Water Supply and Usage in Central Asia, Tian Shan Basin Polina Lemenkova
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Glaciers in Xinjiang, China: Past Changes and Current Status
water Article Glaciers in Xinjiang, China: Past Changes and Current Status Puyu Wang 1,2,3,*, Zhongqin Li 1,3,4, Hongliang Li 1,2, Zhengyong Zhang 3, Liping Xu 3 and Xiaoying Yue 1 1 State Key Laboratory of Cryosphere Science/Tianshan Glaciological Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China; [email protected] (Z.L.); [email protected] (H.L.); [email protected] (X.Y.) 2 University of Chinese Academy of Sciences, Beijing 100049, China 3 College of Sciences, Shihezi University, Shihezi 832000, China; [email protected] (Z.Z.); [email protected] (L.X.) 4 College of Geography and Environment Sciences, Northwest Normal University, Lanzhou 730070, China * Correspondence: [email protected] Received: 18 June 2020; Accepted: 11 August 2020; Published: 24 August 2020 Abstract: The Xinjiang Uyghur Autonomous Region of China is the largest arid region in Central Asia, and is heavily dependent on glacier melt in high mountains for water supplies. In this paper, glacier and climate changes in Xinjiang during the past decades were comprehensively discussed based on glacier inventory data, individual monitored glacier observations, recent publications, as well as meteorological records. The results show that glaciers have been in continuous mass loss and dimensional shrinkage since the 1960s, although there are spatial differences between mountains and sub-regions, and the significant temperature increase is the dominant controlling factor of glacier change. The mass loss of monitored glaciers in the Tien Shan has accelerated since the late 1990s, but has a slight slowing after 2010. Remote sensing results also show a more negative mass balance in the 2000s and mass loss slowing in the latest decade (2010s) in most regions. -
Uyghur Dispossession, Culture Work and Terror Capitalism in a Chinese Global City Darren T. Byler a Dissertati
Spirit Breaking: Uyghur Dispossession, Culture Work and Terror Capitalism in a Chinese Global City Darren T. Byler A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy University of Washington 2018 Reading Committee: Sasha Su-Ling Welland, Chair Ann Anagnost Stevan Harrell Danny Hoffman Program Authorized to Offer Degree: Anthropology ©Copyright 2018 Darren T. Byler University of Washington Abstract Spirit Breaking: Uyghur Dispossession, Culture Work and Terror Capitalism in a Chinese Global City Darren T. Byler Chair of the Supervisory Committee: Sasha Su-Ling Welland, Department of Gender, Women, and Sexuality Studies This study argues that Uyghurs, a Turkic-Muslim group in contemporary Northwest China, and the city of Ürümchi have become the object of what the study names “terror capitalism.” This argument is supported by evidence of both the way state-directed economic investment and security infrastructures (pass-book systems, webs of technological surveillance, urban cleansing processes and mass internment camps) have shaped self-representation among Uyghur migrants and Han settlers in the city. It analyzes these human engineering and urban planning projects and the way their effects are contested in new media, film, television, photography and literature. It finds that this form of capitalist production utilizes the discourse of terror to justify state investment in a wide array of policing and social engineering systems that employs millions of state security workers. The project also presents a theoretical model for understanding how Uyghurs use cultural production to both build and refuse the development of this new economic formation and accompanying forms of gendered, ethno-racial violence. -
Late Cretaceous–Palaeogene Topography of the Chinese Tian Shan
Earth and Planetary Science Letters 499 (2018) 95–106 Contents lists available at ScienceDirect Earth and Planetary Science Letters www.elsevier.com/locate/epsl Late Cretaceous–Palaeogene topography of the Chinese Tian Shan: New insights from geomorphology and sedimentology ∗ Marc Jolivet a, , Laurie Barrier b, Olivier Dauteuil a, Amandine Laborde b, Qian Li c, Bettina Reichenbacher d, Speranta-Maria Popescu e, Jingeng Sha f, Zhaojie Guo c a Univ Rennes, CNRS, Géosciences Rennes, UMR 6118, CNRS, F-35000 Rennes, France b Institut de Physique du Globe de Paris, Sorbonne Paris Cité, Université Paris Diderot, UMR 7154 CNRS, Paris, France c Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Peking University, Beijing, 100871, China d Department für Geo- und Umweltwissenschaften, Paläontologie & Geobiologie, Ludwig-Maximilians-Universität München, Richard-Wagner-Str. 10, 80333 München, Germany e Geobiostratadata Consulting, 385 Route du Mas Rillier, 69140, Rillieux la Pape, France f Nanjing Institute of Geology and Palaeontology, Chinese Academy of Science, Nanjing 210008, China a r t i c l e i n f o a b s t r a c t Article history: The Cenozoic growth of the intra-continental Tian Shan Range initiated during the late Eocene–Oligocene, Received 12 April 2018 and led to a tectonic reactivation of the complex Palaeozoic and Mesozoic lithospheric structure. Due to Received in revised form 25 June 2018 the very low erosion rates linked to the semi-arid climate that characterised the Tian Shan region during Accepted 1 July 2018 most of the Cenozoic, the topography of the range is not at equilibrium with deformation. -
The Xinjiang Problem
THE XINJIANG PROBLEM Graham E. Fuller S. Frederick Starr © Central Asia-Caucasus Institute Paul H. Nitze School of Advanced International Studies The Johns Hopkins University Tel.: 1 202 663 7723 [email protected] The Xinjiang Problem 3 Table of Contents Introduction: The Xinjiang Project............................................. 1 I. What is the Problem in Xinjiang? ...........................................4 II. The Geopolitical Realities: a Primer......................................10 III. What Do The Key Players Want? .......................................16 Uyghur Grievances.................................................................................. 16 Uyghur Goals and Actions ........................................................................22 China’s Grievances..................................................................................26 China’s Goals and Actions ........................................................................30 IV. What Is At Stake? Why The Xinjiang Problem Matters ........33 Implications for Ethnic Minorities.............................................................. 33 Uyghurs and the Muslim World.................................................................34 Terrorism .............................................................................................. 40 China and Regional Geopolitics..................................................................43 Human Rights Issues................................................................................47 Economic -
Cenozoic Deformation of the Tarim Plate and the Implications for Mountain Building in the Tibetan Plateau and the Tian Shan
TECTONICS, VOL. 21, NO. 6, 1059, doi:10.1029/2001TC001300, 2002 Cenozoic deformation of the Tarim plate and the implications for mountain building in the Tibetan Plateau and the Tian Shan Youqing Yang and Mian Liu Department of Geological Sciences, University of Missouri, Columbia, Missouri, USA Received 11 May 2001; revised 14 March 2002; accepted 8 June 2002; published 17 December 2002. [1] The Tarim basin in NW China developed as a the geology and tectonics of the Himalayan-Tibetan orogen complex foreland basin in the Cenozoic in association [Dewey and Burke, 1973; Molnar and Tapponnier, 1975; with mountain building in the Tibetan Plateau to the Allegre et al., 1984; Armijo et al., 1986; Burchfiel et al., south and the Tian Shan orogen to the north. We 1992; Harrison et al., 1992; Avouac and Tapponnier, 1993; reconstructed the Cenozoic deformation history of the Nelson et al., 1996; England and Molnar, 1997; Larson et Tarim basement by backstripping the sedimentary al., 1999; Yin and Harrison, 2000]. However, some funda- mental questions, such as how stress has propagated across rocks. Two-dimensional and three-dimensional finite the collisional zone and how strain was partitioned between element models are then used to simulate the flexural crustal thickening and lateral extruding of the lithosphere, deformation of the Tarim basement in response to the remain controversial. One end-member model, approximat- sedimentary loads and additional tectonic loads ing the Eurasia continent as a viscous thin sheet indented by associated with overthrusting of the surrounding the rigid Indian plate [e.g., England and McKenzie, 1982; mountain belts. -
Chinese Historian Su Beihai's Manuscript About the History Of
UDC 908 Вестник СПбГУ. Востоковедение и африканистика. 2020. Т. 12. Вып. 4 Chinese Historian Su Beihai’s Manuscript about the History of Kazakh People in Central Asia: Historical and Source Study Analysis* T. Z. Kaiyrken, D. A. Makhat, A. Kadyskyzy L. N. Gumilyov Eurasian National University, 2, ul. Satpayeva, Nur-Sultan, 010008, Kazakhstan For citation: Kaiyrken T. Z., Makhat D. A., Kadyskyzy A. Chinese Historian Su Beihai’s Manuscript about the History of Kazakh People in Central Asia: Historical and Source Study Analysis. Vestnik of Saint Petersburg University. Asian and African Studies, 2020, vol. 12, issue 4, pp. 556–572. https://doi.org/10.21638/spbu13.2020.406 The article analyses the research work of Chinese scientist Su Beihai on Kazakh history, one of the oldest nationalities in Eurasia. This work has been preserved as a manuscript and its main merit is the study of Kazakh history from early times to the present. Moreover, it shows Chinese scientists’ attitude to Kazakh history. Su Beihai’s scientific analysis was writ- ten in the late 1980s in China. At that time, Kazakhstan was not yet an independent country. Su Beihai drew on various works, on his distant expedition materials and demonstrated with facts that Kazakh people living in their modern settlements have a 2,500-year history. Although the book was written in accordance with the principles of Chinese communist historiography, Chinese censorship prevented its publication. Today, Kazakh scientists are approaching the end of their study and translation of Su Beihai’s manuscript. Therefore, the article first analyses the most important and innovative aspects of this work for Kazakh history. -
Seismic Hazard in Tien Shan: Basement Structure Control Over the Deformation Induced by Indo-Eurasia Collision
8 Seismic Hazard in Tien Shan: Basement Structure Control Over the Deformation Induced by Indo-Eurasia Collision Buslov, Mikhail M.1 and De Grave, Johan2 1Institute of Geology and Mineralogy SB RAS, Novosibirsk, 2Department of Mineralogy & Petrology, Geological Institute, Ghent University, Gent, 1Russia, 2Belgium 1. Introduction The Tien Shan are an active intracontinental mountain belt that is part of the Central Asian Orogenic System (fig. 1). In general the mountain belt is composed of E-W trending ranges, separated by (sub)-parallel intramontane depressions. The western part of the Tien Shan is for a large extent situated in the Republic of Kyrgyzstan, while the eastern part is located in China. The Tien Shan can be regarded as a mobile belt between two rigid micro-continent or micro- plates: to the south this is the Tarim plate, to the north, the Aktyuz-Boordin (which in fact represents the southern part of Kazakhstan-Junggar plate) (fig. 2). The Tien Shan belt was formed during the Palaeozoic closure of the Turkestan Ocean [Allen et al., 1992; Gao et al., 1998; Chen et al., 1999; Brookfield, 2000]. Island-arc systems and micro-plates converged with the northern margin of Tarim and were accreted to Tarim in the Middle to Late Palaeozoic. Final closure of the Turkestan oceanic basin was accomplished in the Late Palaeozoic, in the Permian, when the Tarim and Tien Shan units collided with the Kazakhstan-Junggar plate [Laurent-Charvet et al., 2002; Van der Voo et al., 2006; Yang et al., 2007]. At this time, in the Permo-Triassic, this entire assemblage was also docked to the Siberian continent further north in present-day co-ordinates [Carroll et al., 1995; Levashova et al. -
UN in Dialogue with China to Visit Xinjiang
UN in dialogue with China to visit Xinjiang April 10, 2021 Several governments have pressed China to allow UN rights inspectors to visit Xinjiang after raising allegations of “appalling” human rights abuses against the Uighur minority people. In news: U.K. urges China to grant UN access to Xinjiang Placing it in syllabus: Foreign Affairs Dimensions Map of Xinjiang Province Ethnic Problem Importance of the region for China Chinese initiatives in the region Problems with the Chinese policies and the UN’s position in it India and the Xinjiang Problem Content: Map of Xinjiang Province: Xinjiang, officially Xinjiang Uygur Autonomous Region (XUAR), is an autonomous region of the People’s Republic of China (PRC). It is located in the northwest of the country close to Central Asia. It is the largest province-level division of China and the 8th-largest country subdivision in the world, Borders: Xinjiang borders the countries of Mongolia, Russia, Kazakhstan, Kyrgyzstan, Tajikistan, Afghanistan, Pakistan and India. The rugged Karakoram, Kunlun and Tian Shan mountain ranges occupy much of Xinjiang’s borders, as well as its western and southern regions. The Aksai Chin region, administered by China, is claimed by India. Xinjiang also borders the Tibet Autonomous Region and the provinces of Gansu and Qinghai. The most well-known route of the historic Silk Road ran through the territory from the east to its northwestern border. Ethnic Problem: Xinjiang is home to a number of ethnic groups, including the Turkic Uyghur, Kazakhs and Kyrgyz, the Han, Tibetans, Hui, Tajiks, Mongols, Russians and Sibe. Xinjiang has seen a history of ethnic tensions between the native Uighur Muslims and majority Han Chinese migrants. -
Geology of the Tarim Basin with Special Emphasis on Petroleum Deposits, Xinjiang Uygur Zizhiqu, Northwest China
Geology of the Tarim Basin with special emphasis on petroleum deposits, Xinjiang Uygur Zizhiqu, Northwest China By K. Y. Lee U.S. Geological Survey Reston, Virginia Open-File Report 85-616 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. 1985 CONTENTS Page Abstract 1 Introduction 2 Regional setting 6 Purpose, scope, and method of report 6 S t rat igraphy 6 Jr r e""D inian Q Sinian 8 Paleozoic 10 Lower Paleozoic 11 Upper Paleozoic 12 Mesozoic 15 Tr ias s i c 15 Jurassi c 16 Cretaceous 17 Cenozoic 18 Tertiary 18 Quat e rnar y 2 0 Structure 21 Kuqa Foredeep 21 Northern Tarim Uplift 21 Eastern Tarim Depression 24 Central Uplift 24 Southwestern Depression 26 Kalpin Uplift 26 Southeastern Faulted Blocks 27 Evolution of the basin 27 Petroleum and coal deposits 36 Petroleum 36 Source rocks 36 Reservoir rocks 44 Cap rocks 45 Types of trap 47 Potential and description of known oil and gas fields 47 Occurrence 50 Potential 50 Summary and conclusions 52 References cited 54 ILLUSTRATIONS Page Figure 1. Index map of China 3 2. Geologic map of the Tarim (Talimu) basin, Xinjiang, northwest China 4 3. Airborne magnetic anomaly contours in Ta 9 4. Principal structural units 22 5. Sketch isopachs of the earth's crust 23 6. Depth to the magnetic basement rocks 25 7. Isopachs of the Paleozoic and Sinian strata 29 8. Isopachs of the Cenozoic and Mesozoic strata 30 9. Isopachs of the Jurassic strata 32 10. -
Geology of the Petroleum and Coal Deposits in the Junggar (Zhungaer) Basin, Xinjiang Uygur Zizhiqu, Northwest China by K. Y
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Geology of the petroleum and coal deposits in the Junggar (Zhungaer) basin, Xinjiang Uygur Zizhiqu, northwest China By K. Y. Lee Open-File Report 85-230 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature, 1985 CONTENTS Page ADS tract ~~ ~~ 1 T.__introduction 4_ ~» ~^ J _ _ -^ 4_ ^ *-* * _ ~~ _ _ __ jO General statement ~ 3 Regional setting ~~ 3 Purpose, scope, and method of the report 6 ot ra t ig rapriy Pre-Carboniferous 6 Lower Paleozoic _______ ^ Devonian o Upper Paleozoic Carboniferous and Permian 8 Carboniferous 8 c"D cA Ly» II1J--y. 3 allf~ _. ~~ "~ "~ ______ ____ ^1 ^1 Me so zoic ~~ 1 j T*^»iLiaysxc -I f* ft ft £ -» ^__ ____ _._ _ __ _ __ _ ^ _^ _ _ _ _ ^1 -jC JurassicT_.___J_ ±o1Q f"tjic1 'r»x.k denozoi c n^A w» ±cJ. Quaternary 2.1 Geotectonics and evolution of the basin 27 .tectonics and sedimentation 2.1 OQ "I"L. **iiI. Ut- r* -f"uUUJL v»£k C _ __ _ "~ "~ JO ^O iNOLLncrnVT -» ~» ^- l_ --. ^» _ iriaLrorm"O 1 « *- f y-k «*rn ~ oz*5 O Northern Tian Shan Foredeep 33 Jretroieum and coal deposits IT~D C£^ -I"L *V*JL (JXcULllf\ 1 A11TYI __ ~~ _________________________________________ j^O /l Source rocks 35 Reservoir rocks ~ 37 LT3f\t- \J LCllLlet Qi->4- -i n -L1 ~~ ~~ ~~ . i+/ i.1 ____________________ _ ______________________________________ /, Q uccurrence ^ ^ ^y T?jxci rt -p Crt T»^Y>JL C11L.CO /^ £1 O t-J./ » "1 t"^k^1Led K>^«*«.^«.^«. -
The Crustal Structure from the Altai Mountains to the Altyn Tagh Fault, Northwest China Youxue Wang,1,2,3 Walter D
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 108, NO. B6, 2322, doi:10.1029/2001JB000552, 2003 The crustal structure from the Altai Mountains to the Altyn Tagh fault, northwest China Youxue Wang,1,2,3 Walter D. Mooney,2 Xuecheng Yuan,4 and Robert G. Coleman5 Received 30 March 2001; revised 7 November 2002; accepted 17 March 2003; published 28 June 2003. [1] We present a new crustal section across northwest China based on a seismic refraction profile and geologic mapping. The 1100-km-long section crosses the southern margin of the Chinese Altai Mountains, Junggar Accretional Belt and eastern Junggar basin, easternmost Tianshan Mountains, and easternmost Tarim basin. The crustal velocity structure and Poisson’s ratio (s), which provide a constraint on crustal composition, were determined from P and S wave data. Despite the complex geology, the crustal thickness along the entire profile is nearly uniform at 50 km. The thickest crust (56 km) occurs at the northern end of the profile beneath the Altai Mountains and the thinnest (46 km) crust is beneath the Junggar basin. Beneath surficial sediments, the crust is found to have three layers with P wave velocities (Vp) of 6.0–6.3, 6.3–6.6, and 6.9–7.0 km/s, respectively. The southern half of the profile, including the eastern Tianshan Mountains and eastern margin of the Tarim basin, shows low P wave velocities and s = 0.25 to a depth of 30 km, which suggests a quartz-rich, granitic upper crustal composition. The northern half of the profile below the Altai Mountains and Junggar Accretional Belt has a higher Poisson’s ratio of s = 0.26–0.27 to a depth of 30 km, indicative of an intermediate crustal composition. -
Flora and Vegetation of the Oytagh Valleys: Phytogeography of an Isolated Coniferous Mountain Forest in Arid Central Asia (Western Kunlun Shan, China)
Flora and vegetation of the Oytagh Valleys: Phytogeography of an isolated coniferous mountain forest in arid Central Asia (Western Kunlun Shan, China) UBBO WüNDISCH W. BERNHARD DICKORÉ & GEORG MIEHE ABSTRACT WÜNOlSCH, U., W. B. OlCKORÉ & G. MIEHE (2003). Flora and vegetation ofthe Oytagh Val leys: Phytogeography of an isolated coniferous mountain forest in arid Central Asia (Western Kunlun Shan, China). Cal/do//ea 58: 215-269. In English, English, French and German abstracts. An annotated list of f10wering plants and ferns from the westernmost fringe of the Kunlun Shan Mountains and adjacent Chinese Eastern Pamir, and an overview on the vegetation of the upper Oytagh Valleys is presented. In total, 431 species ofvascular plants (4 Ptel'idophyta, 3 COl/ifel'ae, 3 Gnetopsida, 321 Dicoty/edol/eae, 100 MOl/ocoty/edoneae) are reported with their respective alti tudinal range, autecological and distributional features. A list of mosses (31 Musci, 1 Hepaticae) and lichens (27 species) is appended. The phytogeographical position and differentiation of the area, phytodiversity and utilisation properties of the natural ressources are discussed. RÉSUMÉ WÜNDISCH, U., W. B. DICKORÉ & G. MIEHE (2003). Flore et végétation des vallées d'Oy tagh: phytogéographie d'une forêt isolée de coniféres d'une montagne d'Asie Centrale (Kunlun Shan occidental, Chine). Cal/dol/ea 58: 215-269. En anglais, résumés anglais, français et alle mand. Les auteurs présentent un bref aperçu des unités végétales de la haute vallée d'Oytagh et une liste commentée des plantes vasculaires du Kunlun Shan occidental et du Pamir oriental chinois. 431 espéces de plantes vasculaires (4 Ptel'idophyta, 3 COl/iferae, 3 GI/etopsida, 321 Dicotyledol/eae, 100 MOl/ocotyledoneae) sont listées avec leur distribution selon l'altitude et leurs caractéristiques autécologiques et chorologiques.