Relevant bibliographies by topics / Himalaya-Tibet

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers

Academic literature on the topic 'Himalaya-Tibet'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Himalaya-Tibet"

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Stı̈we, K., B. Grasemann, and C. Miller. "16th Himalaya-Karakorum-Tibet Workshop." Journal of Asian Earth Sciences 19, no. 3 (2001): xiii. http://dx.doi.org/10.1016/s1367-9120(01)00016-5.

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SEARLE, M. P., and P. J. TRELOAR. "7th Himalaya-Karakoram-Tibet Workshop." Journal of the Geological Society 149, no. 6 (1992): 1045–47. http://dx.doi.org/10.1144/gsjgs.149.6.1045.

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Tremblay, Marissa M., Matthew Fox, Jennifer L. Schmidt, et al. "Erosion in southern Tibet shut down at ∼10 Ma due to enhanced rock uplift within the Himalaya." Proceedings of the National Academy of Sciences 112, no. 39 (2015): 12030–35. http://dx.doi.org/10.1073/pnas.1515652112.

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Exhumation of the southern Tibetan plateau margin reflects interplay between surface and lithospheric dynamics within the Himalaya–Tibet orogen. We report thermochronometric data from a 1.2-km elevation transect within granitoids of the eastern Lhasa terrane, southern Tibet, which indicate rapid exhumation exceeding 1 km/Ma from 17–16 to 12–11 Ma followed by very slow exhumation to the present. We hypothesize that these changes in exhumation occurred in response to changes in the loci and rate of rock uplift and the resulting southward shift of the main topographic and drainage divides from wi
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Clarke, Graham E., Charles Ramble, Martin Brauen, and Gerard Toffin. "Anthropology of Tibet and the Himalaya." Mountain Research and Development 15, no. 4 (1995): 358. http://dx.doi.org/10.2307/3673817.

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ARITA, Kazunori. "19th Himalaya-Karakoram-Tibet Workshop : HKT19." Journal of Geography (Chigaku Zasshi) 114, no. 4 (2005): 655–58. http://dx.doi.org/10.5026/jgeography.114.4_655.

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YUAN, QIONG, CHEN REN, and QIN-ER YANG. "Exclusion of Anemone tetrasepala (Ranunculaceae) from the flora of China." Phytotaxa 343, no. 2 (2018): 175. http://dx.doi.org/10.11646/phytotaxa.343.2.8.

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We demonstrate that all the Xizang (Tibet) specimens previously identified as Anemone tetrasepala (Ranunculaceae) actually belong to A. elongata, a species distributed in east Himalaya. Anemone tetrasepala is not known to occur in China, but is confined to north-west Himalaya only.
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Editor, The. "Guest Editors - 19th Himalaya-Karakoram-Tibet Workshop." Himalayan Journal of Sciences 2, no. 4 (2008): 73. http://dx.doi.org/10.3126/hjs.v2i4.803.

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Pécher, Arnaud, Jean-Luc Bouchez, and Patrick Le Fort. "Miocene dextral shearing between Himalaya and Tibet." Geology 19, no. 7 (1991): 683. http://dx.doi.org/10.1130/0091-7613(1991)019<0683:mdsbha>2.3.co;2.

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Mukherjee, Soumyajit, Barun Kumar Mukherjee, and Rasmus C. Thiede. "Geosciences of the Himalaya–Karakoram–Tibet orogen." International Journal of Earth Sciences 102, no. 7 (2013): 1757–58. http://dx.doi.org/10.1007/s00531-013-0934-0.

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Nadgir, B. B. "Geomorphology and tectonics of Himalaya-Tibet region." Journal of the Geological Society of India 83, no. 1 (2014): 115. http://dx.doi.org/10.1007/s12594-014-0020-7.

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Dissertations / Theses on the topic "Himalaya-Tibet"

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Williams, Helen Myfanwy. "Magmatic and tectonic evolution of Southern Tibet and the Himalaya." Thesis, [n.p.], 2000. http://library7.open.ac.uk/abstracts/page.php?thesisid=58.

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Brouand, Marc. "Pétrogenèse des migmatites de la dalle du Tibet (Himalaya du Népal)." Vandoeuvre-les-Nancy, INPL, 1989. http://www.theses.fr/1989NAN10391.

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La chaîne de collision continentale himalayenne offre le rare privilège, par l'intermédiaire de grandes vallées transversales, d'étudier à la fois les leucogranites cénozoïques, mis en place au Nord du cristallin du Haut Himalaya et leur région source: la formation I de la dalle du Tibet. La compréhension des mécanismes de genèse et de mise en place des granites justifie l'étude des migmatites de la dalle du Tibet. Au Népal Central, la dalle du Tibet est migmatite sur toute son épaisseur, mais le degré de fusion reste modéré (métatexites), ce qui permet de saisir les premiers mécanismes anatec
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Lyon-Caen, Hélène. "Deep structure of the Himalaya and Tibet from gravity and seismological data." Thesis, Massachusetts Institute of Technology, 1985. http://hdl.handle.net/1721.1/54953.

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Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 1986.<br>Microfiche copy available in Archives and Science<br>Includes bibliographies.<br>by Hélène Lyon-Caen.<br>Ph.D.
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Laskowski, Andrew Keith, and Andrew Keith Laskowski. "Tectonic Evolution of the Yarlung Suture Zone, Lopu Range and Lazi Regions, Central Southern Tibet." Diss., The University of Arizona, 2016. http://hdl.handle.net/10150/623178.

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The Yarlung (India-Asia) suture zone in southern Tibet records Middle Jurassic—Late Cretaceous development of the Lhasa terrane (Eurasian) convergent margin and subsequent India-Asia collision beginning in Paleocene time. This dissertation reports data from field-based geologic investigation of the Yarlung suture zone in the Lopu Range and Lazi Regions, ~600 and ~300 km west of the city of Lhasa, respectively. Field data were combined with new geochronology (detrital and igneous zircon U-Pb, garnet Lu-Hf), thermochronology (white mica Ar-Ar and zircon U-Th/He), and metamorphic petrology data t
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Chapman, James B., and Paul Kapp. "Tibetan Magmatism Database." AMER GEOPHYSICAL UNION, 2017. http://hdl.handle.net/10150/626432.

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A database containing previously published geochronologic, geochemical, and isotopic data on Mesozoic to Quaternary igneous rocks in the Himalayan-Tibetan orogenic system are presented. The database is intended to serve as a repository for new and existing igneous rock data and is publicly accessible through a web-based platform that includes an interactive map and data table interface with search, filtering, and download options. To illustrate the utility of the database, the age, location, and Hf-t composition of magmatism from the central Gangdese batholith in the southern Lhasa terrane are
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Laskowski, Andrew K., Paul Kapp, Jeff D. Vervoort, and Lin Ding. "High-pressure Tethyan Himalaya rocks along the India-Asia suture zone in southern Tibet." GEOLOGICAL SOC AMER, INC, 2016. http://hdl.handle.net/10150/622664.

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This study documents an early Cenozoic continental high-pressure (HP) metamorphic complex along the Yarlung (India-Asia) suture zone in southern Tibet. The complex is exposed in the Lopu Range, located similar to 600 km west of the city of Lhasa. HP rocks in the core of the complex have Indian passive-margin (Tethyan Himalaya Sequence) protoliths and are exposed in the footwall of a top-to-the-north, normal-sense shear zone. Phengite geobarometry, Zr-in-rutile geothermometry, and pseudosection modeling indicate that these rocks reached pressures >= 1.4 GPa at temperatures <= 600 degrees C. A m
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Vandenhelsken, Mélanie. "Le monastère bouddhique de Pemayangtse au Sikkim (Himalaya Occidental, Inde) : un monastère dans le monde." Montpellier 3, 2002. http://www.theses.fr/2002MON30048.

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Le monastère bouddhique de Pemayangtse, situé dans l'État himalayen du Sikkim, a la particularité de n'admettre au sein de sa communauté religieuse que les seuls membres de clans apparentés au clan royal. Ces clans constituent la noblesse lhopo, descendante de lointains émigrant du Tibet et du Bhoutan, qui fonda le royaume bouddhiste du Sikkim au XVIIe siècle, et domina les populations locales. Cette étude aborde la question des relations entre ordre temporel et ordre spirituel dans cette région. L'implication du monastère dans la société étant au cœur du sujet, ce dernier est abordé par une e
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Laskowski, Andrew K., Paul Kapp, Lin Ding, Clay Campbell, and XiaoHui Liu. "Tectonic evolution of the Yarlung suture zone, Lopu Range region, southern Tibet." AMER GEOPHYSICAL UNION, 2017. http://hdl.handle.net/10150/623108.

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The Lopu Range, located similar to 600km west of Lhasa, exposes a continental high-pressure metamorphic complex beneath India-Asia (Yarlung) suture zone assemblages. Geologic mapping, 14 detrital U-Pb zircon (n=1895 ages), 11 igneous U-Pb zircon, and nine zircon (U-Th)/He samples reveal the structure, age, provenance, and time-temperature histories of Lopu Range rocks. A hornblende-plagioclase-epidote paragneiss block in ophiolitic melange, deposited during Middle Jurassic time, records Late Jurassic or Early Cretaceous subduction initiation followed by Early Cretaceous fore-arc extension. A d
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Schmidt, Joachim [Verfasser], and Georg [Akademischer Betreuer] Miehe. "Biogeographisch-phylogenetische Untersuchungen an Hochgebirgs-Laufkäfern : ein Beitrag zur Umweltgeschichte des Himalaya-Tibet Orogens / Joachim Schmidt. Betreuer: Georg Miehe." Marburg : Philipps-Universität Marburg, 2011. http://d-nb.info/1013255577/34.

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Hetényi, György. "Evolution of deformation of the Himalayan prism : from imaging to modelling." Paris 11, 2007. http://www.theses.fr/2007PA112258.

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L'Himalaya-Tibet est considéré comme l'exemple classique de collision continentale. Cependant, de nombreuses questions fondamentales sur la structure, la rhéologie et les processus physiques liés à l'évolution de la lithosphère de cette région restent ouvertes. Cette thèse apporte de nouvelles contraintes sur ces sujets. De nouvelles images de la lithosphère sont issues de l'expérience sismologique large-bande Hi-CLIMB. Les caractéristiques du déploiement et l'utilisation des fonctions récepteurs en incluant les multiples ont permis d'imager en détail: le MHT y compris sa partie profonde; des
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Books on the topic "Himalaya-Tibet"

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Mascle, Georges H. Himalaya-Tibet: La collision continentale Inde-Eurasie. Vuibert, 2010.

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Hedin, Sven Anders. Trans-Himalaya: Discoveries and adventures in Tibet. Asian Educational Services, 1999.

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Colliding continents: A geological exploration of the Himalaya, Karakoram, & Tibet. Oxford University Press, 2013.

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Vienna, Austria) Himalaya Karakorum Tibet Workshop (8th 1993. 8th Himalaya Karakorum Tibet Workshop: Vienna, 29.3.--2.4.1993 : abstract volume. Geologische Bundesanstalt, 1993.

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Green, Jonathan. Murder in the high Himalaya: Loyalty, tragedy, and escape from Tibet. PublicAffairs, 2010.

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Murder in the high Himalaya: Loyalty, tragedy, and escape from Tibet. Perseus Books Group, 2010.

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Green, Jonathan. Murder in the high Himalaya: Loyalty, tragedy, and escape from Tibet. PublicAffairs, 2010.

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A Survey of Bonpo monasteries and temples in Tibet and the Himalaya. National Museum of Ethnology, 2003.

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gtan/, 1936 mkhar rme'u bsam. a survey of bonpo monasteries and temples in tibet and the himalaya. The national museum of ethnology, 2003.

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Footprints in the Himalaya: People, places and practices : Bhutan, Darjeeling, Nepal, Sikkim & Tibet. Sonam B. Wangyal, 2006.

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Book chapters on the topic "Himalaya-Tibet"

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Varentsov, Iv M., P. V. Ivanov, I. N. Lozovsky, et al. "Geoelectric Models Along the Profile Crossing the Indian Craton, Himalaya and Eastern Tibet Resulted from Simultaneous MT/MV Soundings." In Springer Proceedings in Earth and Environmental Sciences. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-35906-5_10.

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Buckley, Michael. "A First-Hand Narrative Account on Tibet’s Paper Parks: How China’s Greenwashing in Tibet Flies Under the Radar." In Hindu Kush-Himalaya Watersheds Downhill: Landscape Ecology and Conservation Perspectives. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-36275-1_10.

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Sorkhabi, Rasoul B., and Allison Macfarlane. "Himalaya and Tibet: Mountain roots to mountain tops." In Himalaya and Tibet: Mountain Roots to Mountain Tops. Geological Society of America, 1999. http://dx.doi.org/10.1130/0-8137-2328-0.1.

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Searle, Mike. "The Making of the Himalaya, Karakoram, and Tibetan Plateau." In Colliding Continents. Oxford University Press, 2013. http://dx.doi.org/10.1093/oso/9780199653003.003.0019.

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My quest to figure out how the great mountain ranges of Asia, the Himalaya, Karakoram, and Tibetan Plateau were formed has thus far lasted over thirty years from my first glimpse of those wonderful snowy mountains of the Kulu Himalaya in India, peering out of that swaying Indian bus on the road to Manali. It has taken me on a journey from the Hindu Kush and Pamir Ranges along the North-West Frontier of Pakistan with Afghanistan through the Karakoram and along the Himalaya across India, Nepal, Sikkim, and Bhutan and, of course, the great high plateau of Tibet. During the latter decade I have extended these studies eastwards throughout South East Asia and followed the Indian plate boundary all the way east to the Andaman Islands, Sumatra, and Java in Indonesia. There were, of course, numerous geologists who had ventured into the great ranges over the previous hundred years or more and whose findings are scattered throughout the archives of the Survey of India. These were largely descriptive and provided invaluable ground-truth for the surge in models that were proposed to explain the Himalaya and Tibet. When I first started working in the Himalaya there were very few field constraints and only a handful of pioneering geologists had actually made any geological maps. The notable few included Rashid Khan Tahirkheli in Kohistan, D. N. Wadia in parts of the Indian Himalaya, Ardito Desio in the Karakoram, Augusto Gansser in India and Bhutan, Pierre Bordet in Makalu, Michel Colchen, Patrick LeFort, and Arnaud Pêcher in central Nepal. Maps are the starting point for any geological interpretation and mapping should always remain the most important building block for geology. I was extremely lucky that about the time I started working in the Himalaya enormous advances in almost all aspects of geology were happening at a rapid pace. It was the perfect time to start a large project trying to work out all the various geological processes that were in play in forming the great mountain ranges of Asia. Satellite technology suddenly opened up a whole new picture of the Earth from the early Landsat images to the new Google Earth images.
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Searle, Mike. "Continents in Collision: Kashmir, Ladakh, Zanskar." In Colliding Continents. Oxford University Press, 2013. http://dx.doi.org/10.1093/oso/9780199653003.003.0007.

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To understand how the Himalaya were formed it seemed logical to start at the actual zone of plate collision, the Indus suture zone. Most of this collision zone runs across southern Tibet, which in the 1970s was almost impossible to travel through. Following Mao Tse-tung’s Red Army’s invasion and occupation of Tibet in October 1950, that region had remained firmly closed to all foreigners. In the western Himalaya the Indus suture zone runs right across the northernmost province of Ladakh. Ladakh used to be a part of southwestern Tibet before the British annexed it during the Raj. Leh, the ancient capital of Ladakh at 3,500 metres in the Indus Valley, was the final outpost of British India before the great trans-Himalayan barrier of the Karakoram Range. Only the Nubra Valley and the Tangtse Valley north of Leh were beyond the Indus, and these valleys led directly up to the desolate high plateau of Tibet. Leh was a major caravan route and a crossroads of high Asia, with double-humped dromedary camel caravans coming south from the Silk Route towns of Yarkhand and Khotan; Kashmiris and Baltis came from the west and Indian traders from the Hindu regions of Himachal and Chamba to the south. Ladakh, Zanskar, and Zangla were three ancient Himalayan kingdoms ruled by a Giapo, or King, each from a palace that resembled a small version of the Potala Palace in Lhasa. In 1978, when we were climbing in the mountains of Kulu, I had looked from our high summits across to the desert mountains of Lahoul and Zanskar, north of the main Himalayan watershed. Here, in the ancient Buddhist kingdoms of Zanskar and Ladakh lay wave upon wave of unexplored and unclimbed mountains. They lay north of the monsoon limits and in the rain shadow of the main Himalaya, so the vegetation was sparse, and the geology was laid bare. Flying north from Delhi, or east from Kashmir into Leh, the views were simply mesmerizing.
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Hughes, Nigel C., and Peter A. Jell. "Biostratigraphy and biogeography of Himalayan Cambrian trilobites." In Himalaya and Tibet: Mountain Roots to Mountain Tops. Geological Society of America, 1999. http://dx.doi.org/10.1130/0-8137-2328-0.109.

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Guillot, Stéphane, Michael Cosca, Pascal Allemand, and Patrick Le Fort. "Contrasting metamorphic and geochronologic evolution along the Himalayan belt." In Himalaya and Tibet: Mountain Roots to Mountain Tops. Geological Society of America, 1999. http://dx.doi.org/10.1130/0-8137-2328-0.117.

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Whittington, Alan G., Nigel B. W. Harris, and Robert W. H. Butler. "Contrasting anatectic styles at Nanga Parbat, northern Pakistan." In Himalaya and Tibet: Mountain Roots to Mountain Tops. Geological Society of America, 1999. http://dx.doi.org/10.1130/0-8137-2328-0.129.

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Pêcher, Arnaud, and Patrick Le Fort. "Late Miocene tectonic evolution of the Karakorum–Nanga Parbat contact zone (northern Pakistan)." In Himalaya and Tibet: Mountain Roots to Mountain Tops. Geological Society of America, 1999. http://dx.doi.org/10.1130/0-8137-2328-0.145.

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DiPietro, Joseph A., Kevin R. Pogue, Ahmad Hussain, and Irshad Ahmad. "Geologic map of the Indus syntaxis and surrounding area, northwest Himalaya, Pakistan." In Himalaya and Tibet: Mountain Roots to Mountain Tops. Geological Society of America, 1999. http://dx.doi.org/10.1130/0-8137-2328-0.159.

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Conference papers on the topic "Himalaya-Tibet"

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Liu, Xiaobing, Xiaohan Liu, P. H. Leloup, G. Mahéo, Guangwei Li, and Lijie Wei. "STRUCTURAL CHARACTERISTICS OF THE UPPER HIMALAYA CRYSTALLINE SEQUENCE，IN NYALAM AREA，SOUTHERN TIBET AND GEOLOGICAL IMPLICATIONS." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-300392.

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Krupa, Anthony J., Jay Quade та Paul Kapp. "ΔD VALUES OF SHEAR ZONE MICAS FROM LHAGOI KANGRI IN SOUTH-CENTRAL TIBET SUGGEST A HIGH HIMALAYA BY THE MID-MIOCENE". У GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-340395.

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Soucy La Roche, Renaud, Laurent Godin, Lyal Harris, and Aurélie Gicquel. "THE ROLE OF TRANSVERSE BASEMENT STRUCTURES AND OBLIQUE TERRANE BOUNDARIES ON THE ARCHITECTURE OF LARGE-HOT LONG OROGENS - EXAMPLES FROM THE HIMALAYA-TIBET AND GRENVILLE OROGENS." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-355816.

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