DOCSLIB.ORG

(G219), Kashgar - Ali © Stephan Rankl, 2006

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
(G219), Kashgar - Ali © Stephan Rankl, 2006 Westtibet-Highway (G219), Kashgar - Ali © Stephan Rankl, 2006 Hinweise: Kilometer: Gesamt steht für die Gesamtentfernung, Tag für die unsere Tagesleistung (bin da ganz egoistisch ;-), mit Relativ sind die Abstände den Angaben gemeint. Tagesleistung: Darunter ist immer unsere Fahrzeit in Stunden, sowie die Durchschnittsgeschwindigkeit in km/h angegeben. Wasser: Soll für euch eine Hilfestellung sein, wo es Wasser gibt und wie es zwischen den Städten aussieht. Durchgängig blau bedeutet keine Probleme. GPS: GPS-Koordinaten eigene Messung - Angaben ohne Gewähr (Datum: WGS 84 Positionsformat: Dezimal). In den Städten hab ich die Messung meist beim Hotel gemacht, also wer hier den Koordinaten folgt wird eine schöne Bleibe für die Nacht finden ... ;-) Sicher werdet ihr euch fragen, in wieweit unsere Camps von Interesse sind, aber dort gibt es meist Wasser in der Nähe! Höhe: Von mir selbst mit GPS ermittelt, in der Regel gute Genauigkeit, hin und wieder Messung mit Barometer (gekennzeichnet ). Kilometer Beschreibung Hotel Verpflegung Wasser GPS-Koord. Höhe Kommentar Gesamt Tag Relativ Kashgar ok Rest. / Shop N 39,47057° 1304 m Alles was das Herz begehrt! E 75,96719° Radler-Treffpunkt: Seman-Hotel. Alles nötige hier besorgen, insbesondere Snacks (Schoki), Müsli und Grundsätzliches (Zucker, Tee, Kaffee) 0 0 0 Start An der großen Kreuzung wo es von Westen kommend, gerade zur Mao-Statue gehen würde und links zur Moschee, Asphalt hier nach rechts radeln. Ab in den Süden, westlich am People's Park vorbei. Auf der Straße (Highway 315) bleiben, nicht von Schildern verwirren lassen. 50 50 Ort Shop viele Läden und Straßenstände, ab jetzt Oasenhopping 70 20 Yingsar Rest. / Shop großer Messerbazaar, Wasser nachfüllen! kurz nach Yingsar ein Stausee 94 94 24 Camp N 38,75761° 1420 m Camp in der Wüste, kein Wasser F=5,40h 1. Tag E 76,27282° ø=16,5 114 20 Qizil Bazaar Shop 1300 m vor Qizil mehrere kleine Bäche vom Pamir runter (abh. von der Jahreszeit) großer Markt in Qizil 120 6 Kleiner Ort Shop Hier gibt es nochmal Gelegenheit, seine Wasser-Vorräte aufzu- füllen, danach bis Qarak Wüste. 174 54 Qarak Shop großer Bazaar, ab jetzt wird es wieder grüner, aber auch belebter 197,5 103,5 23,5 Yarkand ok Rest. / Shop N 38,41513° 1235 m Große Stadt mit allem was man so braucht. F=6,21h 2. Tag E 77,24500° Vor der Stadt gabelt sich die Straße, nach links radeln. Vor ø=16,3 einer Kreuzung auf der linken Seite ein Hotel. Gute Uiguren- Restaurants an der Kreuzung links die Straße hoch. 225,5 28 Stadt Shop In Yarkand an der Kreuzung nach Süden, bis es nicht mehr geht, dann links. 251,5 26 Bazaar Shop 261,5 10 Karghilik / ok Rest. / Shop Hotel: Straße macht eine Kurve nach links, es geht den Berg Yecheng hoch. Erste Abzweigung nach rechts. Die Straße runter zum Hotel. Letzte Möglichkeit, um seine Vorräte gut aufzufüllen. Danach wird das Angebot begrenzt. 267,5 ~6 Turn-Off Nach der ersten Abzweigung, den Hügel wieder runter, dann rechts. Beim Abzw. auf Kilometerstein null der G219 achten. 273,5 76 ~6 Camp N 37,81835° 1410 m Camp neben einer Müllhalde, aber mit fließend Wasser F=? 3. Tag E 77,44911° (dreckig). Früher mal war es nicht so gut, in Karghilik ins ø=? Hotel zu gehen, wg. PSB. Aber die Zeiten sind wohl vorbei. Kilometer Beschreibung Hotel Verpflegung Wasser GPS-Koord. Höhe Kommentar Gesamt Tag Relativ 282 8,5 Brücke Fluß 292,5 10,5 Road Repair Road Repair Station. Kein Army-Camp, wie anderswo Station geschrieben. Man kann hier also auch bei Tag vorbeiradeln! 322,5 30 Dörfer Asphalt 329,5 7 Ort Shop 339,5 10 Pusha Rest. / Shop 340,5 67 1 Camp N 37,30809° 2164 m Hinter Pusha gute Camp-Möglichkeiten an einem Bach. F=5,36h 4. Tag E 77,14405° ø=12,0 361,5 21 Ende von Teer Bach 2450 m Schotterpiste beginnt 368,5 7 Akmeqit N 37,10987° 2695 m E 77,00824° 380,5 12 Kudi La N 37,08922° 3296 m 5 Km vor und hinter dem Pass kein Wasser, ansonsten immer 1. Pass E 76,93349° am Bach entlang. Glückwunsch, 1. Pass (leider der niedrigste)! 390 49,5 9,5 Camp N 37,08390° 2839 m Camp an einer der vielen Serpentinen F=6,13h 5. Tag E 76,91422° Wasser nicht ganz so dreckig, wie in den Tälern. ø=7,9 Gute Schotterpiste 396 6 Road Repair S. Fluß 2500 m Straße entlang des großen Flußes (dreckig) 400 4 Army Camp 2500 m Vorsicht, Hund! 403 3 Teer! Ab Kilometerstein 133 Straße wieder asphaltiert 410 7 Klares Wasser Ausschau halten! Immer wieder Tümpel mit klarem Wasser! 416 6 Klares Wasser Noch ein Tümpel mit klarem Wasser. 430 14 Kudi ok Rest. / Shop N 36,84161° 2877 m Nach Kudi Army-Checkpoint. Pässe werden registriert. Asphalt E 76,98151° In der Kaserne dahinter hat es zwei bei Radlern schon recht berüchtigte Hunde! 433,5 43,5 3,5 Camp N 36,82261° 3018 m Beim Camp klares Wasser aus einem Seitental. F=3,58h 6. Tag E 76,99455° ø=11 464 30,5 30,5 Camp N 36,63282° 3950 m Jetzt geht es hoch hinaus! Darum lieber etwas langsamer und F=4,26h 7. Tag E 77,14308° dem Körper Zeit geben, sich an die Höhe anzupassen! ø=6,8 468 4 Ende von Teer Bach 4100 m Altes Haus und Brücke r Piste ganz passabel. Ab und zu grober, loser Schotter. 480 12 Road Repair S. 4550 m Evtl. gibt es hier was zu essen. 491 11 Chiragsaldi La N 36,57892° 4990 m Der derbste Pass von allen! Ab jetzt gibt es kein Zurück mehr Schotte 2. Pass E 77,00325° in Sachen Höhe! Am Pass oben gibt’s kein Wasser. Kilometer Beschreibung Hotel Verpflegung Wasser GPS-Koord. Höhe Kommentar Gesamt Tag Relativ 515 51 24 Mazaar ok Rest. / Shop Fluß N 36,44554° 3811 m Welcome to Bretterbuden-City! Toiletten, hinter den Buden F=6,22h 8. Tag E 77,00552° einen Stein suchen. Über einer Bude hängt ein Welcome!- ø=8,0 Schild. Dort kann man im Dormitory übernachten. Einen kl. Shop hat es auch. Links geht es weiter nach Ali. Rechts zum K2-Basecamp. Army-Base hinter der Stadt. 528 13 Truckstop Restaurant? Sah geschlossen aus, andere haben hier schon übernachtet. Schotterpiste 545,5 30,5 17,5 Camp N 36,45544° 3971 m Piste: Waschbrett mit Schuttauflage. F=3,45h 9. Tag E 77,30690° Es geht immer an einem Fluß entlang. ø=8,1 563,5 18 Road Repair S. 4000 m Vorsicht Hund! Waschbret 566,5 3 Beginn Pass Bach Flache Serpentinen, gute Piste 584,5 18 Kekeate La N 36,43082° 4948 m Ein Schild verkündet 4930m 3. Pass E 77,57814° 600,5 55 16 Camp N 36,41570° 4432 m Verfallene Road Repair Station F=6,58h 10. Tag E 77,71680° Gute Piste ø=7,9 615,5 15 Brücke 3950 m Brücke + Road Repair Station 630,5 15 Alte Festung Fluß 3700 m Links am Hügel oben, Bach dazwischen. 634 3,5 Ruinen 3700 m Piste: Waschbrett mit viel Sand 643,5 9,5 Xaidulla ok Rest. / Shop N 36,34886° 3672 m Großes Armee-Basis. Sehr gut versorgte kleine Läden. E 78,03256° Übernachten evtl. in Dormitories 646,5 46 3 Camp N 36,33148° 3695 m Schönes Camp zw. Büschen nach dem Hügel hinter Xaidulla. F=3,53h 11. Tag E 78,07989° ø=11,8 663,5 17 Army-Camp Neues Army-Camp, Hunde! 664,5 1 Abzweigung Neuer Abzw. nach rechts, G219 gerade aus 682,5 18 Abzweigung 3850 m G219 gerade aus 690 43,5 7,5 Camp N 36,23987° 3876 m Camp am Beginn des nächsten Passes F=4,59h 12. Tag E 78,51064° Waschbrett + Sand + Schutt ø=8,7 692 2 Abzweigung Links Army-Camp, gerade G219 693 1 Abzweigung Links nochmal zur PLA. Brücke, letztes Wasser vor Pass 704 11 Kangxiwar La N 36,21969° 4287 m Piste den Pass hoch ganz gut, runter dann sehr viel Schutt 4. Pass E 78,65340° 713 9 Wasser Wasser in der Nähe 714 1 Denkmal links Denkmal, rechts Ruinen -> Kangxiwar? 715 1 Ende Passabf. 4000 m Ende der Passabfahrt 731 16 Brücke 4080 m Brücke, nicht direkt Wasser in der Nähe Kilometer Beschreibung Hotel Verpflegung Wasser GPS-Koord. Höhe Kommentar Gesamt Tag Relativ 743 53 12 Camp N 36,10213° 4119 m Camp bei Ruinen F=6,16h 13. Tag E 79,00562° ø=8,5 766 23 Dahongliutan ok Rest. / Shop N 35,98137° 4222 m Hier mit Essbaren eindecken. Danach geht es auf das Aksai E 79,18913° Chin. Erst in Tielong gibt es wieder Nachschub (ca. 200km)! 788,5 45,5 22,5 Camp N 35,87047° 4566 m F=5,31h 14. Tag E 79,36311° ø=8,2 791,5 3 Brücke Road Repair Station + Brücke, ersten 6km sehr steil! 816,5 25 Qitai La N 35,68476° 5187 m Aksai Chin voraus! Auf dem Plateau nur einzelne Wasser- 5. Pass E 79,49309° stellen, keine Flüsse oder Bäche! 824,5 36 8 Camp Quelle N 35,62719° 4910 m Quelle bei einem Hügel, vorher lange Zeit nix F=4,38h 15. Tag E 79,51817° ø=7,8 840 15,5 Lagune 4700 m Große Süßwasser-Lagune 859,5 19,5 Tianshuihai N 35,35697° 4846 m Road Repair Station, Militär-Basis, nix zu kaufen E 79,53752° 886,5 62 27 Camp N 35,13491° 4900 m Zelt bei einem kleinen Wasserloch aufgestellt F=5,38h 16.
Load more

Recommended publications
  • Chemical Evolution of Nb-Ta Oxides and Cassiterite in Phosphorus-Rich
    minerals Article Chemical Evolution of Nb-Ta Oxides and Cassiterite in Phosphorus-Rich Albite-Spodumene Pegmatites in the Kangxiwa–Dahongliutan Pegmatite Field, Western Kunlun Orogen, China Yonggang Feng 1,2,* , Ting Liang 1,2,*, Xiuqing Yang 1,2, Ze Zhang 1,2 and Yiqian Wang 1,2 1 School of Earth Science and Resources, Chang’an University, Xi’an 710054, China; [email protected] (X.Y.); [email protected] (Z.Z.); [email protected] (Y.W.) 2 Laboratory of Mineralization and Dynamics, Chang’an University, Xi’an 710054, China * Correspondence: [email protected] (Y.F.); [email protected] (T.L.) Received: 30 January 2019; Accepted: 2 March 2019; Published: 8 March 2019 Abstract: The Kangxiwa–Dahongliutan pegmatite field in the Western Kunlun Orogen, China contains numerous granitic pegmatites around a large granitic pluton (the Dahongliutan Granite with an age of ca. 220 to 217 Ma), mainly including barren garnet-, tourmaline-bearing pegmatites, Be-rich beryl-muscovite pegmatites, and Li-, P-rich albite-spodumene pegmatites. The textures, major element contents, and trace element concentrations of columbite-group minerals (CGM) and cassiterite from three albite-spodumene pegmatites in the region were investigated using a combination of optical microscopy, SEM, EPMA and LA-ICP-MS. The CGM can be broadly classified into four types: (1) inclusions in cassiterite; (2) euhedral to subhedral crystals (commonly exhibiting oscillatory and/or sector zoning and coexisting with magmatic cassiterite); (3) anhedral aggregates; (4) tantalite-(Fe)-ferrowodginite (FeSnTa2O8) intergrowths. The compositional variations of CGM and cassiterite are investigated on the mineral scale, in individual pegmatites and within the pegmatite group.
    [Show full text]
  • Co-Seismic and Cumulative Offsets of the Recent Earthquakes Along The
    Co-seismic and cumulative offsets of the recent earthquakes along the Karakax left-lateral strike-slip fault in western Tibet Haibing Li, Jerome van der Woerd, Zhiming Sun, Jialiang Si, Paul Tapponnier, Jiawei Pan, Dongliang Liu, Marie-Luce Chevalier To cite this version: Haibing Li, Jerome van der Woerd, Zhiming Sun, Jialiang Si, Paul Tapponnier, et al.. Co-seismic and cumulative offsets of the recent earthquakes along the Karakax left-lateral strike-slip fault inwestern Tibet. Gondwana Research, Elsevier, 2011, 21, pp.64-87. 10.1016/j.gr.2011.07.025. hal-00683742 HAL Id: hal-00683742 https://hal.archives-ouvertes.fr/hal-00683742 Submitted on 29 Mar 2012 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. ACCEPTED MANUSCRIPT Co-seismic and cumulative offsets of the recent earthquakes along the Karakax left-lateral strike-slip fault in western Tibet Haibing Li a,b,*, Jérôme Van der Woerd c, Zhiming Sun d, Jialiang Si a,b, Paul Tapponniere,f, Jiawei Pan a,b, Dongliang Liu a,b, Marie-Luce Chevaliera,b a State Key Laboratory of Continental Tectonic and Dynamics b Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, P.R.
    [Show full text]
  • The 2015 Ms 6.5 Pishan Earthquake, Northwest Tibetan Plateau: a Folding Event in the Western Kunlun Piedmont
    Research Paper GEOSPHERE The 2015 Ms 6.5 Pishan earthquake, Northwest Tibetan Plateau: A folding event in the western Kunlun piedmont 1,2 2 2 2 2 2 2 GEOSPHERE, v. 15, no. 3 Chuanyong Wu , Jianming Liu , Jin Li , Weihua Hu , Guodong Wu , Xiangde Chang , and Yuan Yao 1Guangdong Provincial Key Laboratory of Geodynamics and Geohazards, School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou, China 2Earthquake Agency of Xinjiang Uygur Autonomous Region, Urumqi, China https://doi.org/10.1130/GES02063.1 7 figures; 2 tables ■ ABSTRACT investigate whether the Pishan earthquake generated a surface fault and what the deformation characteristics of this event are. The surface rupture caused CORRESPONDENCE: [email protected] Folding earthquakes are a popular area of research in convergent orogenic by an earthquake can provide a unique opportunity to investigate the impact of belts because they can cause destruction without an obvious surface offset. coseismic faulting on landscape evolution and to refine regional deformation CITATION: Wu, C.Y., Liu, J.M., Li, J., Hu, W.H., Wu, G.D., Chang, X.D., and Yao, Y., The 2015 Ms 6.5 Pishan The Ms 6.5 Pishan earthquake (Ms represents Richter magnitude scale), which models (Wallace, 1977; Yeats et al., 1997; Bull, 2009). The tectonic deformation earthquake, Northwest Tibetan Plateau: A folding event occurred in the western Kunlun piedmont, Northwest Tibetan Plateau, caused and uplift of the Tibetan Plateau have been popular areas of research. Two in the western Kunlun piedmont: Geosphere, v. 15, no. 3, significant property losses. Based on surface deformation data combined main models of upper crustal shortening and faulting (e.g., Tapponnier et al., p.
    [Show full text]
  • CD De La Semaine 27
    Semaine 27– 9 juillet 2021 CD de la Semaine 27 JC & Dom Ein Schweizer kämpft für Julian Assange - Nils Melzer wehrt sich gegen westliche Justizwillkür (NZZ) Kompromisse sind nicht seine Sache (NZZ) « Der Schweizer Jurist Nils Melzer, der Uno-Experte für Folter, geht vor allem gegen westliche Staaten vor: «Jeder weiss, dass Schweden und Grossbritannien Assange wegen seiner Wikileaks- Tätigkeit verfolgen und nicht wegen irgendwelcher Sexualdelikte.» Nils Melzer (Uno-Sonderberichterstatter für Folter) » Le juriste suisse Nils Melzer défend Julian Assange, l’homme des Wikileaks contre l’arbitraire judi- ciaire occidental qui n’a rien à envier à l’arbitraire syrien ou iranien, c’est écrit dans les articles. Afin de le maintenir éternellement dans sa prison à l’isolement de Londres dans laquelle il est torturé psychiquement, ils inventent toutes sortes d’histoires avec fausses preuves. La journaliste Katharina Fontana ne mâche pas ses mots. Tout le monde sait qu’on lui reproche d’avoir dit la vérité et qu’il faut le maltraiter suffisamment pour qu’il ne puisse plus dire la vérité et que ça serve d’exemple pour ceux qui voudraient faire pareil derrière lui. Julian Assange ist ein wenig glaubwürdiges Opfer einer grossen Verschwörung (NZZ) « Die Autorin ist Direktorin der Abteilung Strafrecht am Max-Planck-Institut für ausländisches und internationales Strafrecht in Freiburg im Breisgau sowie Professorin an der Humboldt-Universität Berlin. » Madame la professeure est payée pour enfoncer Julian Assange et Nils Melzer. Donc c’est intéressant de lui donner la parole pour voir comment elle s’y prend. Pour la réfuter, il faut toujours paraphraser Saint-Paul : la loi est l’aiguillon du péché.
    [Show full text]
  • Age and Origin of High Ba–Sr Appinite–Granites at the Northwestern
    Available online at www.sciencedirect.com Gondwana Research 13 (2008) 126–138 www.elsevier.com/locate/gr Age and origin of high Ba–Sr appinite–granites at the northwestern margin of the Tibet Plateau: Implications for early Paleozoic tectonic evolution of the Western Kunlun orogenic belt ⁎ Hai-Min Ye a, Xian-Hua Li b, Zheng-Xiang Li c, Chuan-Lin Zhang a, a Nanjing Institute of Geology and Mineral Resources, China Geological Survey, Nanjing 210016, China b Key Laboratory of Isotope Geochronology and Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China c Institute of Geoscience Research (TIGeR), Department of Applied Geology, Curtin University of Technology, GPO Box U1987, Perth WA 6845, Australia Received 10 May 2007; received in revised form 3 August 2007; accepted 5 August 2007 Available online 7 September 2007 Abstract The Buya appinite–granite is a typical high Ba–Sr granite emplaced at the northern West Kunlun orogenic belt along the northwestern margin of the Tibetan Plateau. The granite is dated at ca. 430 Ma using the SHRIMP U–Pb zircon method. It consists of alkaline feldspar granites with coeval appinite enclaves. The granite possesses high SiO2 (69.77–72.69%), K2O (4.44–5.10%) and total alkalinity (K2O+Na2O=8.80–9.92%), Sr (655–1100 ppm), Ba (1036–1433 ppm) and LREE, and low HREE and HFSE contents and insignificant negative Eu anomalies. Consequently, # the samples have very high Sr/Y (74–141) and (La/Yb)N (37–96) ratios. On the other hand, they have low MgO (or Mg ), Cr and Ni contents and low radiogenic Nd isotopes (ɛNd(T)=−8.4 to −10.4).
    [Show full text]
  • 493-495 Baiping.P65
    Synopsis Sustainably Managing Montane Forests in Arid Mountain Regions: The Oytag Valley of West Kunlun The Oytag valley, about 100 km west of Kashi (Kashgar), is one of the few valleys with forests in the Kunlun Mountains. It underwent severe forest destruction in the late 1950s, and about only one fourth of the natural forest remains. Since the early 1980s, forest conservation and artificial regeneration have been carried out in the valley. In arid mountain regions, forests only de- such as stabilizing highland/lowland hy- velop on slopes with a relatively humid drological system, reducing natural disas- climate, and usually a limited area. To the ters, ensuring oases development down- local people, these forests are rare re- stream, etc. Consequently, sustainably sources and of special value. The ecology managing these mountain forests looms of these forests is often very fragile. It is especially large in northwestern arid very difficult or even impossible for these China. forests to recover if they are seriously de- The Kunlun Mountain range, lies be- stroyed. As a result, sustainably manag- tween the world famous Tibetan Plateau ing these forests is important for the lo- and the low-lying Tarim Basin, and is one cal and downstream people and environ- of the most extensive extremely high and ment. In the vast northwestern arid China, arid mountain ranges in the world. It is desert landscape dominates, and extensive characterized by an arid climate and desert arid mountain areas (e.g. the Kunlun, landscape (1). The annual rainfall is 61.3 Tianshan, Qilian, etc.) and deserts (e.g.
    [Show full text]
  • The 2015 Ms 6.5 Pishan Earthquake, Northwest Tibetan Plateau: a Folding Event in the Western Kunlun Piedmont
    Research Paper GEOSPHERE The 2015 Ms 6.5 Pishan earthquake, Northwest Tibetan Plateau: A folding event in the western Kunlun piedmont 1,2 2 2 2 2 2 2 GEOSPHERE, v. 15, no. 3 Chuanyong Wu , Jianming Liu , Jin Li , Weihua Hu , Guodong Wu , Xiangde Chang , and Yuan Yao 1Guangdong Provincial Key Laboratory of Geodynamics and Geohazards, School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou, China 2Earthquake Agency of Xinjiang Uygur Autonomous Region, Urumqi, China https://doi.org/10.1130/GES02063.1 7 figures; 2 tables ■ ABSTRACT investigate whether the Pishan earthquake generated a surface fault and what the deformation characteristics of this event are. The surface rupture caused CORRESPONDENCE: [email protected] Folding earthquakes are a popular area of research in convergent orogenic by an earthquake can provide a unique opportunity to investigate the impact of belts because they can cause destruction without an obvious surface offset. coseismic faulting on landscape evolution and to refine regional deformation CITATION: Wu, C.Y., Liu, J.M., Li, J., Hu, W.H., Wu, G.D., Chang, X.D., and Yao, Y., The 2015 Ms 6.5 Pishan The Ms 6.5 Pishan earthquake (Ms represents Richter magnitude scale), which models (Wallace, 1977; Yeats et al., 1997; Bull, 2009). The tectonic deformation earthquake, Northwest Tibetan Plateau: A folding event occurred in the western Kunlun piedmont, Northwest Tibetan Plateau, caused and uplift of the Tibetan Plateau have been popular areas of research. Two in the western Kunlun piedmont: Geosphere, v. 15, no. 3, significant property losses. Based on surface deformation data combined main models of upper crustal shortening and faulting (e.g., Tapponnier et al., p.
    [Show full text]
  • समाचार प से च यत अंश Newspapers Clippings
    Dec 2020 समाचार प से चयत अशं Newspapers Clippings A Daily service to keep DRDO Fraternity abreast with DRDO Technologies, Defence Technologies, Defence Policies, International Relations and Science & Technology खंड : 45 अंक : 290 19-21 दसंबर 2020 Vol.: 45 Issue : 290 19-21 December 2020 ररा ववानान प ुपतकालयु तकालय DefenceDefence Science Science Library Library रार वैा वैानाकन कस चूसनूचान ाए एवव ं ं लेखनलेखन कक DefenceDefence Scientific Scientific Information Information & & Documentation Documentation Centre Centre , 110 054 मेटकॉफ हाउसहाउस, ददलल - - 110 054 MetcalfeMetcalfe House, House, Delhi Delhi - -110 110 054 054 CONTENTS S. No. TITLE Page No. DRDO News 1-22 DRDO Technology News 1-22 1. Raksha Mantri Shri Rajnath Singh hands over DRDO systems to Armed Forces 1 Chiefs 2. रा मंी ी राजनाथ सहं ने सश बल के मुख को डीआरडीओ क णालयां सपी 2 3. 4 .ఆ..ఓ. వవసలను ాయధ దల అపతలక అందజిన - రణ ాఖ మం ా ిం 4. Inauguration of Hypersonic Wind Tunnel at DRDO Hyderabad 6 5. डीआरडीओ हैदराबाद म हाइपरसोनक वडं टनल का उघाटन 7 6. Rajnath Singh hands over three important DRDO developed systems to Army, 9 Navy and Air Force 7. DRDO can play significant role in making India superpower: Defence Minister 10 Rajnath Singh 8. सीडीएस रावत बोले- भवय म जंग होने पर हम वदेशी हथयार से चटाएंगे दु मन को धलू 11 9. Defence Minister Rajnath Singh felicitates eminent scientists at DRDO award 12 function 10.
    [Show full text]
  • Organic-Inorganic Geochemical Characteristics of the Upper
    Hindawi Geofluids Volume 2021, Article ID 6651747, 26 pages https://doi.org/10.1155/2021/6651747 Research Article Organic-Inorganic Geochemical Characteristics of the Upper Permian Pusige Formation in a High-Saline Lake Basin, Tarim Basin: Implications for Provenance, Paleoenvironments, and Organic Matter Enrichment Jingbin Wang ,1,2,3 Zhiliang He ,1,2,4 Dongya Zhu ,2,3 Zhiqian Gao,1 Xiaowei Huang,1,2,3 and Quanyou Liu2,3 1China University of Geosciences (Beijing), Beijing 100083, China 2State Key Laboratory of Shale Oil and Gas Enrichment Mechanisms and Effective Development, Beijing 100083, China 3Petroleum Exploration and Production Research Institute, SINOPEC, Beijing 100083, China 4Department of Science and Technology, SINOPEC, Beijing 100728, China Correspondence should be addressed to Jingbin Wang; [email protected] Received 6 January 2021; Revised 27 February 2021; Accepted 3 March 2021; Published 7 April 2021 Academic Editor: Kun Zhang Copyright © 2021 Jingbin Wang et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. The third member (M3) of the Upper Permian Pusige Formation is a prominent organic-rich lacustrine mudstone sequence within the Yecheng-Hetian Sag, Tarim Basin, hosting major petroleum resources. However, its depositional history and organic matter (OM) enrichment mechanism have received little attention. Therefore, various organic and inorganic geochemical analyses were performed on thirty-four core samples from the Well DW1, to elucidate their depositional paleoenvironments, provenance, and tectonic setting, as well as the controlling factors of OM enrichment. Results showed that the M3 mudstones are classified as poor- to fair-quality hydrocarbon source rocks with mature type II-III kerogen, considering their low organic geochemical parameters.
    [Show full text]
  • Xiao Et Al..Fm
    International Geology Review, Vol. 45, 2003, p. 303¡ª¡-328. Copyright © 2003 by V. H. Winston & Son, Inc. All rights reserved. Multiple Accretionary Orogenesis and Episodic Growth of Continents: Insights from the Western Kunlun Range, Central Asia WENJIAO XIAO,1 Key Laboratory of Lithosphere Tectonic Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, P.O. Box 9825, Beijing 100029, China FANGLIN HAN, Shaanxi Institute of Geology Survey, Xianyang 712000, Shaanxi, China BRIAN F. WINDLEY, Department of Geology, University of Leicester, Leicester LE1 7RH, United Kingdom CHAO YUAN, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, Guangdong, China HUI ZHOU, Bureau of Science and Technology, Peking University, Beijing 100871, China AND JILIANG LI Key Laboratory of Lithosphere Tectonic Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, P.O. Box 9825, Beijing 100029, China Abstract The Western Kunlun Range in northwestern Tibet records a history of enlargement of the Central Asian crust. In the Early Ordovician a south-dipping intra-oceanic subduction-accretion complex was accreted to the Tarim block, forming an Andean-type margin in the Late Ordovician. This mar- gin grew southward (present-day coordinates) in the Early Silurian, with an accretionary complex on its southern side against which the Kudi gneiss-schist complex was attached. Clastic sediments continued to infill forearc/intra-arc basins on the top of the arc-accretionary complexes during Devo- nian–Carboniferous time. In the Early to Mid-Carboniferous, tectonic and magmatic quiescence is indicated by an absence of volcanic and plutonic rocks in the Kudi area, whereas subduction was still active in the western part of the range in the Gaz area near the present-day Pamir syntaxis.
    [Show full text]
  • Features of Permafrost in the West Kunlun Mountains
    BulletinofGlacierResearch7（1989）161－167 J（；J ⑥DataCenterforGlacierResearch，JapaneseSocictyofSnowandIce FeaturesofpermafrostintheWestKunlun Mountains u Shude and HEYixian LanzhouInstituteofGlacioIogyandGeocryology，AcademiaSinica，Lanzhou，China くReceivedDecember5，1988；R即isedmantlSCriptreceivedJaTluary23，1989） Abstract Permafro或isdistriblユted bo軌aiorlgtbe Xinjiang▼Ⅹizaロg Higbway and wide areasl〕etWeen TianshuihaiandKeriyaPass，Thelowerlimitofscatteredpermafrostisataround4300m aLS・1・ Thicknessofpermafrostvariesgreatly，fromlessthan5matthelowerlimittoaroundlOOmat Tianshuihai．MeanannualgroundtcmperaturerangesfromO・00CtoM3・2OC・Alongthesteepshoreof TianshuihaiLake，grOundiceincludingsma11icewedgeshavebeenobserved・Theverticalrange withinwhichtheperiglacialprocessesoccurisaround3000m‥from3800mtomorethan6000m▲ Almostalltypesofperiglaciallarldformsaredistributedinpermafrostareas・ 1．lntroduction featl汀eS：irlterlSivewindactionsirlCOidclimateoccl汀 SubseqⅥently，Wide pediment and diluvialねn were Thispaperdescribesthemainfeaturesofperma・ formed at the feet of theinteI㌧mOntane basins．The frostintheWestKunlunMountains，Withagreatdeal ridgesareusuallycoveredwithPrcpcambriancrystal・ OfdataobtainedintheSinoLJapanesejoirltCOmpre・ linerocksandgraniteandHercyniangranite（Yanget hensiveinvestigations carried outin1985and1987． αg．，1983）． BeforetbeseirlVeStigatiorlS，O111ybriefdescriptio‡lSOn BecatlSe Of tbeiocation of thel好est Ktlnlun 鱒rmafrostandperiglacialphenomenaintわisregion Mountains，也eprecipitationintbisreglOnismuchless Weregiveningeomorphologicalbooks（Geomorpho－
    [Show full text]
  • Application of High-Resolution Remote Sensing Technology for the Iron Ore
    2021 | 74/1 | 57–72 | 11 Figs. | 7 Tabs. | 2 Pls. | www.geologia-croatica.hr Journal of the Croatian Geological Survey and the Croatian Geological Society Application of high-resolution remote sensing technology for the iron ore deposits of the West Kunlun Mountains in China Yuhai Fan1,2,3,*, Hui Wang1,*, Xingke Yang3, Guofeng Zhang4, Zhaoyang Li1, Furong Tan1, Shaopeng Zhang1,2 and Wenbo Wang1 1 Geological Exploration Institute of Aerial Photogrammetry and Remote Sensing Bureau, Xi’an,710199 China; (*corresponding author: [email protected] / [email protected]) 2 Yulin University, School of Management, Yulin, 719000 China 3 Chang’an University, School of Earth Science and Land and Resources, Xi’an, 710054 China 4 Inner Mongolia Mining Exploitation CO.LTD, Hohhot, 010051 China doi: 10.4154/gc.2021.03 Abstract Article history: This study focuses on the iron ore of Taxkorgan and Heiqia in the West Kunlun mountains as a Manuscript received May 09, 2019 case study, for the application of WorldView−2 and IKONOS remote sensing images as major Revised manuscript accepted February 03, 2021 data sources in the fabrication of a standard image map and in the adoption of image enhance- Available online February 28, 2021 ment methods to extract information on the ore-controlling factors and mineralization, to interpret remote sensing for the mineral resources in these areas. ASTER, WorldView−2, and IKONOS data were applied for the extraction of alteration anomaly information. With an appropriate amount of field sampling and verification tests, this was used to establish a remote sensing ge- ology prospecting model, that would provide the basis for future remote sensing of metalloge nic belts in West Kunlun in the hope of discovering similar minerals.
    [Show full text]