Coordinated Development Between Assistance to Tibet and Tourism Development: Spatial Patterns and Influencing Factors
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Modelling the Effects of Climatic Factors on the Biomass and Rodent Distribution in a Tibetan Grassland Region in China
University of Kentucky UKnowledge International Grassland Congress Proceedings XXII International Grassland Congress Modelling the Effects of Climatic Factors on the Biomass and Rodent Distribution in a Tibetan Grassland Region in China Quanzhen Wang Northwest A&F University, China Maolin Xia Tibet Autonomous Region, China Bai-Song Tibet Autonomous Region, China Xi-Rao-Zhuo-Ma Tibet Autonomous Region, China Ba-Sang Tibet Autonomous Region, China See next page for additional authors Follow this and additional works at: https://uknowledge.uky.edu/igc Part of the Plant Sciences Commons, and the Soil Science Commons This document is available at https://uknowledge.uky.edu/igc/22/2-13/2 The XXII International Grassland Congress (Revitalising Grasslands to Sustain Our Communities) took place in Sydney, Australia from September 15 through September 19, 2013. Proceedings Editors: David L. Michalk, Geoffrey D. Millar, Warwick B. Badgery, and Kim M. Broadfoot Publisher: New South Wales Department of Primary Industry, Kite St., Orange New South Wales, Australia This Event is brought to you for free and open access by the Plant and Soil Sciences at UKnowledge. It has been accepted for inclusion in International Grassland Congress Proceedings by an authorized administrator of UKnowledge. For more information, please contact [email protected]. Presenter Information Quanzhen Wang, Maolin Xia, Bai-Song, Xi-Rao-Zhuo-Ma, Ba-Sang, Jiang- Cuo, Zha-Dui, Jin-Mei, Ze-Duo, Surong Li, Zha-Xi, Yang-Ba, Jia-Yang, Dan-Pei, Jian Cui, and Jimin Cheng This event -
Himalaya - Southern-Tibet: the Typical Continent-Continent Collision Orogen
237 Himalaya - Southern-Tibet: the typical continent-continent collision orogen When an oceanic plate is subducted beneath a continental lithosphere, an Andean mountain range develops on the edge of the continent. If the subducting plate also contains some continental lithosphere, plate convergence eventually brings both continents into juxtaposition. While the oceanic lithosphere is relatively dense and sinks into the asthenosphere, the greater sialic content of the continental lithosphere ascribes positive buoyancy in the asthenosphere, which hinders the continental lithosphere to be subducted any great distance. Consequently, a continental lithosphere arriving at a trench will confront the overriding continent. Rapid relative convergence is halted and crustal shortening forms a collision mountain range. The plane marking the locus of collision is a suture, which usually preserves slivers of the oceanic lithosphere that formerly separated the continents, known as ophiolites. The collision between the Indian subcontinent and what is now Tibet began in the Eocene. It involved and still involves north-south convergence throughout southern Tibet and the Himalayas. This youthful mountain area is the type example for studies of continental collision processes. The Himalayas Location The Himalayas form a nearly 3000 km long, 250-350 km wide range between India to the south and the huge Tibetan plateau, with a mean elevation of 5000 m, to the north. The Himalayan mountain belt has a relatively simple, arcuate, and cylindrical geometry over most of its length and terminates at both ends in nearly transverse syntaxes, i.e. areas where orogenic structures turn sharply about a vertical axis. Both syntaxes are named after the main peaks that tower above them, the Namche Barwa (7756 m) to the east and the Nanga Parbat (8138 m) to the west, in Pakistan. -
Holocene Erosion of the Lesser Himalaya Triggered by Intensified
Holocene erosion of the Lesser Himalaya triggered by intensifi ed summer monsoon Peter D. Clift School of Geosciences, University of Aberdeen, Aberdeen AB24 3UE, UK Liviu Giosan Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA Jerzy Blusztajn Ian H. Campbell Research School of Earth Sciences, Australian National University, Canberra, ACT 0200, Australia Charlotte Allen Malcolm Pringle Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, USA Ali R. Tabrez Mohammed Danish National Institute for Oceanography, Clifton, Karachi 75600, Pakistan M.M. Rabbani Anwar Alizai Geological Survey of Pakistan, Block 2, Gulistan e Jauhar, Karachi, Pakistan Andrew Carter School of Earth Sciences, University and Birkbeck College London, Gower Street, London WC1E 6BT, UK Andreas Lückge Bundesanstalt für Geowissenschaften und Rohstoffe, Stilleweg 2, D-30655 Hannover, Germany ABSTRACT We study the erosional response of the Indus drainage basin, encom- Climate is one of the principal controls setting rates of conti- passing a number of ranges located in the western Himalaya (Fig. 1). The nental erosion. Here we present the results of a provenance analysis vast majority of the sediment eroded in this region is delivered to the delta of Holocene sediments from the Indus delta in order to assess climatic via the Indus River and its tributaries. Consequently changes in the prov- controls on erosion over millennial time scales. Bulk sediment Nd iso- enance of sediment reaching the delta can be used to understand how cli- tope analysis reveals a number of changes during the late Pleistocene mate change since the last deglaciation has infl uenced Himalayan erosion. -
Food Security: Indicators, Measurement, and the Impact of Household
Food Security: Indicators, Measurement, and the Impact of Household Behavior on Food Acquisition and Allocation, Experimental Evidence from Tibet, China Yuan-lin HUANG1, Xiang-mei LI2,3, Lars Lefgren4, 1.College of Natural Resource and Environment, Qinzhou University, Guangxi, China, 535000; 2. College of Economics and Management, Nanjing Agricultural University,Nanjing ,China 210095; 3. China Center for Food Security Studies, Nanjing Agricultural University,Nanjing ,China 210095; 4.Department of Economics, Brigham Young University, Provo, UT, United States, 84604) Yuan-lin HUANG, Ph.D, Associate Professor, [email protected] Corresponding Author: Xiang-mei LI, Ph.D. Professor. Email: [email protected] Selected Paper prepared for presentation at the 2015 AAEA & WAEA Joint Annual Meeting, San Francisco, California, 26-28 July 2015 Abstract This paper aimed to determine the magnitude of food insecurity and its determinants in rural households of Tibet, China. In this paper, a community based cross-sectional study was conducted from 2002 to 2013, whole about Tibet (this survey program was founded by Tibet Government Founding). In the study, household heads were recruited using a multistage random sampling technique. Data were collected by face-to-face interviews using the Household Food Insecurity Access Scale (HFIAS) tool after verbal informed consent. We chosen the same districts, same household, collected data every two years, totally number of the households is 736. Based on the data of sample investigation, combined with individual anthropometric estimates for children and a thorough understanding of household behavior, we moved beyond the simple head count measure of food insecurity in this paper and proposed three measures of food insecurity, along the lines of new poverty measures and explained the desirable properties of these measures that are not present in the head count measure. -
Human-Wildlife Conflict in the Chang Tang Region of Tibet
Human-Wildlife Conflict in the Chang Tang Region of Tibet: The Impact of Tibetan Brown Bears and Other Wildlife on Nomadic Herders Dawa Tsering, John Farrington, and Kelsang Norbu August 2006 WWF China – Tibet Program Author Contact Information: Dawa Tsering, Tibet Academy of Social Sciences and WWF China – Tibet Program Tashi Nota Hotel 24 North Linkuo Rd. Lhasa, Tibet Autonomous Region 850 000 People’s Republic of China [email protected] (+86)(891) 636-4380 John D. Farrington Tibet University 36 Jiangsu Road Lhasa, Tibet Autonomous Region 850 000 People’s Republic of China [email protected] [email protected] Kelsang Norbu WWF China – Tibet Program Tashi Nota Hotel 24 North Linkuo Rd. Lhasa, Tibet Autonomous Region 850 000 People’s Republic of China [email protected] Human-Wildlife Conflict in the Chang Tang Region of Tibet Abstract The multiple-use Chang Tang and Seling Lake Nature Reserves were created in 1993 to protect the unique assemblage of large fauna inhabiting the high-altitude steppe grasslands of northern Tibet, including the Tibetan antelope, Tibetan wild ass, Tibetan brown bear, Tibetan Gazelle, wild yak, and snow leopard. Prior to creation of the reserve, many of these species were heavily hunted for meat and sale of parts. Since creation of the reserve, however, killing of wildlife by subsistence hunters and commercial poachers has declined while in the past five years a new problem has emerged, that of human-wildlife conflict. With human, livestock, and wildlife populations in the reserves all increasing, and animals apparently emboldened by reserve-wide hunting bans, all forms of human-wildlife conflict have surged rapidly since 2001. -
Tibet Advocacy Coalition
TIBET ADVOCACY COALITION SUBMISSION TO THE UN COMMITTEE ON THE ELIMINATION OF RACIAL DISCRIMINATION FOLLOW-UP TO THE CONCLUDING OBSERVATIONS OF CHINA’S COMBINED FOURTEENTH TO SEVENTEENTH PERIODIC REPORTS Joint Report Submitted on 30 July 2020 CONTENTS INTRODUCTION 3 BROAD DEFINITION OF SEPARATISM 3 2.1 The Committee’s Concluding Observations 3 2.2 Tibet Advocacy Coalition’s Assessment 4 DETENTION OF TIBETANS 6 3.1 The Committee’s Concluding Observations 6 3.2 Tibet Advocacy Coalition’s Assessment 6 ERASING THE TIBETAN LANGUAGE 9 4.1 The Committee’s Concluding Observations 9 4.2 Tibet Advocacy Coalition’s Assessment 9 RESTRICTIONS ON TIBETANS’ FREEDOM OF MOVEMENT 12 5.1 The Committee’s Concluding Observations 12 5.2 Tibet Advocacy Coalition’s Assessment 12 DISCRIMINATION IN EMPLOYMENT 14 6.1 The Committee’s Concluding Observations 14 6.2 Tibet Advocacy Coalition’s Assessment 14 1. INTRODUCTION Tibet Advocacy Coalition presents this submission to the United Nations (UN) Committee on the Elimination of Racial Discrimination (the Committee) to inform the follow-up procedure in relation to the Concluding Observations on the combined fourteenth to seventeenth periodic reports of the People’s Republic of China (PRC) in August 2018.1 As requested by the Committee, Tibet Advocacy Coalition evaluates China’s progress in implementing the Committee’s recommendations and would like to provide the following information in relation to: broad definitions of terrorism and separatism (paragraphs 36 and 37), Torture and ill-treatment (paragraphs 38 and 39), Tibetans (paragraphs 43 and 44); and employment (paragraphs 47 and 48). 1 UN Committee on the Elimination of Racial Discrimination (CERD), UN Committee on the Elimination of Racial Discrimination: Concluding Observations, People's Republic of China, 19 September 2018, CERD/C/CHN/CO/14-17, available at: https://tbinternet.ohchr.org/_layouts/15/treatybodyexternal/Download.aspx?symbolno=CERD%2fC%2fCHN%2fCO%2f14-17&Lang=en 2. -
Quaternary River Erosion, Provenance, and Climate Variability
Louisiana State University LSU Digital Commons LSU Doctoral Dissertations Graduate School 2017 Quaternary River Erosion, Provenance, and Climate Variability in the NW Himalaya and Vietnam Tara Nicole Jonell Louisiana State University and Agricultural and Mechanical College Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_dissertations Part of the Earth Sciences Commons Recommended Citation Jonell, Tara Nicole, "Quaternary River Erosion, Provenance, and Climate Variability in the NW Himalaya and Vietnam" (2017). LSU Doctoral Dissertations. 4423. https://digitalcommons.lsu.edu/gradschool_dissertations/4423 This Dissertation is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Doctoral Dissertations by an authorized graduate school editor of LSU Digital Commons. For more information, please [email protected]. QUATERNARY RIVER EROSION, PROVENANCE, AND CLIMATE VARIABILITY IN THE NW HIMALAYA AND VIETNAM A Dissertation Submitted to the Graduate Faculty of the Louisiana State University and Agricultural and Mechanical College in partial fulfillment of the requirements for the degree of Doctor of Philosophy in The Department of Geology and Geophysics by Tara Nicole Jonell B.S., Kent State University 2010 M.S., New Mexico State University, 2012 May 2017 ACKNOWLEDGMENTS There are so many people for which I am thankful. Words can barely express the gratitude I have for my advisor, Dr. Peter D. Clift, who has countlessly provided humor and outstanding support throughout this project. I cannot imagine completing this research without his untiring guidance both in the lab and outside in the field. I also wish to thank my advisory committee for their invaluable insight and patience: Dr. -
October 21, 1953 Cable from Zhang Jingwu, 'On Issues of Relations Between China and India in Tibet'
Digital Archive digitalarchive.wilsoncenter.org International History Declassified October 21, 1953 Cable from Zhang Jingwu, 'On Issues of Relations between China and India in Tibet' Citation: “Cable from Zhang Jingwu, 'On Issues of Relations between China and India in Tibet',” October 21, 1953, History and Public Policy Program Digital Archive, PRC FMA 105-00032-23, 76-81. Translated by 7Brands. http://digitalarchive.wilsoncenter.org/document/114754 Summary: Zhang Jingwu reports on the Simla Accord and the McMahon line running between India and Tibet, and offers policy recommendations. Credits: This document was made possible with support from the MacArthur Foundation. Original Language: Chinese Contents: English Translation [...] On Issues of Relations between China and India in Tibet To the Ministry of Foreign Affairs: Your correspondence dated 7 October [1953] and the two types of Indian documents have been received. Research shows that the assumption that “India intends to capitalize on this opportunity to have some benefit in Tibet,” as mentioned in your correspondence, is very accurate. Based on the information that we have at hand about Tibet, we still need Indian cooperation in some international issues. However, India is capitalizing on our temporary difficulties in Tibet, particularly our insufficient understanding of imperialist privileges in Tibet and the ideal solution to border disputes, as well as our need for India’s cooperation in various areas, to gain benefits by offering a general solution to the Tibet issue. As a matter of fact, there have always been disputes on some issues, e.g. commercial exchanges and representative offices, because we have always claimed our sovereignty over Tibet. -
176-Mcrivette Etal-20+
Tectonophysics 751 (2019) 150–179 Contents lists available at ScienceDirect Tectonophysics journal homepage: www.elsevier.com/locate/tecto Cenozoic basin evolution of the central Tibetan plateau as constrained by U- Pb detrital zircon geochronology, sandstone petrology, and fission-track T thermochronology ⁎ Michael W. McRivettea, , An Yinb,c, Xuanhua Chend, George E. Gehrelse a Department of Geological Sciences, Albion College, Albion, MI 49224, USA b Department of Earth, Planetary, and Space Sciences, University of California, Los Angeles, CA 90095-1567, USA c Structural Geology Group, School of Earth Sciences and Resources, China University of Geosciences (Beijing), Beijing 10083, China d Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China e Department of Geosciences, University of Arizona, Tucson, AZ 85721, USA ARTICLE INFO ABSTRACT Keywords: We conduct sandstone-composition analysis, U-Pb detrital-zircon dating, and apatite fission-track thermo- Hoh Xil Basin chronology to determine how basin development was associated with the Cenozoic deformation across central Qaidam Basin Tibet. Our results are consistent with a two-stage basin development model: first a single fluvial-lacustrine Kunlun Range system formed (i.e., Paleo-Qaidam basin) in between two thrust belts (i.e., the Fenghuoshan and Qilian Shan Tibetan plateau thrust belts) in the Paleogene, which was later partitioned into two sub-basins in the Neogene by the Kunlun U-Pb zircon geochronology transpressional system and its associated uplift. The southern sub-basin (i.e., Hoh Xil basin) strata have detrital- zircon age populations at 210–300 Ma and 390–480 Ma for the Eocene strata and at 220–310 Ma and 400–500 Ma for the early Miocene strata; petrologic analysis indicates that the late Cretaceous-Eocene strata were recycled from the underlying Jurassic rocks. -
Études Mongoles Et Sibériennes, Centrasiatiques Et Tibétaines, 50 | 2019 Dismemberment and Sharing of Game Meat by Pastoralist Hunters on the Tibetan
Études mongoles et sibériennes, centrasiatiques et tibétaines 50 | 2019 Animals in the religion and culture of the Tibetan Plateau Dismemberment and sharing of game meat by pastoralist hunters on the Tibetan Plateau Démembrement et partage de la viande de gibier par les chasseurs des communautés pastorales du plateau tibétain Toni Huber Electronic version URL: https://journals.openedition.org/emscat/3969 DOI: 10.4000/emscat.3969 ISSN: 2101-0013 Publisher Centre d'Etudes Mongoles & Sibériennes / École Pratique des Hautes Études Electronic reference Toni Huber, “Dismemberment and sharing of game meat by pastoralist hunters on the Tibetan Plateau”, Études mongoles et sibériennes, centrasiatiques et tibétaines [Online], 50 | 2019, Online since 04 March 2019, connection on 13 July 2021. URL: http://journals.openedition.org/emscat/3969 ; DOI: https://doi.org/10.4000/emscat.3969 This text was automatically generated on 13 July 2021. © Tous droits réservés Dismemberment and sharing of game meat by pastoralist hunters on the Tibetan ... 1 Dismemberment and sharing of game meat by pastoralist hunters on the Tibetan Plateau Démembrement et partage de la viande de gibier par les chasseurs des communautés pastorales du plateau tibétain Toni Huber Introduction 1 Among rural societies of the Tibetan Plateau and immediately adjacent Himalayan highlands, most hunting practices can be clearly divided into three phases. This is so regardless of the actual hunting technique involved (e.g. driving, ambush, trapping, etc.). The initial phase occurs prior to a chase, the second during the chase itself and includes the actual kill, while the final one involves processing of the animal’s carcass. My study reports on this third phase of practices during hunting. -
A New Species of Triplophysa (Cypriniformes, Nemacheilidae) from Weihe River in Gansu Province, China
ZOOLOGICAL RESEARCH A new species of Triplophysa (Cypriniformes, Nemacheilidae) from Weihe River in Gansu Province, China DEAR EDITOR, (Supplementary Table S1). Following an investigation of Triplophysa species from Weihe River (Figure 1A), 15 A new species of Tibetan loach, Triplophysa weiheensis sp. specimens superficially resembling Triplophysa stoliczkae nov., is described from the Weihe River in Gansu Province, Steindachner 1866 (Supplementary Figure S1) were collected China, based on morphological and molecular analyses. The and are described herein as a new species based on new species can be distinguished from all known congeners morphological and molecular analyses. by a unique combination of the following characters: scaleless; After euthanization (see Supplementary Methods), the left snout abruptly sloping downward, anterior to anterior nostril; ventral fin of some specimens was removed and preserved in lower jaw crescentic, not sharp; body without obvious mottling; 95% ethanol for DNA extraction. Voucher specimens were lateral line interrupted on posterior trunk at pelvic-fin distal labeled and stored in 70% ethanol. Specimens were deposited extremity; caudal-peduncle length 2.0–2.7 times its depth; in the collection of the Northwest Institute of Plateau Biology branched rays of pectoral fin 10–11; branched rays of pelvic (NWIPB), Chinese Academy of Sciences, Xining, Qinghai, fin 5–6; inner gill rakers on 1st gill arch 14–16; vertebrae China. Morphological measurements and counts followed 4+34–36; intestine with 6–7 loops, length ca. 1.8 times SL Kottelat (1990) and Prokofiev (2007). Additional (n=3); bony capsule of air bladder small and thin; posterior measurements are described in the Supplementary Methods. -
Mt. Kailash Parikrama/ Trekking /Kora
Kailash ψ Om Namah Shivay ψ Kailash Mansarovar Yatra yatra.org - https://www.kailash INFORMATION☎ +91 11 40504050 GUIDE 8800750030 [email protected] https://www.kailashMax Holidays-yatra.org Pvt. Ltd. yatra.org - Embark on the holiest adventure to rejuvenate your mind, body and https://www.kailash ☎ +91 11 40504050 8800750030 [email protected] https://www.kailash-yatra.org Kailash Manasarovar Yatra ___ Carrying a prolific relevance for the Hindus, Buddhists, Bonpos as well as the Jains, this heavenly abode to Lord Shiva is an immensely pious journey for all the divinity seekers. Tucked in the Tibet Autonomous Region in China, the beguiling and positive aura of the Kailash Manasarovar Yatra is here to let you entangle in its extreme auspiciousness. -------------------------------------------------------------------------------------------------------------------------------------- Mt. Kailash and Lake Manasarovar Mt. Kailash is known to be the heavenly abode of Lord Shiva and is also considered to be a pilgrimage destination packed with some of the most fascinating lessons of spirituality. It is situated in the Kailash Range (Gangdise Mountains) of the Transhimalaya and carries a highly religious importance too. yatra.org - On the other hand, considered as the most sacred lake in Tibet, Lake Manasarovar is majorly prominent as the world's highest freshwater lake and millions of ardent devotees come from the nook and corners of this world to experience its unique beauty lying at an elevation of 4,590 m. https://www.kailash People and Language Mount Kailash lies in the Tibet Autonomous Region in China and the people living here are the Tibetans covering more than 90% of the population, Chinese and also the Nepalis.