The free Aceh movement : Islam and democratisation

The Free Aceh Movement (GAM) has been characterised by some observers and the Indonesian government as being a radical Islamic organisation intent on establishing an Islamic state in northern Sumatra. This article explores GAM's relationship with Islam and shows that while GAM members are devout Muslims and that Islam pervades their political thinking, the organisation and its members are explicitly opposed to the creation of an Islamic state or the imposition of Islamic law. The article reports how senior members of GAM's hierarchy discuss their personal relationship with Islam, noting consistencies and differences in their approaches. A common theme is that Islam provides a motive for the struggle, based on notions of justice and equality, and that these and related aspects of Acehnese political organisation provide the groundwork for a functional form of democracy in Aceh's post-peace settlement environment.

Autonomy and disintegration in Indonesia

Fragmentation in Indonesia is by far the most critical issue now facing the state. This book analyses social unrest, autonomy and separatism in the wake of the Indonesian economic crisis, placing them in the context of state evolution, and looking at the competing aims of economic and political globalisation with local agendas.

The politics of Indonesia

The Politics of Indonesia is the only book to provide a complete analysis of Indonesian politics, from the declaration of independence until the election of Susilo Bambang Yudhoyono in late 2004. The book examines the underlying themes and tensions that affect Indonesian politics, from the dichotomy between the small wealthy elite and the poverty in which most of the population live to the system of corruption and patronage within which the political system and armed forces operate. Analyzing the role and impact of the military, separatism, the media, law, and the economy on Indonesia, this book provides a topical and thought-provoking guide to one of the regions most populous countries, and the largest predominantly Muslim country in the world.

Letting go without a fight : decolonization, democracy and war, 1900-94

Does the type of regime really make no difference to the likelihood of violent conflict over basic issues of stateness such as separatism and decolonization? Can democratic peace theory be successfully applied when dealing with the national identity or stateness question? This article extends the application of the democratic peace to the process of decolonization. It examines conflict between imperial states and their colonies during the process of decolonization and investigates the question of whether democracy affects the likelihood of conflict. The central finding is that, contrary to the implications of some prominent theories of state formation and democracy, democratic imperial states are significantly less likely to go to war with their colonial possessions in the process of achieving independence. Further, the authors find only a monadic, not dyadic, democratic peace effect. The regime type of the colony does not have a significant effect on the likelihood of war. It is the nature of the regime of imperial states, rather than that of colonies, that is a significant factor. In addition, the predominant source of this effect appears to be the institutional constraints placed on executive action within democracies, rather than the influence of mass politics or the effects of political competition. Regarding power-related factors, power parity between sovereign and colony makes conflict more likely (a colonial power-transition effect), but imperial decline actually makes war with colonies less likely. Sensitivity analysis reveals that a number of other hypothesized effects cannot find robust support. Simulations are used to assess the magnitude of the effect of regime type pre- and post-independence. Overall, the article contributes to theory development by investigating different institutional aspects of democracy and by distinguishing monadic and dyadic effects.

Rebellion and reform in Indonesia : Jakarta's security and autonomy polices in Aceh

Armed separatist movements in Papua, East Timor and Aceh have been a serious problem for Indonesia's central government. This book examines the policies of successive Indonesian governments to contain secessionist forces, focusing in particular on Jakarta's response towards the armed separatist movement in Aceh. Unlike other studies of separatism in Indonesia, this book concentrates on the responses of the central government rather than looking only at the separatist forces. It shows how successive governments have tried a wide range of approaches, including military repression, offers of autonomy, peace talks and a combination of these. It discusses the lessons that have been learned from these different approaches and analyzes the impact of the tsunami, including the successful accommodation of former rebels within an Indonesian devolved state structure and the expanding implementation of Islamic law.

The role of hegemony in secessionist movements : the case study of the Moldovan Republic of Transnistria

The aim of the article is to analyse the secessionist phenomenon by applying the concept of hegemony. Based on critical realist interpretations of the concept, it is argued that hegemonic practice incorporates both inter-subjective and structural aspects. The inter-subjective aspect of hegemony places emphasis on the relations between social groups and the way hegemonic practice leads social agents towards political projects that secure consensus in favour of the interest of particular elites. The structural character of hegemonic practice is evident in the reproduction of social conditions and values that underlie the relations between social agents both globally and domestically. Accordingly, the inter-subjective character of secession as hegemonic practice is evident in the organization of social agents towards a political option (territorial separatism) to the extent that it serves the goals of certain elites. The sturctural aspect of secessionist practice is hegeminic because it reproduces international structures that tend to associate political organization with ethnicity at the state level. The analysis then turns to the case study of Transnistria in Moldova as an empirical illustration of the two tendencies of hegemonic practice in secessionist politics leading ot useful conclusions both for the case study in particular and the study of secession in general. 

Succeeding and seceding in Iraq: the case for a Shiite State

The US project to democratize Iraq has given way to a dramatic upsurge in ethno-religious factionalism in which a series of groups have sought to use ‘democracy’ to create or exacerbate division. Among these divisive political elements a relatively fringe idea held mostly by power-hungry elites has become a central driving force of much political debate within Iraq: separatism. Although there are many examples of political factions within Iraq which have called for territorial separatism since 2003 (such as some Kurdish, Sunni, Assyrian and Turcoman political parties), this chapter focuses on the less known case for a Shiite state. Specifically, it concentrates on the Shia Arab Islamist political party, the Supreme Council for the Islamic Revolution in Iraq (SCIRI), which differs from other Shia political factions in their calls for a decentralized federal Iraq with an autonomous Shia Islamic state in the south.

Negotiating sustainable peace in separatist context

This volume examines the various aspects of territorial separatism, focusing on how and why separatist movements arise.

Conclusion

This volume examines the various aspects of territorial separatism, focusing on how and why separatist movements arise.

Secessionist aspects to the Buddhist-Muslim sectarian conflict in Rakhine State, Myanmar

This volume examines the various aspects of territorial separatism, focusing on how and why separatist movements arise.

Self-determination and collective responsibility in the secessionist struggle

The often violent emergence of new independent states following the end of the Cold War generated discussion about the normative grounds of territorial separatism. A number of opposing approaches surfaced debating whether and under which circumstances there is a right for a community to secede from its host country. Overwhelmingly, these studies placed emphasis on the right to secession and neglected the moral stance of secessionist movements as agents in international relations. In this book Costas Laoutides explores the collective moral agency involved in secessionist struggles offering a theoretical model for the collective responsibility of secessionist groups. Case-studies on the Kurds and the people of Moldova-Transdniestria illustrate the author’s theoretical arguments as he seeks to establish how, although the principle of self-determination was envisaged as a means of gradually bestowing political power upon the people, it never managed to realize its full potential because it was interpreted strictly within a framework of exclusionary politics of identity.

Fragmentação geopolítica: uma análise estrutural das propostas de separatismo no Brasil

Este trabalho tem por objetivo dar luz ao debate sobre a criação dos novos entes federativos, trazendo elementos objetivos sobre a caracterização socioeconômica dos novos espaços geopolíticos e seus respectivos papéis no novo contexto espacial do sistema inter-regional brasileiro. O artigo traz resultados inéditos para a discussão, buscando, inicialmente, identificar padrões hierárquicos e de dependência espacial e produtiva neste novo contexto federativo. Tais resultados subsidiama analise subsequente dos impactos da nova configuração das transferências constitucionais, que identifica pormeio de simulações comummodelo inter-regional de insumo-produto especialmente calibrado para as 33 regiões consideradas no estudo, não apenas os potenciais ganhadores e perdedores, mas também os mecanismos de interação espacial subjacentes a estes processos.

Geochronology, geochemistry and isotopic compositions of the volcanic rocks from oceanic (Hawaii) and continental (Eifel) intra-plate environments

The Eifel volcanism is part of the Central European Volcanic Province (CEVP) and is located in the Rhenish Massif, close to the Rhine and Leine Grabens. The Quaternary Eifel volcanism appears to be related to a mantle plume activity. However, the causes of the Tertiary Hocheifel volcanism remain debated. We present geochronological, geochemical and isotope data to assess the geotectonic settings of the Tertiary Eifel volcanism. Based on 40Ar/39Ar dating, we were able to identify two periods in the Hocheifel activity: from 43.6 to 39.0 Ma and from 37.5 to 35.0 Ma. We also show that the pre-rifting volcanism in the northernmost Upper Rhine Graben (59 to 47 Ma) closely precede the Hocheifel volcanic activity. In addition, the volcanism propagates from south to north within the older phase of the Hocheifel activity. At the time of Hocheifel volcanism, the tectonic activity in the Hocheifel was controlled by stress field conditions identical to those of the Upper Rhine Graben. Therefore, magma generation in the Hocheifel appears to be caused by decompression due to Middle to Late Eocene extension. Our geochemical data indicate that the Hocheifel magmas were produced by partial melting of a garnet peridotite at 75-90 km depth. We also show that crustal contamination is minor although the magmas erupted through a relatively thick continental lithosphere. Sr, Nd and Pb isotopic compositions suggest that the source of the Hocheifel magmas is a mixing between depleted FOZO or HIMU-like material and enriched EM2-like material. The Tertiary Hocheifel and the Quaternary Eifel lavas appear to have a common enriched end-member. However, the other sources are likely to be distinct. In addition, the Hocheifel lavas share a depleted component with the other Tertiary CEVP lavas. Although the Tertiary Hocheifel and the Quaternary Eifel lavas appear to originate from different sources, the potential involvement of a FOZO-like component would indicate the contribution of deep mantle material. Thus, on the basis of the geochemical and isotope data, we cannot rule out the involvement of plume-type material in the Hocheifel magmas. The Ko’olau Scientific Drilling Project (KSDP) has been initiated in order to evaluate the long-term evolution of Ko’olau volcano and obtain information about the Hawaiian mantle plume. High precision Pb triple spike data, as well as Sr and Nd isotope data on KSDP lavas and Honolulu Volcanics (HVS) reveal compositional source variations during Ko’olau growth. Pb isotopic compositions indicate that, at least, three Pb end-members are present in Ko’olau lavas. Changes in the contributions of each component are recorded in the Pb, Sr and Nd isotopes stratigraphy. The radiogenic component is present, at variable proportion, in all three stages of Ko’olau growth. It shows affinities with the least radiogenic “Kea-lo8” lavas present in Mauna Kea. The first unradiogenic component was present in the main-shield stage of Ko’olau growth but its contribution decreased with time. It has EM1 type characteristics and corresponds to the “Ko’olau” component of Hawaiian mantle plume. The second unradiogenic end-member, so far only sampled by Honololu lavas, has isotopic characteristics similar to those of a depleted mantle. However, they are different from those of the recent Pacific lithosphere (EPR MORB) indicating that the HVS are not derived from MORB-related source. We suggest, instead, that the HVS result from melting of a plume material. Thus the evolution of a single Hawaiian volcano records the geochemical and isotopic changes within the Hawaiian plume.

Entwicklung einer Anordnung zur Nutzung von Massenschwerebewegungen beim Quarzitabbau im Rheinischen Schiefergebirge

Die (Wieder-)Nutzung auf Schwerkraft basierender Fördertechniken, die insbesondere durch das niedrige Energiepreisniveau in den Jahrzehnten nach dem 2. Weltkrieg in der Tagebautechnik nahezu vollständig verdrängt wurden, ist bei den heutigen wirtschaftlichen Randbedingungen und anzustrebenden ökologischen Standards eine Herausforderung für die bergbautreibende Industrie. Seit Aufnahme der Entwicklung des Förderkonzeptes – Geführte Versturztechnik – Mitte der 1990er Jahre haben sich die Kosten für Rohöl vor Steuern nach dem Tiefstand um das Jahr 1998 bis heute mehr als verdreifacht, alleine seit 2004 mehr als verdoppelt. Gesetzliche Regelwerke wie die europäische IVU-Richtlinie 96/61/EG zur „integrierten Vermeidung und Verminderung der Umweltverschmutzung“ fordern, Genehmigungen nur noch bei Einsatz der besten verfügbaren Techniken (BVT oder BAT: „best available techniques“) zu erteilen. Die Umsetzung in nationale Vorschriften wie das Bundes-Immissionsschutzgesetz und nachgeordnete Regelwerke fordern hierauf aufbauend, dass Umweltbelastungen nicht in andere Medien verlagert werden dürfen. Die Anordnung einer Versturzrinne zur Nutzung von Massenschwerebewegungen am Beispiel von Quarzitabbau im Rheinischen Schiefergebirge bei denen die Förderbezugsebene unterhalb der Strossen liegt, die zur sichern und selektiven Gewinnung des Rohstoffs aufgefahren werden müssen, erfüllt durch Rückgriff auf ein vermeintlich „archaisches“ Förderkonzept durch Nutzung der Schwerkraft die obigen Anforderungen. Offenkundige Umweltbelastungen, die alleine durch die Verbrennung von Dieselkraftstoff und hieraus resultierender Schadstoff- und Wärmeeinträge in die Luft beim verbreiteten Einsatz von SLKW zur Abwärtsförderung entstehen, können erheblich vermindert werden. Der Aspekt der Betriebssicherheit einer solchen Anordnung kann durch Auffahren eines geradlinigen Bauwerks mit an das Fördergut angepassten Dimensionen sowie Einrichtungen zur Beschränkung der kinetischen Energie erreicht werden. Diese stellen auch gleichzeitig sicher, dass die Zerkleinerung des durch die Versturzrinne abwärts transportierten Materials betrieblich zulässige Grenzen nicht überschreitet. Hierfür kann auf das umfangreiche Wissen zu Massenschwerebewegungen Rückgriff genommen werden. Dem Aspekt des Umweltschutzes, der sich in Bezug auf das Medium Luft auf den autochtonen Staub reduziert, kann durch Vorrichtungen zur Staubniederschlagung Rechnung getragen werden. Vertiefende Untersuchungen sind erforderlich, um die mit komplexen, aber erprobten Techniken arbeitende Tagebauindustrie auch in dicht besiedelten Regionen wieder an die Nutzung von Schwerkraft (-gestützten) Fördertechniken heranzuführen. Auch das Konzept – Geführte Versturztechnik – ist auf konkrete Anwendungsfälle hin in Details anzupassen.

Räumliche Verbreitung geogener Schwermetallgehalte in Böden des Taunus: Einfluss von periglazialer Deckschichtengenese

Während der Glazialphasen kam es in den europäischen Mittelgebirgen bedingt durch extensive solifluidale Massenbewegungen zur Bildung von Deckschichten. Diese Deckschichten repräsentieren eine Mischung verschiedener Substrate, wie anstehendes Ausgangsgestein, äolische Depositionen und lokale Erzgänge. Die räumliche Ausdehnung der Metallkontaminationen verursacht durch kleinräumige Erzgänge wird durch die periglaziale Solifluktion verstärkt. Das Ziel der vorliegenden Untersuchung war a) den Zusammenhang zwischen den Reliefeigenschaften und den Ausprägungen der solifluidalen Deckschichten und Böden aufzuklären, sowie b) mittels Spurenelementgehalte und Blei-Isotopen-Verhältnisse als Eingangsdaten für Mischungsmodelle die Beitrage der einzelnen Substrate zum Ausgangsmaterial der Bodenbildung zu identifizieren und quantifizieren und c) die räumliche Verteilung von Blei (Pb) in Deckschichten, die über Bleierzgänge gewandert sind, untersucht, die Transportweite des erzbürtigen Bleis berechnet und die kontrollierenden Faktoren der Transportweite bestimmt werden. Sechs Transekte im südöstlichen Rheinischen Schiefergebirge, einschließlich der durch periglaziale Solifluktion entwickelten Böden, wurden untersucht. Die bodenkundliche Geländeaufnahme erfolgte nach AG Boden (2005). O, A, B und C-Horizontproben wurden auf ihre Spurenelementgehalte und teilweise auf ihre 206Pb/207Pb-Isotopenverhältnisse analysiert. Die steuernden Faktoren der Verteilung und Eigenschaften periglazialer Deckschichten sind neben der Petrographie, Reliefeigenschaften wie Exposition, Hangneigung, Hangposition und Krümmung. Die Reliefanalyse zeigt geringmächtige Deckschichten in divergenten, konvexen Hangbereichen bei gleichzeitig hohem Skelettgehalt. In konvergent, konkaven Hangbereichen nimmt die Deckschichtenmächtigkeit deutlich zu, bei gleichzeitig zunehmendem Lösslehm- und abnehmendem Skelettgehalt. Abhängig von den Reliefeigenschaften und -positionen reichen die ausgeprägten Bodentypen von sauren Braunerden bis hin zu Pseudogley-Parabraunerden. Des Weiteren kommen holozäne Kolluvien in eher untypischen Reliefpositionen wie langgestreckten, kaum geneigten Hangbereichen oder Mittelhangbereichen vor. Außer für Pb bewegen sich die Spurenelementgehalte im Rahmen niedriger Hintergrundgehalte. Die Pb-Gehalte liegen zwischen 20-135 mg kg-1. Abnehmende Spurenelementgehalte und Isotopensignaturen (206Pb/207Pb-Isotopenverhältnisse) von Pb zeigen, dass nahezu kein Pb aus atmosphärischen Depositionen in die B-Horizonte verlagert wurde. Eine Hauptkomponentenanalyse (PCA) der Spurenelementgehalte hat vier Hauptsubstratquellen der untersuchten B-Horizonte identifiziert (Tonschiefer, Löss, Laacher-See-Tephra [LST] und lokale Pb-Erzgänge). Mittels 3-Komponenten-Mischungsmodell, das Tonschiefer, Löss und LST einschloss, konnten, bis auf 10 Ausreißer, die Spurenelementgehalte aller 120 B-Horizontproben erklärt werden. Der Massenbeitrag des Pb-Erzes zur Substratmischung liegt bei <0,1%. Die räumliche Pb-Verteilung zeigt Bereiche lokaler Pb-Gehaltsmaxima hangaufwärtiger Pb-Erzgänge. Mittels eines 206Pb/207Pb-Isotopenverhältnis-Mischungsmodells konnten 14 Bereiche erhöhter lokaler Pb-Gehaltsmaxima ausgewiesen werden, die 76-100% erzbürtigen Bleis enthalten. Mit Hilfe eines Geographischen Informationssystems wurden die Transportweiten des erzbürtigen Bleis mit 30 bis 110 m bestimmt. Die steuerenden Faktoren der Transportweite sind dabei die Schluffkonzentration und die Vertikalkrümmung. Diese Untersuchung zeigt, dass Reliefeigenschaften und Reliefposition einen entscheidenden Einfluss auf die Ausprägung der Deckschichten und Böden im europäischen Mittelgebirgsbereich haben. Mischungsmodelle in Kombination mit Spurenelementanalysen und Isotopenverhältnissen stellen ein wichtiges Werkzeug zur Bestimmung der Beiträge der einzelnen Glieder in Bodensubstratmischungen dar. Außerdem können lokale Bleierzgänge die natürlichen Pb-Gehalte in Böden, entwickelt in periglazialen Deckschichten der letzten Vereisungsphase (Würm), bis über 100 m Entfernung erhöhen.