Search Results - "Tibet"
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Baseline map of soil organic carbon in Tibet and its uncertainty in the 1980s
Published 2019“…Much of the carbon (C) stored in the soil of the high Qinghai–Tibet Plateau could be lost as a result of global warming. …”
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Origin of postcollisional magmas and formation of porphyry Cu deposits in southern Tibet
Published 2018“…We review the literature and compile available data on whole rock and isotope geochemistry for Cenozoic igneous rocks from Tibet, and add new zircon Ce4+/Ce3+ and Ti-in-zircon thermometry data to better understand variations in oxidation state and thermal evolution of these suites, which are key controls on Cu mineralization. …”
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Integrating multi-source data to improve water erosion mapping in Tibet, China
Published 2018“…However, due to the large area, sparse and limited data in Tibet, soil erosion there is still poorly quantified. …”
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Pliocene-Quaternary crustal melting in central and northern Tibet and insights into crustal flow
Published 2016“…Here we report petrological and geochemical data on magmas erupted 4.7-0.3 Myr ago in central and northern Tibet, demonstrating that they were generated by partial melting of crustal rocks at temperatures of 700-1,050°C and pressures of 0.5-1.5 GPa. …”
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Pan-African granulites of Madagascar and southern India: Gondwana assembly and parallels with modern Tibet
Published 2016“…Bounding sutures most likely record transfer of this microcontinent across the Neoproterozoic Mozambique Ocean, analogous to Gondwanan terranes that crossed Tethys before final India-Asia collision and, like Tibet, these sutures mark the edges of a plateau that formed following terminal ocean closure and collision. …”
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U-Pb SHRIMP zircon geochronology and T-t-d history of the Kampa Dome, southern Tibet
Published 2008“…Structural, petrographic and geochronologic studies of the Kampa Dome provide insights into the tectonothermal evolution of orogenic crust exposed in the North Himalayan gneiss domes of southern Tibet. U–Pb ion microprobe dating of zircons from granite gneiss exposed at the deepest levels within the dome yields concordia 206Pb/238U age populations of 506 ± 3 Ma and 527 ± 6 Ma, with no evidence of new zircon growth during Himalayan orogenesis. …”
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The Influence of Public Financial Input on the development of regional cultural industry: A case study of Tibet
Published 2020“…This dissertation adopts the statistical data of Tibet Autonomous Region, DEA model, VAR model and other methods to evaluate the performance of public investment on the development of cultural industry in Tibet Autonomous Region from the horizontal and vertical perspectives, predicts the development of cultural industry until 2030, and finally puts forward policy Suggestions based on the conclusions. …”
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The Nadun Cu-Au mineralization, central Tibet: Root of a high sulfidation epithermal deposit
Published 2016“…A new high sulfidation epithermal Cu–Au occurrence (Nadun) has been discovered adjacent to the Cretaceous Duolong porphyry Cu–Au deposit within the Bangong–Nujiang metallogenic belt, central Tibet. The Nadun Cu–Au mineralization is hosted in a tectonic–hydrothermal breccia with advanced argillic alteration, which occurs above sandstone, associated with quartz–pyrite veins. …”
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To Further Understating of Environmental, Social and Cultural Sustainability Issues and Chinese Governments Role in the Tourism Development in Tibet
Published 2008“…Abstract Chinese government recently years, has realized the pillar position and potential market power of Tibets tourism industry. In order to attract more direct foreign investment and tourists, Chinese government has made great efforts on the initial stage of constructing Tibets tourism infrastructure facilities and developing Tibets tourism market. …”
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Eocene Neo-Tethyan slab breakoffconstrained by 45 Ma oceanic island basalt-type magmatism in southern Tibet
Published 2016“…Slab breakoffis one of the primary processes in the evolution of many collisional orogens. In the Tibet-Himalaya orogen, the timing of breakoffof the Neo-Tethyan slab remains controversial because of a scarcity of solid evidence. …”
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Landscapes of resistance: Tibetan modernity and the online politics of representation in contemporary China
Published 2019Subjects: “…tibet…”
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Petrogenesis and tectonic setting of Early Cretaceous granodioritic porphyry from the giant Rongna porphyry Cu deposit, central Tibet
Published 2018“…© 2018 The Rongna Cu-(Au) deposit is a recently discovered giant low-grade composite porphyry-high sulfidation epithermal system in the Duolong ore district of central Tibet. We present zircon U-Pb ages, bulk-rock geochemical and Sr-Nd isotope data, as well as zircon Hf-O isotope data to constrain the petrogenesis of the Rongna granodioritic porphyry, on which the ore system is centered. …”
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Geochronology, geochemistry, and zircon Hf isotopic compositions of Mesozoic intermediate-felsic intrusions in central Tibet: Petrogenetic and tectonic implications
Published 2014“…Mesozoic intermediate-felsic intrusions are widely distributed in the southern Qiangtang terrane, central Tibet. Zircon U-Pb dating shows that these intrusions formed in two periods in the Jurassic (169-150Ma) and Cretaceous (127-113Ma). …”
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Petrogenesis of Paleocene-Eocene porphyry deposit-related granitic rocks in the Yaguila-Sharang ore district, central Lhasa terrane, Tibet
Published 2016“…The Paleocene-Eocene ore deposits in the Gangdese Metallogenic Belt, Tibet, are thought to have been formed during the main period of India-Asia continental collision. …”
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Thermal history of the giant Qulong Cu-Mo deposit, Gangdese metallogenic belt, Tibet: Constraints on magmatic-hydrothermal evolution and exhumation
Published 2015“…A complete thermal history for the Qulong porphyry Cu–Mo deposit, Tibet is presented. Zircon U–Pb geochronology indicates that the mineralization at Qulong resulted from brecciation-veining events associated with the emplacement of a series of intermediate-felsic intrusions. …”
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