Jesuit Schools and Missions in the Orient

On 27th February 1540, the Papal Bull Regimini Militantis Eclesiae estabilished the oficial institution of The Society of Jesus, centred on Ignacio de Layola. Its creation marked the begining of a new Order that would accomplish its apostolic mission through education and evangelisation. The Society´s first apostolic activity was in service of the Portuguese Crown. Thus, Jesuits became involdev within the missionary structure of the Portuguese Patronage and ended up preaching massively across non-European spaces and societies

Play the cards, roll the dice – the integration of casinos within Asian tourism destination development strategy

New Asian casino destinations continue to emerge and expand their gambling options. The historical rhetoric of being a panacea to economic and tourism woes continues to dominant decades later. Yet the excessive regulatory environments and taxation regimes by authorities on the casino industry are unlike those applied to other destination tourism products. Once the domain of the United States in the 1990s with entertainment capitals such as Las Vegas and Atlantic City, the proliferation of legalised casino gaming is now accentuated in Asia in destinations such as Macao, Korea, Singapore and the Philippines. As a tourism product, this article highlights that the arguments for and against casinos are narrowly embedded in social and economic influences, with a limited emphasis on a broader holistic approach on the implications on overall tourism management and development. Observations to date suggest greater prominence and participation by Asia’s NTOs (National Tourism Offices) and DMOs (Destination Management Companies) are needed on the future of the casino’s role within the tourism system and destination master plan and vision

Increasing Chinese Tourist Gamblers in Macao: Crucial Player Characteristics to Identify and Exploit

Casinos are today considered major tourist attractions and are a strategic component in the development of a tourism destination. Tourist gamblers are an important market segment providing a reliable source of revenue for casinos. It is necessary to understand the characteristics of these gamblers and to design services and products that cater for their needs. In this study a survey of 402 Chinese tourist gamblers indicated that they have distinctive characteristics, gambling motivations, behaviors and preferences that must be considered and catered to for depth of understanding and devising ways to attract, keep and increase these important customers. Management and marketing implications for local casino operators and destination marketers are drawn

FDI, R&D and Innovation Output in the Chinese Automobile Industry

After joining the World Trade Organization (WTO), China witnessed a major inflow of Foreign Direct Investment (FDI). Many famous automobile firms of developed countries were attracted to invest in China to cooperate with domestic firms. This paper uses firm-level data of the Chinese automobile industry to analyze the determinants of, and the interrelationships between, innovation input and innovation output, and in particular whether FDI had any influence on these two aspects of innovation. A generalized tobit model will be estimated for both R&D and the share of innovative sales for 2002/2003 and 2005/2006. The findings show that FDI firms are less R&D intensive but, when they innovate in new products, they are more product innovative than domestic-funded firms.FDI, China, R&D, innovation, automobile industry

Destination image in travel magazines: A textual and pictorial analysis of Hong Kong and Macau

Based on the analyses of texts and pictures in the top six outbound travel magazines in Mainland China, this article presents an evaluation of the destination images of Hong Kong and Macau as portrayed in 88 travel articles over a three-year period. The results showed that the projected destination images of Hong Kong and Macau were dominated by attributes related to culture, history, and art and leisure and recreation. Hong Kong was often described by image attributes such as places and attractions, shopping, cuisine and food, hotels, and the creative industries. For Macau, history and heritage, places and attractions, gambling, cuisine and food, and hotels were the most often reported. During the study period, Hong Kong and Macau witnessed several significant changes in the image attributes featured in both texts and pictures. These changes were partly influenced by news and events over the period. In this article, implications for destination marketing organizations and directions for future research were suggested

State intervention, local indebtedness, investment overheating and their systemic background during global crisis in China

This paper focuses on the immediate economic and systemic reasons of steadily increasing local government indebtedness and investment overheating in China. These two phenomena emerged between 2008 and 2011 as a direct consequence of an external shock caused by the global crisis and the subsequent internal reaction in the form of intensified stimulating state intervention. New chances for resource distribution and investments through state intervention mobilized distribution priorities and politically rational economic behavior of actors, characteristic to party-state systems. Locations of mobilization were defined by the decentralized Chinese system specifics along the intertwined institutional party-state structure. Systemic characteristics and its Chinese specifics together resulted in investment overheating, and steadily growing local indebtedness through large and state-owned enterprises and local governments. This process was further amplified by the characteristics of transforming economy in China as actors in the private sphere were mobilized by the increased input demand of those privileged by the systemic priorities of state intervention

Petrology and geochemistry of the igneous rocks from Macao (South China) : Tectono-magmatic implications

The territory of Macao is composed of several granitic intrusions belonging to one of the biggest granite provinces in the world, the Southeast China Magmatic Belt (SCMB), located in the southeast (SE) area of the Cathaysia Block. The SCMB is known by the occurrence of large volumes of Mesozoic magmatic rocks (over 90% are granitic rocks and equivalent volcanic rocks with minor basalts), occupying a total outcrop area of nearly 200.000 km2. The geology of Macao (~30 Km2) is dominated by granitic rocks displaying a wide range of textural, mineralogical and chemical features, making it an ideal region to study these rocks and the petrogenetic processes responsible for their diversity. This study employed a wide range of research methodologies, namely field studies, petrography, zircon geochronology, mineral chemistry, whole-rock elemental and isotopic geochemistry to determine the nature of the source, the petrogenetic processes and the tectonic regimes of the Mesozoic magmatism in this region. Thus, the data collected along this study aims to provide new knowledge on the tectono-magmatic evolution of Macao, in particular, and of SE China, in general. The results obtained from the high-precision U–Pb zircon geochronology, acquired through isotope dilution thermal ionization mass spectrometry (ID-TIMS) and in-situ laser ablation multi-collector inductively coupled mass spectrometry (LA-MC-ICPMS), revealed different ages for Macao granites. Despite its relatively small area, the determined ages tightly constrain the Macao granitic magmatism to two periods, ranging from 164.5 ± 0.6 to 162.9 ± 0.7 Ma (MGI – Macao Group I granites) and 156.6 ± 0.2 to 155.5 ± 0.8 Ma (MGII – Macao Group II granites). In addition, younger dacitic rocks were dated at 150.6 ± 0.6 Ma and <120 Ma. The existence of two proximal but distinct granitic pulses, spanning for a time of about 9 Ma and separated by ca. 6 Ma, in the Macao granitic suite suggests that it was incrementally assembled. This hypothesis is also extendable to the neighbouring Hong Kong region, where the magmatic activity occurred in four major pulses spanning for about 24 Ma. However, the MGII granites indicate the occurrence, on the Pearl River Delta region, of a magmatic pulse between those defined in Hong Kong at the origin of Lamma Suite (165–160 Ma) and the Kwai Chung Suite (148–146 Ma). In addition, Rare Element Earth (REE) ratios suggest that this pulse may only occur in Macao area, while MGI granites show evolving trends of REE ratios similar to those of Jurassic granites outcropping in vast areas of the Cathaysia Block (SE China). Inheritance patterns in the zircon U–Pb data indicate the presence of a population of antecrysts (165–180 Ma) crystallized from earlier magmatic pulses and a population of inherited zircons, from Precambrian to Phanerozoic sources, incorporated into the magmas during melting and/or ascent/emplacement at crustal levels. The oldest inherited ages (2.4 Ga and possibly 2.9 Ga) suggest contribution of Proterozoic and possibly of late Archaean crustal sources for the Macao magmatism. The granitic rocks of Macao are mainly high-K calc-alkaline metaluminous to weakly peraluminous I-type granites with variable degrees of fractionation. Fractional crystallization played an important role in the evolution of these granites, though the fractionation paths differ for the highly fractionated facies of both groups mainly due to distinct accessory fractionating phases. Such difference is evident by distinct REE evolution trends: while MGI magmas seem to have evolved by gradual enrichment in heavy REE relatively to light REE, originating progressively flatter REE patterns, magmas from MGII are marked by depletion of middle REE, leading to progressively concave upward REE patterns. However, while most of the geochemical variation of the MGII granites can be explained by fractional crystallization, the same is not true for MGI granites. The MGI highly fractionated granites show evidence for the REE tetrad effect and are characterized by non-CHArge-and-RAdius-Controlled (non-CHARAC) behaviour of trace elements, suggesting late-stage melt/fluid interactions involving F-rich fluids. The stage of evolution represented by the MGI highly fractionated granites corresponds to the onset of fluid/melt interaction in a highly evolved granitic system, which may have led to enhanced hydrothermal activity in more evolved stages, as those represented in neighbouring areas in SE China. Significant differences in isotopic composition were also observed, with the MGII being characterized by a much narrow range of initial 87Sr/86Sr ratios and εNd(t) and εHf(t) values than MGI. Based on these differences, the MGII granites are considered to be part of a comagmatic suite that has evolved in closed system, contrasting with what can be inferred for MGI. The increase in initial 87Sr/86Sr ratios with degree of evolution, the presence of metasedimentary enclaves and the high percentage of inherited zircon with Paleozoic ages in MGI, suggest the occurrence of an assimilation fractionation crystallization (AFC) process. The AFC processes were a major cause for the I-S transitional characteristics of the MGI highly fractionated granites and possibly of the other similar Jurassic biotite granites in SE China. The observed decoupling of Sr, Nd and Hf isotope systems might have resulted from magma mixing between the granitic and more mafic magmas, which caused the homogenization of Sr isotope ratios but not of the Nd and Hf ones. Such process is also supported by the occurrence of Microgranular Mafic Enclaves (MME) hosted by the granites. Isotope and major element compositions together with model ages strongly suggest that Macao granitic magmas were generated by partial melting of infracrustal medium-to-high K basaltic Paleo-Proterozoic to Mesoproterozoic protoliths heated by, and mixed to some degree with mantle-derived magmas. The temporal and spatial association of Macao and SE China Jurassic I-type granites with basaltic/gabbroic rocks, syenites and A-type granites, displaying typical intraplate chemical features, indicates an extensional regime rather than an active margin for the origin of these rocks. It also points to an important role of mantle-derived magmas in the production of SE China Jurassic granites. Adiabatic decompression melting of the asthenospheric mantle produced mafic magmas, which underplated at the base of the crust (Moho), subsequently triggering partial melting of the lower crust to generate the granitic magmas. The Jurassic Macao granites are interpreted as being produced in an intraplate extensional setting related to the break-off and foundering of a previously flat-slab (Paleo-Pacific plate) beneath the Eurasian plate. The boundary between east and west Cathaysia blocks is roughly along the Zhenghe-Dapu Fault (ZDF), which intersects the SE China coast near Hong Kong and is thought to have played a major role for the Mesozoic magmatic activity in this region. The stronger isotopic affinities of Macao granites with the other granitic rocks and lower crustal xenoliths from the western Cathaysia Block suggest that the ZDF is likely to pass south of Macao, a fact that has not been mentioned before. In addition to the Early Yanshanian (Jurassic) granitic magmatism in Macao, the younger ages obtained for the dacite dykes indicate that the territory was also affected, to a lesser degree, by Late Yanshanian (Cretaceous) magmatism. The transition from granitic to dacitic magmatism most likely corresponds to a change in the regional tectonic regime, which induced a significant change in the magma genesis processes. In contrast with the intraplate features of Macao and SE China Jurassic granites and coeval mafic rocks, the geochemical features of the Macao dacite dykes (e.g. high LILE/HFSE ratios and negative anomalies of Nb, Ta and Ti) are identical to those characterizing arc-like subduction-related magmas. These dacites are most likely evolved products of arc-like magmatism and may testify the reestablishment of a normal subduction system in this area of SE China

Community Participation in Heritage Management: A Case in Macao

This thesis examines what community participation means in heritage management, particularly the notion of a meaningful participatory process in preservation. The discourse of historic preservation today is shifting focus from physical intervention of a site to a more integrated approach which embraces also the social contexts of a cultural heritage. There is growing recognition that cultural heritage can benefit social well-being, especially in the formation of personal or collective identities. Community participation then becomes an indispensable component of contemporary preservation practice. Management of participatory processes is key to successful community participation, and it requires the use of mechanisms to interpret and solicit these processes. This thesis proposes two frameworks to enhance participatory processes in heritage management. The first one is an interpretative framework that allows preservationists to evaluate the different levels of participatory activities and what each level means. The second model is a joint fact-finding framework that seeks to enhance collaborative endeavors between local communities and decision-makers in consultative programs. The thesis also uses the city of Macao as a case study to understand the dynamics and nuances of community participation in heritage management. The case study analyzes contexts of community participation in Macao and explains why direct dialogue between local citizens and the government is not necessarily effective. It also examines three incidents that involve contentious preservation practices in Macao and evaluates the level of participation in each case. In the last part, the thesis proposes a joint fact-finding framework that is specific to the context of heritage management in Macao

The Marketing Plan of the Cotai Strip

In 2003, when most the current Cotai Strip was still a piece of reclaimed land, Sheldon Adelson started a visionary development on this piece of land: the Asian Las Vegas - the Cotai Strip under the corporate Sands China Limited. Its first property, the Venetian Macau was opened in August 2007 followed with a Four Seasons hotel in 2008 with a great success. The forthcoming project is the Sands Cotai Central which includes a 1,200-rooms Holiday Inn Macau, a 600-rooms Conrad Macau and a 4,000-rooms Sheraton Macao with an additional complex of casino, meeting facilities, and shopping mall. Marketing these different hotels and the Venetian Macao separately is not only costly but is also possibly conflicting to each other. Together with the existing resources Sands China owns (the Cotai Jet – ferry service between HK & Macau, the largest fleet of tour bus and the existing strong brand image of the Venetian Macau), it will be much cost effective and efficient to market a new tourist destination – the entire Cotai Strip, that consists of different hotels and other element of entertainment where customers have a great variety of choice to stay and experience