The European level in EU governance: territory, authority and trans-scalar networks     

Virginie Mamadouh  Herman van der Wusten 《GeoJournal》2008,72(1-2):19-31

This article offers an analysis of the emerging scalar configuration of the governance of the European Union. It discusses how European integration stands for a move from a collection of territorially homogenous systems of rule towards a new assemblage of territories, authorities and rights. The paper first questions the stretchy territoriality of the seemingly obvious European level. Second it analyses the sectoral differences in the evolution of the width and the depth of integration, measured as the transfer of competencies to the EU level between the Rome Treaty (1958) and the Lisbon Treaty (200y). Third it turns to the day-to-day decision-making to assess the relations between players in EU governance and finally it looks more closely at the administrative wheels of the EU machinery.  相似文献   

Model for the development of kyanite during partial convective overturn of Archean granite–greenstone terranes: the Pilbara Craton, Australia     

COLLINS  & VAN KRANENDONK 《Journal of Metamorphic Geology》1999,17(2):145-156

Restricted occurrences of early, syn- and late-kinematic kyanite adjacent to large domal batholiths in the Archean granite–greenstone terrane of the east Pilbara craton, Australia, are considered to result from partial convective overturn of the crust. The analogue models of Dixon & Summers (1983) and thermo-mechanical models of Mareschal & West (1980), involving gravitionational overturn of dense greenstone crust that initially overlay sialic basement, successfully explain the geometry, dimension, kinematics and strain patterns of the batholiths and greenstone rims. Application of these models suggests that andalusite and sillimanite are the stable aluminosilicate polymorphs in domal crests and rims, where prograde clockwise P–T–t paths, with small pressure changes, should be recorded. Both aluminosilicates are predicted to overprint kyanite, which is observed locally around the east Pilbara domes. Kyanite is the predicted aluminosilicate polymorph in the deeper parts of domal rims and within sinking greenstone keels, reflecting rapid, near-isothermal burial. The narrow zones of kyanite-bearing schists adjacent to some batholiths in the Pilbara craton are metamorphosed, highly strained equivalents of altered felsic volcanic rocks in the low-grade greenstone succession, dragged to mid-crustal depths (6 kbar) during greenstone sinking. The schists rebounded as an arcuate tectonic wedge along the southern Mount Edgar batholith rim, during the later stages of doming, and were juxtaposed against regional, greenschist facies, low-strain greenstones. Thus, kyanite was preserved: if the walls had remained at depth, it would have been overprinted by the higher-temperature aluminosilicate polymorphs during thermal recovery. Kyanite growth in the Pilbara craton is unlikely to have resulted from ballooning of plutons, mantled gneiss doming, metamorphic core complex formation, or early crustal overthickening. The typical subvertical foliations and lineations of the tectonic wedge suggest that subvertical fabrics extended to mid-crustal depths (c. 20 km) before rebound, providing a three-dimensional glimpse of Archean dome-and-keel structures. The general occurrence of large granitoid domes in Archean granite–greenstone terranes, restriction of rare kyanite to the adjacent, high-strain batholith margins, and its absence from the batholiths, suggest that partial convective overturn of the crust may have been a common process at this early stage of Earth history.  相似文献   

Radiocarbon analyses along the EDML ice core in Antarctica     

R. S. W. VAN DE WAL  H. A. J. MEIJER  M. DE ROOIJ  C. VAN DER VEEN 《Tellus. Series B, Chemical and physical meteorology》2007,59(1):157-165

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Coupled numerical–analytical approach to landscape evolution modeling          下载免费PDF全文

Sean D. Willett  Frédéric Herman  Jean Braun 《地球表面变化过程与地形》2014,39(4):522-545

The Earth's topography is shaped by surface processes that operate on various scales. In particular, river processes control landscape dynamics over large length scales, whereas hillslope processes control the dynamics over smaller length scales. This scale separation challenges numerical treatments of landscape evolution that use space discretization. Large grid spacing cannot account for the dynamics of water divides that control drainage area competition, and erosion rate and slope distribution. Small grid spacing that properly accounts for divide dynamics is computationally inefficient when studying large domains. Here we propose a new approach for landscape evolution modeling that couples irregular grid‐based numerical solutions for the large‐scale fluvial dynamics and continuum‐based analytical solutions for the small‐scale fluvial and hillslope dynamics. The new approach is implemented in the landscape evolution model DAC (divide and capture). The geometrical and topological characteristics of DAC's landscapes show compatibility with those of natural landscapes. A comparative study shows that, even with large grid spacing, DAC predictions fit well an analytical solution for divide migration in the presence of horizontal advection of topography. In addition, DAC is used to study some outstanding problems in landscape evolution. (i) The time to steady‐state is investigated and simulations show that steady‐state requires much more time to achieve than predicted by fixed area calculations, due to divides migration and persistent reorganization of low‐order streams. (ii) Large‐scale stream captures in a strike‐slip environment are studied and show a distinct pattern of erosion rates that can be used to identify recent capture events. (iii) Three tectono‐climatic mechanisms that can lead to asymmetric mountains are studied. Each of the mechanisms produces a distinct morphology and erosion rate distribution. Application to the Southern Alps of New Zealand suggests that tectonic advection, precipitation gradients and non‐uniform tectonic uplift act together to shape the first‐order topography of this mountain range. Copyright © 2014 John Wiley & Sons, Ltd.  相似文献   

A critical view of the environmental condition of the Sognefjord     

Manzetti S  Stenersen JH 《Marine pollution bulletin》2010,60(12):2167-2174

The world oceans and seas are experiencing a dramatic decline in their health and viability. In the midst of this crisis, the Norwegian fjords represent under-studied and highly vulnerable ecosystems. Fjord chemistry and fjord ecosystems are poorly studied given the current focus on polar ice melting, fish stock reductions and oil disasters. For this reason, this review sheds light on and aims to accumulate local and national findings concerning the current viability of the Sognefjord, the world's second longest fjord and Norway's longest and deepest fjord, stretching 205 km (127 miles) and reaching 1308 m below sea level as its deepest point. This review shows that there is a critical need to establish knowledge and parameters to better monitor and prevent an ecosystem catastrophe from developing in Norwegian fjords. The poor circulation in fjords compared to opens seas reduces their ability to circulate waste and transport fresh water from hydroelectricity plants. Because of fjord morphology, pollutants and heavy metals are potentially trapped within them at great depths for decades. The monitoring of Norwegian fjords is thus of fundamental importance.  相似文献   

Cooperation at different scales: challenges for local and international water resource governance in South Africa     

N MIRUMACHI  E VAN WYK† 《The Geographical journal》2010,176(1):25-38

Theory on environmental governance and water governance emphasises decentralised, devolved forms of interaction between stakeholders. As previously excluded actors are empowered to take part in governance, new forms of cooperation are created. This paper examines how the cooperative principle has influenced stakeholder interaction at the local and international scales of water governance in South Africa. Water policies and initiatives have been set up to promote multi-level governance that emphasises cooperation between various stakeholders. The emphasis on cooperation and inclusiveness is particularly pertinent to the South African context because of its apartheid past. The paper asks whether there have been new forms of cooperation between a wider array of actors, as the theory proposes. By using the case studies of the Sabie catchment and the Lesotho Highlands Water Project to examine local and international level governance, the paper finds challenges related to power disparity and interdependence of actors, and risk perceptions of inclusive decision-making. It is found that at both the local and international level, the state, which is a 'traditional' actor, still plays an influential role in decision-making. 'New' actors such as businesses, civil society, and regional institutions are more visible but have limited decision-making power. Non-linear, time-consuming forms of cooperation occur in water governance.  相似文献   

Siliceous Cementation of Chlorite-Coated Grains in the Permian Sandstone Gas Reservoirs, Ordos Basin     

FAN Aiping  YANG Renchao  LI Jinbu  ZHAO Zhongjun  A.J. 《《地质学报》英文版》2017,91(3):1147-1148

<正>Objective It has long been controversial that whether authigenic chlorite coatings in sandstone reservoirs can prevent precipitation of siliceous cements.It is commonly believed that chlorite coatings(also called chlorite films,chlorite linings,or chlorite rims)may prevent quartz overgrowth,and thus help the preservation of original pores in sandstone reservoirs.Recently,however,this assumption has been challenged by reservoir geologists.This dispute cannot be solved by mere analysis of thin sections,nor by chemical equations and diagenesis analysis.The main objective of the present contribution is to shed light on this  相似文献   

The Metamorphic Evolution and Tectonic Significance of the Sumdo High and Ultrahigh Pressure Metamorphic Terrane, Central-South Lhasa Block, Tibet     

ZHAGN Cong  Thomas BADER  Herman van ROERMUND  YANG Jingsui  SHEN Tingting  QIU Tian  LI Peng 《《地质学报》英文版》2017,91(Z1):52-52

Asthemaintectoniccomponentofthe Himalayan–Tibetan orogen,the Lhasa terrane has received much attention as it records the entire history of the orogeny.The occurrence of high pressure eclogite in the Sumdo complex in central Lhasa terrane has a significant importance on the understanding of the Paleo-Tethys subduction and plate itineration processes in this area.The petrological,geochemical and geochronological data of eclogite and associated blueschist and garnet-bearing mica schist from Sumdo,Jilang and Bailang area have been briefly reviewed to explore the origin and metamorphic evolution of this suture.Eclogites from the Sumdo complex have experienced low temperature,high pressure to ultrahigh pressure metamorphism,revealing a fastsubduction and exhumation process in a typical oceanic subduction zone.The large P-T range between different eclogites in the literature may be affected by the big error of unappropriated using geothermobarometry and may also because of slices of subducted blocks derived from different depths juxtapose together during exhumation.By summarizing the U-Pb,Lu-Hf and Sm-Nd ages of eclogites,the eclogite facies metamorphism is likely to occur in early Triassic during 245-225 Ma,but not the previously accepted late Permian at ca.260 Ma by the reinterpretation of the former geochronological data from literature.The opening of Paleo-Tethys Ocean between the Lhasa terrane initiate prior to ca.280 Ma and ultimate closure to integrate the Lhasa terrane was no earlier than225 Ma and may triggered by the initial subduction of Bangong-Nujiang Tethys Ocean in the north.  相似文献   

About Herman Bouwer     

Bouwer H 《Ground water》2003,41(5):709-713

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Combined measurements of UV-A actinic flux, UV-A irradiance and global radiation in relation to photodissociation rates     

MICHIEL VAN WEELE  JORDI VILÀ-GUERAU DE ARELLANO  FOEKE KUIK 《Tellus. Series B, Chemical and physical meteorology》1995,47(3):353-364

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