The “Tibet question”: Tibetan, Chinese and Western perspectives

2013 ◽  
Vol 41 (6) ◽  
pp. 1100-1135 ◽  
Author(s):  
David M. Crowe

The historical conflict between Tibet and China goes back almost a thousand years. Both sides use history to argue their point about the core issues in this dispute – Tibet's claim of independence and autonomy, and China's of suzerainty. This article looks at the historical roots of this conflict, particularly since 1949, when China began its gradual takeover of Tibet. Chinese policies toward Tibet, which have been driven by a desire to communize and sinicize Tibet, has been met by stiff resistance from the Tibetans, who see Han Chinese dominance as a force that will, over time, destroy Tibet's unique religion, language, culture, and history. This resistance has drawn the attention of the West, who see Chinese policies in Tibet as a symbol of the failings of Beijing's rulers to embrace a strong commitment to human rights at the same time that China is becoming a global economic power. The 14th Dalai Lama, a key figure in this conflict, and his government-in-exile have served as bridges to Western efforts to try to force Beijing to embrace more open, humane policies toward Tibetans throughout China. His retirement as political head of the exile government in 2011, coupled with China's growing economic and strategic power globally, raises serious questions about the willingness of the USA, and other democratic powers to risk their relationships with Beijing to continue to promote true human rights and autonomy throughout the Tibetan Plateau.

2021 ◽  
pp. 1-22
Author(s):  
Qiang Zha

Abstract This paper examines several research questions relating to equality and equity in Chinese higher education via an extended literature review, which in turn sheds light on evolving scholarly explorations into this theme. First, in the post-massification era, has the Chinese situation of equality and equity in higher education improved or deteriorated since the late 1990s? Second, what are the core issues with respect to equality and equity in Chinese higher education? Third, how have those core issues evolved or changed over time and what does the evolution indicate and entail? Methodologically, this paper uses a bibliometric analysis to detect the topical hotspots in scholarly literature and their changes over time. The study then investigates each of those topical terrains against their temporal contexts in order to gain insights into the core issues.


2020 ◽  
Vol 3 (1) ◽  
Author(s):  
Jiekun He ◽  
Siliang Lin ◽  
Jiatang Li ◽  
Jiehua Yu ◽  
Haisheng Jiang

AbstractThe Tibetan Plateau (TP) and surrounding regions have one of the most complex biotas on Earth. However, the evolutionary history of these regions in deep time is poorly understood. Here, we quantify the temporal changes in beta dissimilarities among zoogeographical regions during the Cenozoic using 4,966 extant terrestrial vertebrates and 1,278 extinct mammal genera. We identify ten present-day zoogeographical regions and find that they underwent a striking change over time. Specifically, the fauna on the TP was close to the Oriental realm in deep time but became more similar to the Palearctic realms more recently. The present-day zoogeographical regions generally emerged during the Miocene/Pliocene boundary (ca. 5 Ma). These results indicate that geological events such as the Indo-Asian Collision, the TP uplift, and the aridification of the Asian interior underpinned the evolutionary history of the zoogeographical regions surrounding the TP over different time periods.


Author(s):  
James A. Gross

This book makes four important contributions to our understanding of U.S. labor law and policy. First, given my previous three volume study of the work of the NLRB, this book is able to discuss the Board’s path under Chairmen Gould, Truesdale, Battista and Liebman in historical context. Second, this book demonstrates the consequences of applying different and conflicting values to real world issues of labor law. Third, the book’s inward assessment of U.S. labor law and policy using international human rights principles as standards for judgment constitutes new perspectives on old issues. These new perspectives challenge the commonly held view among practitioners and academics that workers’ organizing and collective bargaining are merely tests of economic power by adversarial interest groups exercising commercial rights not human rights. Finally, rather than joining those writing obituaries for the Act and the NLRB, this book maintains, despite the unrelenting pounding of hostile forces, that the core of the Act remains a solid foundation for the realization of workers’ rights–but calls for a new more creative vision because more is needed than merely fine tuning for marginal adjustments.


Author(s):  
Dov Waxman

No conflict in the world has lasted as long, generated as many news headlines, or incited as much controversy as the Israeli-Palestinian conflict. Yet, despite, or perhaps because of, the degree of international attention it receives, the conflict is still widely misunderstood. While Israelis and Palestinians and their respective supporters trade accusations, many outside observers remain confused by the conflict's complexity and perplexed by the passion it arouses. The Israeli-Palestinian Conflict: What Everyone Needs to Know® offers an even-handed and judicious guide to the world's most intractable dispute. Rather than presenting a traditional, narrative history, this book employs an accessible question-and-answer format. Writing in an engaging, jargon-free style, Dov Waxman, a leading expert on the Middle East, provides clear and concise answers to common questions, from the most basic to the most contentious. Covering the conflict from its nineteenth-century origins to the latest developments of the twenty-first century, this book explains the key events, examines the core issues, and presents the competing claims and narratives of both sides. Readers will learn what the Israeli-Palestinian conflict is all about, how it has evolved over time, and why it continues to defy diplomatic efforts at a resolution.


2014 ◽  
Vol 14 (2) ◽  
pp. 913-937 ◽  
Author(s):  
B. Škerlak ◽  
M. Sprenger ◽  
H. Wernli

Abstract. In this study we use the ERA-Interim reanalysis data set from the European Centre for Medium-Range Weather Forecasts (ECMWF) and a refined version of a previously developed Lagrangian methodology to compile a global 33 yr climatology of stratosphere–troposphere exchange (STE) from 1979 to 2011. Fluxes of mass and ozone are calculated across the tropopause, pressure surfaces in the troposphere, and the top of the planetary boundary layer (PBL). This climatology provides a state-of-the-art quantification of the geographical distribution of STE and the preferred transport pathways, as well as insight into the temporal evolution of STE during the last 33 yr. We confirm the distinct zonal and seasonal asymmetry found in previous studies using comparable methods. The subset of "deep STE", where stratospheric air reaches the PBL within 4 days or vice versa, shows especially strong geographical and seasonal variations. The global hotspots for deep STE are found along the west coast of North America and over the Tibetan Plateau, especially in boreal winter and spring. An analysis of the time series reveals significant positive trends of the net downward mass flux and of deep STE in both directions, which are particularly large over North America. The downward ozone flux across the tropopause is dominated by the seasonal cycle of ozone concentrations at the tropopause and peaks in summer, when the mass flux is nearly at its minimum. For the subset of deep STE events, the situation is reversed and the downward ozone flux into the PBL is dominated by the mass flux and peaks in early spring. Thus surface ozone concentration along the west coast of North America and around the Tibetan Plateau are likely to be influenced by deep stratospheric intrusions. We discuss the sensitivity of our results on the choice of the control surface representing the tropopause, the horizontal and vertical resolution of the trajectory starting grid, and the minimum residence time τ used to filter out transient STE trajectories.


2021 ◽  
Vol 9 ◽  
Author(s):  
Chongjin Zhao ◽  
Luolei Zhang ◽  
Peng Yu ◽  
Xi Xu

The Songpan−Aba region is located on the northeastern edge of the Tibetan Plateau. Tectonically, the area is surrounded by the West Qinling orogenic belt in the north, the Longmenshan orogenic belt in the southeast, and the East Kunlun and Sanjiang orogenic belts in the west and southwest, forming a triangle that provides an ideal location to study the crust-mantle structure and deep tectonics of the eastward extrusion of the Tibetan Plateau. In this study, the magnetic and electrical structures of the Songpan−Aba area were investigated by inversion using high-precision magnetic anomaly and magnetotelluric data to obtain the subsurface magnetization inversion intensity and resistivity of Songpan–Aba and adjacent areas. The results revealed a continuous magnetic layer up to 20 km below Songpan–Aba and its surrounding areas in the south, possibly originating from a magma root southwest of the Longmenshan massif. In the West Qinling, Songpan–Aba, and Longmenshan areas, pervasive low-resistance, weakly magnetic, or magnetic layers were identified below 20 km that might be formed from the molten mantle material extruded from the eastern edge of the Tibetan Plateau.


Lithosphere ◽  
2020 ◽  
Vol 2020 (1) ◽  
Author(s):  
Yi-Peng Zhang ◽  
Wen-Jun Zheng ◽  
Wei-Tao Wang ◽  
Yun-Tao Tian ◽  
Renjie Zhou ◽  
...  

Abstract Cenozoic exhumation in the northeastern Tibetan Plateau provides insights into spatial-temporal patterns of crustal shortening, erosion, landscape evolution, and geodynamic drivers in the broad India-Eurasia collision system. The NW-SE trending West Qinling Belt has been a central debate as to when crustal shortening took place. Within the West Qinling Belt, a thick succession of Cretaceous sedimentary rocks has been deformed and exhumed along major basin-bounding thrust faults. We present new apatite (U-Th)/He ages from the hanging wall and footwall of this major thrust. Contrasting thermal histories show that rapid cooling commenced as early as ca. 45 Ma and continued for 15–20 Myr for the hanging wall, whereas the footwall experiences continuous cooling and slow exhumation since the late Mesozoic. We infer that accelerated exhumation was driven by thrusting in response to the northward growth of the Tibetan Plateau during the Eocene (ca. 45–35 Ma) based on regional sedimentological, structural, and thermochronological data.


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