northern margin of the Arabian Plate.

The sense of ending: the closing of a psychiatric hospital in Lisbon - Hospital Miguel Bombarda

RESUMO: Este estudo foi realizado com o objectivo de conhecer os efeitos da desinstitucionalização dos doentes psiquiátricos crónicos durante o processo de encerramento do Hospital Miguel Bombarda (2007-2011). Este processo incluiu a fusão, em 2008, dos dois principais hospitais psiquiátricos de Lisboa- Hospital Miguel Bombarda (HMB) e Hospital Júlio de Matos (HJM), no Centro Psiquiátrico Hospitalar de Lisboa (CHPL). Foi criado um grupo controlo de pacientes ainda hospitalizados no CHPL (n=166) para comparação com o grupo de casos desinstitucionalizados (n=146). Desta amostra inicial (n=312) apenas 142 (76 casos e 66 controlos) foram incluídos, sendo as principais causas de exclusão: diagnóstico (patologia orgânica, demência ou debilidade mental, como diagnóstico primário) e transferência entre hospitais. A desinstitucionalização foi principalmente avaliada em termos de psicopatologia, utilização de serviços, satisfação, crime, condição de “sem abrigo” ou morte. Os resultados mostraram que a maioria dos doentes crónicos pode sair do hospital psiquiátrico para a comunidade sem agravamento da psicopatologia, aumento do crime ou da condição de “sem abrigo”. A satisfação parece estar aumentada na população desinstitucionalizada. A mortalidade, por outro lado, revelou-se uma questão problemática: apesar de não ter sido possível estabelecer uma comparação entre casos e controlos, a Taxa de Mortalidade Standard encontrada neste estudo foi muito superior ao esperado, de acordo com os resultados encontrados na literatura. Um estudo longitudinal da mesma população poderá ser objecto de futura investigação, possivelmente comparada com outra população similar de um programa de desinstitucionalização noutro país.--------- RÉSUMÉ: Cette étude a été menée afin de déterminer les effets de la désinstitutionnalisation des patients chroniques lors de la fermeture de l'hôpital Miguel Bombarda (2007-2011). Ce processus comprenait la fusion en 2008 de deux grands hôpitaux psychiatriques de Lisbonne: À savoir, Hôpital Miguel Bombarda (HMB) et Hôpital Julio de Matos (HJM), maintenant Centre de l'Hôpital Psychiatrique de Lisbonne (CHPL). Il a été créé un groupe contrôle des patients toujours hospitalisés à CHPL (n = 166) pour comparer avec les cas désinstitutionnalisés (n = 146). De cet échantillon initial (n= 312) à peine 142 (76 cas et 66 contrôles) ont été inclus, les principales raisons d'exclusion: diagnostique (maladie organique, démence ou d'arriération mentale comme diagnostic primaire) et les transferts entre hôpitaux. La désinstitutionnalisation a été principalement évaluée en termes de psychopathologie, de l'utilisation des services, la satisfaction, la criminalité, les “sans abri” et de la mort. Les résultats ont montré que la majorité des malades chroniques peuvent quitter l'hôpital psychiatrique et s´intégrer dans la communauté sans aggravation de la psychopathologie, augmentation de la criminalité ou du nombre de “sans-abri”. La satisfaction semble être en hausse dans la population désinstitutionnalisée. Toutefois, la mortalité s'est avéré être une question problématique, même si il n´a pas été possible d'établir une comparaison entre les cas et les contrôles, le Taux de Mortalité Standard estimé dans cette étude fut beaucoup plus élevé que prévu, en tenant compte des résultats établis dans la littérature. Une étude longitudinale de la même population pourra faire l'objet de futures recherches, peut-être comparé à une population similaire d'un programme de désinstitutionnalisation dans un autre pays. ----------- ABSTRACT:This study was conducted to assess the effects of deinstitutionalization of “long-stay” patients during the process of closing Hospital Miguel Bombarda (2007-2011). This process included the fusion, in 2008, of the two main psychiatric hospitals in Lisbon- Hospital Miguel Bombarda (HMB) and Hospital Júlio de Matos (HJM), into Centro Psiquiátrico Hospitalar de Lisboa (CHPL). A control group of still institutionalized patients in CHPL (n=166) was used as a comparison with the deinstitutionalized population (n=146). Of this 312 initial sample only 142 (76 cases and 66 controls) were included, the main causes of exclusion being diagnoses (organic disease, dementia and mental retardation- as first diagnoses) and transference between hospitals. Deinstitutionalization is mainly evaluated in terms of psychopathology, use of services, satisfaction, crime, vagrancy and deaths. The results show that most long-stay patients can successfully leave psychiatric hospitals and be relocated in the community without an increase in psychopathology, crime or vagrancy. Satisfaction seems to be improved in those patients. On the other hand, mortality remains an issue of concern: Although there was no possibility of comparing it between cases and controls, the Standard Mortality Rate (SMR) in our study was found to be much higher than expected judging by other studies results. A longitudinal further study of this same population will be the matter for a future investigation, possibily compared with another similar population from a desinstitutionalization programme in another country.

Entities delaying payments in times of crisis and its impact on profitability

A Work Project, presented as part of the requirements for the Award of a Masters Degree in Finance from the NOVA – School of Business and Economics

How bank business models relate with risk?: The case of Portugal in times of financial crisis

A Work Project, presented as part of the requirements for the Award of a Masters Degree in Finance from the NOVA – School of Business and Economics

On an organizational level: How can the emergency department at Rouge Valley Centenary hospital improve their wait times?

The prolonged wait times may arguably put into question the Canadian Health Act of 1984. Statistics show throughput wait times are 5.5 hours and output wait times for admitted patients are 32.4 hours. After probing and analyzing best practices through a qualitative/quantitative Value Stream Mapping and a qualitative SWOT Analysis; Team Triage and an Overcapacity Protocol is suggested to improve non-admitted patients wait times by 1.89 hours and admitted patients wait times by 16 hours by eliminating wasteful steps in the patient process and upon overcapacity, effectively sharing already stabilized and admitted patients with all wards in the hospital.