Spatial Fairness and Changes in Transport Infrastructure in the Qinghai-Tibet Plateau Area from 1976 to 2016

Total Page:16

File Type:pdf, Size:1020Kb

Spatial Fairness and Changes in Transport Infrastructure in the Qinghai-Tibet Plateau Area from 1976 to 2016 sustainability Article Spatial Fairness and Changes in Transport Infrastructure in the Qinghai-Tibet Plateau Area from 1976 to 2016 Xingchuan Gao 1,2,3 , Tao Li 2,3 and Xiaoshu Cao 2,3,* 1 School of Geography and Tourism, Shaanxi Normal University, Xi’an 710119, China; [email protected] 2 Northwest Land and Resource Research Centre, Shaanxi Normal University, Xi’an 710119, China; [email protected] 3 Key Laboratory for Urbanization and Land Environment Geo-simulation in Northwest China, Xi’an 710119, China * Correspondence: [email protected] Received: 30 October 2018; Accepted: 17 January 2019; Published: 23 January 2019 Abstract: The Qinghai-Tibet Plateau area (QTP) is the most unique environmental-population region and an important natural laboratory for the study of human-land relations. The poor transportation conditions have long restricted socio-economic development. The research on the transport infrastructure and spatial effect in the QTP is of significance to the sustainable development of the region. Accordingly, a spatial accessibility model was used to analyze the spatial pattern of accessibility in QTP from 1976–2016, examine the accessibility evolution trend on the township scale and reveal the spatial fairness and changes in accessibility. The main conclusions are as follows: (1) The accessibility to major cities improved and the time-space convergence effect was significant. (2) The spatial autocorrelation analysis results showed that the improvement in transport infrastructure had a significant impact on the agglomeration of the accessibility level. (3) Access time from towns to the nearest major city are much shorter. More Tibetan people have more opportunities to access cities. (4) The accessibility coefficient and relative accessibility revealed distributive effects and spatial fairness of accessibility. (5) The global coefficient of variation value demonstrated an increasing trend, which indicates that spatial unfairness of transport is increasing. Keywords: spatial fairness; distributive effects; transport infrastructure; accessibility; the Qinghai-Tibet Plateau area 1. Introduction Transport infrastructure is a necessary prerequisite for promoting regional social and economic development and is a key factor in regional cohesion [1]. Transport construction and network expansion play vital roles in the future development of a region. Accessibility is an important measure of transport networks, used to measure the interaction potential between cities and towns [2]. Harris first measured accessibility using the market potential model in 1954 [3]. Then in 1959, Hansen studied the impact of accessibility on land use [4]. Transport fairness, brought about by the development of the transport network, is closely related to many social issues, such as the number of jobs available and the time spent in public transport [5]. Accessibility has been gradually recognized as an indicator of transport fairness [6–8]. Transport fairness is derived from the study of fairness and justice in other fields [7], in which “fairness” is regarded as the core component of “justice” [9,10]. The research on transport fairness is mostly concentrated on population distribution, investment and public facilities but the concept does not have a single, widely accepted definition [11–13]. In identifying transport fairness, two broad methods to conceive fairness are well-recognized: social fairness and spatial fairness [14]. The first is viewed from a social perspective, wherein vulnerable Sustainability 2019, 11, 589; doi:10.3390/su11030589 www.mdpi.com/journal/sustainability Sustainability 2019, 11, 589 2 of 16 or disadvantaged populations are targeted. The second approach defines fairness in terms of spatial distributive effects, which means easy access, regardless of socioeconomic characteristics, satisfaction or disability [15,16]. In this paper, we adopt the viewpoints from Forth et al. [11] and Delbosc et al. [17] and define the spatial fairness of transport as transport infrastructure that provides benefits evenly among different geographic units. Because the effects of public policies tend to cluster around specific physical locations [18], spatial fairness approaches are well-suited to assess such distributive effects [19]. Transport fairness influences many social aspects, such as territorial cohesion [20], the cost and time spent on daily commutes [21] and on public services [22]. Accessibility is, though imperfect, the most appropriate measure of benefits from transport infrastructure investments [23,24] and transport equity [6,17,25]. Presently, the evaluation of transport fairness has mostly focused on the needs of different social groups [26–28], investment in transport facilities [24,29–31], access to urban facilities [32–34], transportation planning [23,35–38] and interregional linkage strength [25,39–41]. The development of transport infrastructure and improved accessibility have promoted economic relationships and enhanced regional fairness and cohesion in countries and regions such as the UK, Holland, Poland and the European Union (EU) [42–45]. Therefore, the study of accessibility and spatial fairness has become a hot topic in the fields of social economics, transportation planning and human geography. Studies have mainly discussed transport fairness in urban areas or in metropolitan areas, especially emphasizing the root causes of inequity in the distribution of public facilities in a city, while ignoring the spatial effects and spatial fairness of transport in areas of undeveloped economy and unbalanced ecosystem. Although studies on densely populated urban areas are important, the research at the regional scale can guide large-scale transportation and sustainable development planning. As stated above, research on the accessibility and transport fairness in ecologically fragile areas is an important issue in social sustainability and will be a focus of future research. 2. Study Area and Data 2.1. Study Area We selected the Qinghai-Tibet Plateau area as the study area. The Qinghai–Tibet Plateau area is known as “the Roof of the World,” as it contains the headwaters of most streams in Asia and the Third Pole of the Earth [46]. It is an important environmental barrier and the water source in the world and is also the frontier region and a concentrated severely poverty–stricken area of China [47]. However, due to restrictions related to geography, climate and society, transport development in the area has lagged behind for a long time, which historically has hindered the socio–economic development of the region [48]. However, with China Western Development and the construction of major infrastructure, the transport network greatly improved, which has promoted socio–economic development and stability in the region and improved living standards. Tibetans, almost herdsmen, exhibit seasonal rotational grazing, who graze at higher altitudes in summer and at lower altitudes (usually along roads or around towns) in winter. We believe that compared with social fairness, spatial fairness can better solve the current and future transportation planning and construction in a shorter period of time. Therefore, the study on the spatial fairness of transportation in the study area is conducive to improving people’s living standards and providing a useful reference for the development of such underdeveloped regions. The Qinghai–Tibet Plateau area lies between 25◦59037” and 39◦49033” N, 73◦29056” and 104◦40020” E (Figure1), with an area of about 2,542,400 km 2. In order to compare and analyze the evolution and characteristics of the transport network, we selected the administrative divisions of the Qinghai–Tibet Plateau area in 2016 as the study area, which covers six provinces and autonomous regions including Qinghai, Tibet and parts of Xinjiang, Gansu, Sichuan and Yunnan. The major cities include two provincial capitals—Xining and Lhasa, five prefecture–level cities (Haidong, Changdu, Linzhi, Shannan and Shigatse), seven county–level cities (Delingha, Golmud, Yushu, Hezuo, Maerkang, Kangding and Shangrila) and 18 prefecture–level cities within the 100km buffer zone, including Kashi, Jiuquan Sustainability 2019, 11, 589 3 of 16 Sustainability 2019, 11, x FOR PEER REVIEW 3 of 15 andKashi, Chengdu. Jiuquan Thereand Chengdu. are 1972 There township are 1972 administrative township administrative units in the Qinghai–Tibet units in the Qinghai–Tibet Plateau area. ForPlateau maintaining area. For analytical maintaining continuity, analytical changing continuity, administrative changing divisions administrative was not considered divisions during was datanot processingconsidered andduring analysis. data processing and analysis. Figure 1. The location of the study area. 2.2. Data Sources and Processing In this study, thethe Qinghai–Tibet PlateauPlateau areaarea datadata werewere sourcedsourced fromfrom thethe National Earth System Scientific DataData Sharing Sharing Service Service Platform. Platform. Administrative Administrative division division data were data obtained were obtained from the Resourcesfrom the andResources Environment and Environment Science Data Science Center Data of Chinese Center Academy of Chinese of Sciences.Academy The of Sciences. traffic road The network traffic road data werenetwork based data on were the national based on database the national at a 1:25,000 database scale at (Table a 1:25,0001). Vector scale data (Table for transport1). Vector networks data for intransport different networks years were in different
Recommended publications
  • A Study of Thermal History Since the Paleozoic in the Eastern Qaidam Basin, Northwest China
    A Study of Thermal History Since the Paleozoic in the Eastern Qaidam Basin, Northwest China WANG Li 1,2 , LI Zongxing 1,2*, LIU Chenglin3, PENG Bo1,2, FANG Xinxin 1,2, YUAN Guide4 1 The Key Laboratory of Shale Oil and Gas Geological Survey, Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing, China; 2 Institute of Geomechanics,Chinese academy of geological sciences,Beijing 100081, China 3 State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum, Beijing 102249, China; 4 PetroChina Qinghai Oilfield Company, Branch of Petroleum Exploration, Dunhuang, Gansu 736202 Abstract: Qaidam Basin is the one of three major petroliferous basin in Northeastern Tibetan Plateau, which experienced multiphase superimposition and transformation. A study on thermal history not only plays an important role on analysis the tectonic origin of the Qaidam basin, revealing the forming mechanism and uplift history of Tibetan plateau, but also is available to provide scientific evidence on oil & gas resources appraising. Using balanced cross-sections technique, and combination of analysis of apatite fission track ages with modeling of fission track length distribution, it was infered that eastern Qaidam basin experienced significant tectonic movement in the early Jurassic movement (~200 Ma), which caused the carboniferous uplift and denudation, the geological movement in late Cretaceous, characterized by stretch in the early and the northeast-southwest extrusion in late; Himalayan movement in multi-stage development in the eastern Qaidam basin, Mainly divided into the early Himalayan movement (41.1~33.6 Ma) and the late Himalayan movement (9.6~7.1 Ma, 2.9~1.8 Ma), which large-scale orogeny caused pre-existing faults reactivated in late Himalayan movement.
    [Show full text]
  • Xining to Lhasa (Vice Versa)
    TRAIN : Qinghai Tibet Railways JOURNEY : Xining to Lhasa (vice versa) Journey Duration : Upto 2 Days Day to Day Itinerary Unlike trains to Tibet from other gateway cities, the trains from Xining depart several times a day, since all other Tibet trains will stop in Xining before reaching Lhasa. The departure time of Xining Lhasa trains ranges from 12:27 at noon to 21:27 in the evening, offering flexible choices for tourists. Among all the trains to Tibet, there are two trains directly originated from Xining , one numbered as No.Z6801 departing every other day, and the other as No.Z6811 scheduled to run within a seasonal period. Timetable of Direct Xining to Lhasa Train Train No. Z6801 is the only train that starts directly from Xining and ends in Lhasa. It departs every other day at 14:01 from Xining Railway Station and arrives in Lhasa at 11:20 on the next day. Besides, Train No. Z6811 which bounds for Shigatse can also take tourists to Lhasa from Xining. The train from Xining to Shigatse is a seasonal train departing every day. Timetable of Xining to Lhasa Train - No.Z6801 Station Arrival Departure Stop Time Days Distance Xining -- 14:01 -- Day 1 -- Delingha 18:03 18:09 6 min Day 1 521 km Golmud 20:53 21:18 25 min Day 1 830 km Amdo 05:54 05:58 4 min Day 2 1,524 km Nagchu 07:24 07:30 6 min Day 2 1,650 km Damxung 09:06 09:10 4 min Day 2 1,800 km Lhasa 11:20 -- -- Day 2 1,972 km Timetable of Xining to Lhasa Train - No.Z6811 Station Arrival Departure Stop Time Days Distance Xining -- 20:30 -- Day 1 -- Delingha 00:32 00:38 6 min Day 2 521 km Golmud 03:28 03:53 25 min Day 2 830 km Amdo 12:01 12:05 4 min Day 2 1,524 km Nagchu 13:39 13:45 6 min Day 2 1,650 km Damxung 15:39 15:47 8 min Day 2 1,800 km Lhasa 17:45 18:10 25 min Day 2 1,972 km Timetable of Direct Lhasa to Xining Train As the return trip back to mainland China, the train from Lhasa to Xining (No.
    [Show full text]
  • Estimations of Undisturbed Ground Temperatures Using Numerical and Analytical Modeling
    ESTIMATIONS OF UNDISTURBED GROUND TEMPERATURES USING NUMERICAL AND ANALYTICAL MODELING By LU XING Bachelor of Arts/Science in Mechanical Engineering Huazhong University of Science & Technology Wuhan, China 2008 Master of Arts/Science in Mechanical Engineering Oklahoma State University Stillwater, OK, US 2010 Submitted to the Faculty of the Graduate College of the Oklahoma State University in partial fulfillment of the requirements for the Degree of DOCTOR OF PHILOSOPHY December, 2014 ESTIMATIONS OF UNDISTURBED GROUND TEMPERATURES USING NUMERICAL AND ANALYTICAL MODELING Dissertation Approved: Dr. Jeffrey D. Spitler Dissertation Adviser Dr. Daniel E. Fisher Dr. Afshin J. Ghajar Dr. Richard A. Beier ii ACKNOWLEDGEMENTS I would like to thank my advisor, Dr. Jeffrey D. Spitler, who patiently guided me through the hard times and encouraged me to continue in every stage of this study until it was completed. I greatly appreciate all his efforts in making me a more qualified PhD, an independent researcher, a stronger and better person. Also, I would like to devote my sincere thanks to my parents, Hongda Xing and Chune Mei, who have been with me all the time. Their endless support, unconditional love and patience are the biggest reason for all the successes in my life. To all my good friends, colleagues in the US and in China, who talked to me and were with me during the difficult times. I would like to give many thanks to my committee members, Dr. Daniel E. Fisher, Dr. Afshin J. Ghajar and Dr. Richard A. Beier for their suggestions which helped me to improve my research and dissertation.
    [Show full text]
  • A 3585-Year Ring-Width Dating Chronology of Qilian Juniper from the Northeastern Qinghai-Tibetan Plateau
    IAWA Journal, Vol. 30 (4), 2009: 379–394 A 3585-YEAR RING-WIDTH DATING CHRONOLOGY OF QILIAN JUNIPER FROM THE NORTHEASTERN QINGHAI-TIBETAN PLATEAU Xuemei Shao1 *, Shuzhi Wang2, Haifeng Zhu1, Yan Xu1, Eryuan Liang3, Zhi-Yong Yin4, Xinguo Xu5 and Yongming Xiao5 SUMMARY This article documents the development of a precisely dated and well- replicated long regional tree-ring width dating chronology for Qilian juniper (Juniperus przewalskii Kom.) from the northeastern Qinghai- Tibetan Plateau. It involves specimens from 22 archeological sites, 24 living tree sites, and 5 standing snags sites in the eastern and northeastern Qaidam Basin, northwestern China. The specimens were cross-dated suc- cessfully among different groups of samples and among different sites. Based on a total of 1438 series from 713 trees, the chronology covers 3585 years and is the longest chronology by far in China. Comparisons with chronologies of the same tree species about 200 km apart suggest that this chronology can serve for dating purposes in a region larger than the study area. This study demonstrates the great potential of Qilian juniper for dendrochronological research. Key words: Northeastern Qinghai-Tibetan Plateau; Qilian juniper; den- drochronology; cross-dating; 3585-year chronology; archeological wood. INTRODUCTION One of the aims of dendrochronology is to construct long-term chronologies covering hundreds to thousands of years. These chronologies have major applications to climatic interpretations, radiocarbon analysis, and dating of past events (Lara & Villalba 1993; Scuderi 1993; Hughes & Graumlich 1996; Stahle et al. 1998, 2007; Grudd et al. 2002; Helama et al. 2002; Naurzbaev et al. 2002; Friedrich et al. 2004; Bhattacharyya & Shah 2009; Fang et al.
    [Show full text]
  • Sichuan/Gansu/Qinghai/Tibet (14 Days) We Love Road Journeys
    Tibetan Highlands: Sichuan/Gansu/Qinghai/Tibet (14 Days) We love road journeys. They are by far our favourite way of traveling. We think the world of western China and the countries that border on this region – think Vietnam, Lao, Thailand, Myanmar, for example. On the Road Experiences is all about sharing with like-minded travelers just how beautiful a road journey in these varied lands can be. Now turn the page to find out what we’ve come to love so much… p2 p3 Itinerary Map …where you will travel… p. 006 Yes, it is possible… p. 008 Journey of Discovery… p. 010 Day-by-day… p. 056 In closing... Any car you like, so long as it is an SUV… p. 077 Adventures and discoveries in local cuisines p. 078 What’s included/Best Months to Go... p. 080 Photo credits p. 083 p5 Itinerary Map Day1 Day8 Arrival in Chengdu – Dulan to Golmud – Apply for your temporary driving Across the Qaidam Basin to Golmud license and visit Chengdu’s beautiful Panda Reserve Day9 Golmud to Tuotuohe – Day2 Up, up, up - Onto the Plateau and Chengdu to Maerkang – into the highlands of Qinghai Through the valleys to the Gyarong Tibetan region Day10 Tuotuohe to Naqu – Day3 Cross the famous Tanggula Pass on Maerkang to Ruoergai – your way to Tibet itself Towards the very north of Sichuan on the way to Gansu Day11 Naqu to Damxung – Day4 Visit one of Tibet’s holiest lakes, Ruoergai to Xiahe – Lake Nam-tso Your first and only stop in Gansu province Day12 Damxung to Lhasa – Day5 Complete your journey with Xiahe to Qinghai’s capital, Xining – a beautiful drive to your final On your way to Qinghai destination Day6 Day13 Xining – In and around Lhasa – Spend a day in and around Xining for Visit Potala Palace and explore the a bit of rest and visit the spectacular old city of Lhasa Ta’er Monastery Day14 Day7 Depart from Lhasa – Xining to Dulan – Lift must go on...Farewell Lhasa On the way to Golmud..
    [Show full text]
  • Qinghai WLAN Area 1/13
    Qinghai WLAN area NO. SSID Location_Name Location_Type Location_Address City Province 1 ChinaNet Quality Supervision Mansion Business Building No.31 Xiguan Street Xining City Qinghai Province No.160 Yellow River Road 2 ChinaNet Victory Hotel Conference Center Convention Center Xining City Qinghai Province 3 ChinaNet Shangpin Space Recreation Bar No.16-36 Xiguan Street Xining City Qinghai Province 4 ChinaNet Business Building No.372 Qilian Road Xining City Qinghai Province Salt Mansion 5 ChinaNet Yatai Trade City Large Shopping Mall Dongguan Street Xining City Qinghai Province 6 ChinaNet Gome Large Shopping Mall No.72 Dongguan Street Xining City Qinghai Province 7 ChinaNet West Airport Office Building Business Building No.32 Bayi Road Xining City Qinghai Province Government Agencies 8 ChinaNet Chengdong District Government Xining City Qinghai Province and Other Institutions Delingha Road 9 ChinaNet Junjiao Mansion Business Building Xining City Qinghai Province Bayi Road Government Agencies 10 ChinaNet Higher Procuratortate Office Building Xining City Qinghai Province and Other Institutions Wusi West Road 11 ChinaNet Zijin Garden Business Building No.41, Wusi West Road Xining City Qinghai Province 12 ChinaNet Qingbai Shopping Mall Large Shopping Mall Xining City Qinghai Province No.39, Wusi Avenue 13 ChinaNet CYTS Mansion Business Building No.55-1 Shengli Road Xining City Qinghai Province 14 ChinaNet Chenxiong Mansion Business Building No.15 Shengli Road Xining City Qinghai Province 15 ChinaNet Platform Bridge Shoes City Large Shopping
    [Show full text]
  • Tibet Outside the TAR Page 2159
    CFP-W, Chentsa Chinese: Jianza Xian Alliance for Research in Tibet (ART) Tibet Outside the TAR page 2159 roll/neg: 54:15 subject: wide angle view of the town location: Chentsa Dzong CFP-W-éE,, Malho -é, Tibetan Autonomous Prefecture, Tsongön UWê-¢éP, [Ch: Jianza , Huangnan TAP, Qinghai Province] approx. date: winter 1995/1996 comment: In the distance is the Machu (Huanghe, Yellow R.). Across the river is Haidong Prefecture with two million inhabitants, at least two thirds of them Chinese and Hui. Official population in Chentsa is about 49,000, with a 60% Tibetan majority claimed. The true Tibetan proportion is probably lower. Demographic pressure is intense: population density in Chentsa, the nearest to Xining and Haidong, is 28 persons/km2 . The next county, the capital, Regong, has 21. In Tsekhog it is 7 and only 4 in Yülgan. (Viewed from the south.) © 1997 Alliance for Research in Tibet (ART), all rights reserved Alliance for Research in Tibet (ART) Tibet Outside the TAR page 2161 b. Chentsa [Ch: Jianza] i. Brief description and impressions Chentsa CFP-W-éE, (Ch. Jianza Xian ) is one of the most vulnerable of all the Tibetan counties to patterns of development preferred by China. Only the Yellow River (Ma Chu), edging its northern border, now divides it from the densely-populated Chinese and Hui region of Haidong Prefecture. This geographical feature once served as a clear and formidable marker between a totally Tibetan world to the south and a region which, though sinicizing gradually over the centuries, did not overleap the Yellow River until the Communist Chinese occupation.
    [Show full text]
  • Mapping and Evaluating Human Pressure Changes in the Qilian Mountains
    remote sensing Article Mapping and Evaluating Human Pressure Changes in the Qilian Mountains Quntao Duan 1,2 , Lihui Luo 1,2,* , Wenzhi Zhao 1,2,3, Yanli Zhuang 1,3 and Fang Liu 1,2 1 Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China; [email protected] (Q.D.); [email protected] (W.Z.); [email protected] (Y.Z.); [email protected] (F.L.) 2 University of Chinese Academy of Sciences, Beijing 100049, China 3 Linze Inland River Basin Research Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China * Correspondence: [email protected] Abstract: Human activities have dramatically changed ecosystems. As an irreplaceable ecological barrier in western China, the Qilian Mountains (QLM) provide various ecosystem services for humans. To evaluate the changes in the intensity of human activities in the QLM and their impact on the ecosystem, the human footprint (HF) method was used to conduct a spatial dataset of human activity intensity. In our study, the NDVI was used to characterize the growth of vegetation, and six categories of human pressures were employed to create the HF map in the QLM for 2000–2015 at a 1-km scale. The results showed that the mean NDVI during the growing season showed a significant increasing trend over the entire QLM in the period 2000–2015, while the NDVI showed a significant declining trend of more than 70% concentrated in Qinghai. Human pressure throughout the QLM occurred at a low level during 2000–2015, being greater in the eastern region than the western region, while the Qinghai area had greater human pressure than the Gansu area.
    [Show full text]
  • Research Article the Carboniferous Arc of the North Pamir
    GeoScienceWorld Lithosphere Volume 2021, Article ID 6697858, 26 pages https://doi.org/10.2113/2021/6697858 Research Article The Carboniferous Arc of the North Pamir 1 1 2 3 4 Johannes Rembe , Edward R. Sobel , Jonas Kley , Renjie Zhou , Rasmus Thiede , 5 and Jie Chen 1Institute of Geosciences, University of Potsdam, 14476 Golm Potsdam, Germany 2Department of Structural Geology and Geodynamics, Georg-August-Universität Göttingen, 37077 Göttingen, Germany 3School of Earth and Environmental Sciences, The University of Queensland, St. Lucia QLD 4072, Australia 4Institute for Geosciences, Christian-Albrechts-Universität Kiel, 24118 Kiel, Germany 5State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, X9GJ+RV Chaoyang, Beijing, China Correspondence should be addressed to Johannes Rembe; [email protected] Received 28 October 2020; Accepted 7 January 2021; Published 8 February 2021 Academic Editor: Pierre Valla Copyright © 2021 Johannes Rembe et al. Exclusive Licensee GeoScienceWorld. Distributed under a Creative Commons Attribution License (CC BY 4.0). In this study, we investigate the age and geochemical variability of volcanic arc rocks found in the Chinese, Kyrgyz, and Tajik North Pamir in Central Asia. New geochemical and geochronological data together with compiled data from the literature give a holistic view of an early to mid-Carboniferous intraoceanic arc preserved in the northeastern Pamir. This North Pamir volcanic arc complex involves continental slivers in its western reaches and transforms into a Cordilleran-style collision zone with arc- magmatic rocks. These are hosted in part by Devonian to Carboniferous oceanic crust and the metamorphic Kurguvad basement block of Ediacaran age (maximum deposition age) in Tajikistan.
    [Show full text]
  • The Thickness and Structural Characteristics of the Crust Across Tibetan Plateau from Active-Sources Seismic Profiles∗
    Earthq Sci (2009)22: 21−31 21 Doi: 10.1007/s11589-009-0021-6 The thickness and structural characteristics of the crust across Tibetan plateau from ∗ active-sources seismic profiles Qiusheng Li 1,2, Rui Gao 1,2 Zhanwu Lu 1,2 Ye Guan 1,2 Jisheng Zhang 1,2 Pengwu Li 1,2 Haiyan Wang 1,2 Rizheng He 1,2 and Marianne Karplus3 1 Lithosphere Research Center, Institute of Geology, Chinese Academy of Geology Science,Beijing 100037, China 2 Earthprobe and Geodynamics Open Laboratory of Chinese Academy of Geology Science, Beijing 100037, China 3 Crustal Geophysics Group, Stanford University, Stanford CA 94305, USA Abstract The Tibetan plateau as one of the youngest orogen on the Earth was considered as the result of conti- nent-continent collision between the Eurasian and Indian plates. The thickness and structure of the crust beneath Tibetan pla- teau is essential to understand deformation behavior of the plateau. Active-source seismic profiling is most available geo- physical method for imaging the structure of the continental crust. The results from more than 25 active-sources seismic pro- files carried out in the past twenty years were reviewed in this article. A preliminary cross crustal pattern of the Tibetan Pla- teau was presented and discussed. The Moho discontinuity buries at the range of 60−80 km on average and have steep ramps located roughly beneath the sutures that are compatible with the successive stacking/accretion of the former Cenozoic blocks northeastward. The deepest Moho (near 80 km) appears closely near IYS and the crustal scale thrust system beneath southern margin of Tibetan plateau suggests strong dependence on collision and non-distributed deformation there.
    [Show full text]
  • Studies on Ethnic Groups in China
    Kolas&Thowsen, Margins 1/4/05 4:10 PM Page i studies on ethnic groups in china Stevan Harrell, Editor Kolas&Thowsen, Margins 1/4/05 4:10 PM Page ii studies on ethnic groups in china Cultural Encounters on China’s Ethnic Frontiers Edited by Stevan Harrell Guest People: Hakka Identity in China and Abroad Edited by Nicole Constable Familiar Strangers: A History of Muslims in Northwest China Jonathan N. Lipman Lessons in Being Chinese: Minority Education and Ethnic Identity in Southwest China Mette Halskov Hansen Manchus and Han: Ethnic Relations and Political Power in Late Qing and Early Republican China, 1861–1928 Edward J. M. Rhoads Ways of Being Ethnic in Southwest China Stevan Harrell Governing China’s Multiethnic Frontiers Edited by Morris Rossabi On the Margins of Tibet: Cultural Survival on the Sino-Tibetan Frontier Åshild Kolås and Monika P. Thowsen Kolas&Thowsen, Margins 1/4/05 4:10 PM Page iii ON THE MARGINS OF TIBET Cultural Survival on the Sino-Tibetan Frontier Åshild Kolås and Monika P. Thowsen UNIVERSITY OF WASHINGTON PRESS Seattle and London Kolas&Thowsen, Margins 1/7/05 12:47 PM Page iv this publication was supported in part by the donald r. ellegood international publications endowment. Copyright © 2005 by the University of Washington Press Printed in United States of America Designed by Pamela Canell 12 11 10 09 08 07 06 05 5 4 3 2 1 All rights reserved. No part of this publication may be repro- duced or transmitted in any form or by any means, electronic or mechanical, including photocopy, recording, or any infor- mation storage or retrieval system, without permission in writ- ing from the publisher.
    [Show full text]
  • Himalayan Journal of Sciences Vol 2 Issue 4 (Special Issue) July 2004
    EXTENDED ABSTRACTS: 19TH HIMALAYA-KARAKORAM-TIBET WORKSHOP, 2004, NISEKO, JAPAN Northeastward growth and uplift of the Tibetan Plateau: Tectonic- sedimentary evolution insights from Cenozoic Hoh Xil, Qaidam and Hexi Corridor basins Chengshan Wang†‡*, Zhifei Liu§ and Lidong Zhu† † State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, CHINA ‡ China Univesity of Geosciences, Beijing 100083, CHINA § Laboratory of Marine Geology, Tongji University, Shanghai 200092, CHINA * To whom correspondence should be addressed. E-mail: [email protected] .................................................................................................................................................................................................................................................................... The northeastward growth of the Tibetan Plateau was addressed distributed clastic sediments. The Hexi Corridor Basin was as a major uplift process of Northeast Tibet, deduced mainly from formed under the Altyn Tagh Fault activity as a strike-slip basin the Qaidam, Gonghe-Guide, and Hexi Corridor basins (Métivier started from 37.7 Ma. During 30.3-0.13 Ma period, with the et al. 1998; Pares et al. 2003). These studies contributed to a movement of the Qilian orogen, the basin depocenter shifted significant in understanding of the crustal thickening and oblique southwards to the mountain edge that indicates the formation stepwise rise of Plio-Quaternary Tibet (Meyer et al. 1998; of a foreland basin. From 0.13 Ma, the basin has evolved into an Tapponnier et al. 2001). But sedimentary basins in central Tibet intermontane basin with a less than 100 m thick sediments. still remain less studied because of harsh conditions for fieldwork. The three Cenozoic sedimentary basins have a similar The Hoh Xil Basin, as the largest Cenozoic sedimentary basin in tectonic-sedimentary history, i.e.
    [Show full text]