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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. -
ARUN IYER Chairman & Chief Creative Officer Lowe Lintas
January 1-15, 2018 Volume 6, Issue 14 `100 6 INTERVIEW ARUN IYER Chairman & Chief Creative Officer Lowe Lintas KEROVIT A Different Take Will Anushka Sharma’s 20 histrionics do the trick? 10 VIJAY SALES Taking Them On How is this retail store handling online rivals? 22 VOOT Subs riber o yf not or resale Changing the Game How to get eyeballs without spending much. “I SEE EVERYBODY ZEE MEDIA Another Addition 8 BLACK SWAN AS COMPETITION” On a Roll 8 A breezy chat with one of the brightest creative MTV INDIA Star-studded Teams 18 minds in Indian advertising. MUSIC ON DEMAND Music vs Music 23 eol This fortnight... Volume 6, Issue 14 got my appointment for this interview with Arun Iyer in 30 seconds. He heard me EDITOR Sreekant Khandekar I out over a call and said, ‘Let’s do it.’ No ‘Let me check my schedule’, no ‘Send PUBLISHER January 1-15, 2018 Volume 6, Issue 14 `100 me a mail first’, no ‘Depends on what you’re going to ask me’, no ‘Talk to my PR Sreekant Khandekar 6 INTERVIEW team’, or any of the things journalists typically hear from a lot of senior folks who EXECUTIVE EDITOR ARUN IYER Chairman & Chief Creative Officer Ashwini Gangal Lowe Lintas work for large, globally networked corporates. Sure, I may have caught him on a good KEROVIT A Different Take day, but this exchange reflects how simple Arun likes to keep things. ASSOCIATE EDITOR Will Anushka Sharma’s 20 histrionics do the trick? Sunit Roy 10 PRODUCTION EXECUTIVE I’ve been writing about Indian advertising for almost eight years and am surprised Andrias Kisku VIJAY SALES Taking Them On to discover that this is the first time I’ve interviewed Arun, at length; (I have a How is this retail store ADVERTISING ENQUIRIES handling online rivals? feeling this is the real reason I pitched this idea to my boss, shhh). -
Outcome-AGM-2016.Pdf
Spine to be adjusted by printer C-13, Balaji House, Dalia Industrial Estate, Opposite Laxmi Industrial Estate, New Link Road, Andheri (West) Mumbai - 400 053. www.balajitelefilms.com world.com dickenson www. dickenson Spine to be adjusted by printer Spine to be adjusted by printer Spine to be adjusted by printer We are content innovators, creators and producers of unmatched credentials and long-standing success. We operate as a vertically integrated studio model, which allows us to create, distribute and monetise content, not only in ways that are best aligned with viewer preferences, but in ways in which we can capture the maximum value stream. With a focus on chasing quality growth, we continue to create gripping content – content that is relevant to As global viewership diverse sets of audiences and accessible across multiple platforms. continues to evolve, we have With geographical boundaries disappearing in the seamless world of the anticipated future trends and internet, we aim to make our content seamlessly available. Improvement in created new entertainment mobile broadband infrastructure, gradual reduction in cost of internet and paradigms. Today, we increase in smartphone screen sizes is driving consumer preferences. straddle across all the three The Subscription Video on Demand (SVOD) market in India is on the cusp distinct platforms through of a meteoric take-off. As Over The Top (OTT) video consumption continues which people consume to grow tremendously, we are leveraging our capabilities to create content entertainment – across platforms. Our motive is vertical integration across the value chain by Television, offering our own OTT services. We are making our delivery channels more closely aligned to the emerging needs and creating entertainment-on-the-go Movies and for our dynamic audiences. -
Prokaryotic Biodiversity of Lonar Meteorite Crater Soda Lake Sediment and Community Dynamics During Microenvironmental Ph Homeostasis by Metagenomics
Prokaryotic Biodiversity of Lonar Meteorite Crater Soda Lake Sediment and Community Dynamics During Microenvironmental pH Homeostasis by Metagenomics Dissertation for the award of the degree "Doctor of Philosophy" Ph.D. Division of Mathematics and Natural Sciences of the Georg-August-Universität Göttingen within the doctoral program in Biology of the Georg-August University School of Science (GAUSS) Submitted by Soumya Biswas from Ranchi (India) Göttingen, 2016 Thesis Committee Prof. Dr. Rolf Daniel Department of Genomic and Applied Microbiology, Institute of Microbiology and Genetics, Faculty of Biology and Psychology, Georg-August-Universität Göttingen, Germany PD Dr. Michael Hoppert Department of General Microbiology, Institute of Microbiology and Genetics, Faculty of Biology and Psychology, Georg-August-Universität Göttingen, Germany Members of the Examination Board Reviewer: Prof. Dr. Rolf Daniel, Department of Genomic and Applied Microbiology, Institute of Microbiology and Genetics, Faculty of Biology and Psychology, Georg-August-Universität Göttingen, Germany Second Reviewer: PD Dr. Michael Hoppert, Department of General Microbiology, Institute of Microbiology and Genetics, Faculty of Biology and Psychology, Georg-August-Universität Göttingen, Germany Further members of the Examination Board: Prof. Dr. Burkhard Morgenstern, Department of Bioinformatics, Institute of Microbiology and Genetics, Faculty of Biology and Psychology, Georg-August-Universität Göttingen, Germany PD Dr. Fabian Commichau, Department of General Microbiology, -
Lake Status Records from China: Data Base Documentation
Lake status records from China: Data Base Documentation G. Yu 1,2, S.P. Harrison 1, and B. Xue 2 1 Max Planck Institute for Biogeochemistry, Postfach 10 01 64, D-07701 Jena, Germany 2 Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences. Nanjing 210008, China MPI-BGC Tech Rep 4: Yu, Harrison and Xue, 2001 ii MPI-BGC Tech Rep 4: Yu, Harrison and Xue, 2001 Table of Contents Table of Contents ............................................................................................................ iii 1. Introduction ...............................................................................................................1 1.1. Lakes as Indicators of Past Climate Changes........................................................1 1.2. Chinese Lakes as Indicators of Asian Monsoonal Climate Changes ....................1 1.3. Previous Work on Palaeohydrological Changes in China.....................................3 1.4. Data and Methods .................................................................................................6 1.4.1. The Data Set..................................................................................................6 1.4.2. Sources of Evidence for Changes in Lake Status..........................................7 1.4.3. Standardisation: Lake Status Coding ..........................................................11 1.4.4. Chronology and Dating Control..................................................................11 1.5. Structure of this Report .......................................................................................13 -
The Moho Beneath Western Tibet: Shear Zones and Eclogitization in the Lower Crust ∗ Zhongjie Zhang A,1, Yanghua Wang B, Gregory A
Earth and Planetary Science Letters 408 (2014) 370–377 Contents lists available at ScienceDirect Earth and Planetary Science Letters www.elsevier.com/locate/epsl The Moho beneath western Tibet: Shear zones and eclogitization in the lower crust ∗ Zhongjie Zhang a,1, Yanghua Wang b, Gregory A. Houseman c, , Tao Xu a, Zhenbo Wu a, Xiaohui Yuan d, Yun Chen a, Xiaobo Tian a, Zhiming Bai a, Jiwen Teng a a Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China b Department of Earth Science and Engineering, Imperial College London, SW7 2AZ, UK c School of Earth and Environment, University of Leeds, LS2 9JT, UK d GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany a r t i c l e i n f o a b s t r a c t Article history: The Tibetan Plateau is formed by continuing convergence between Indian and Asian plates since ∼50 Ma, Received 11 July 2014 involving more than 1400 km of crustal shortening. New seismic data from western Tibet (the TW-80 Received in revised form 10 October 2014 ◦ experiment at 80 E) reveal segmentation of lower crustal structure by the major sutures, contradicting Accepted 13 October 2014 the idea of a mobile lower crust that flows laterally in response to stress variations. Significant changes Available online xxxx in crustal structure and Moho depth occur at the mapped major tectonic boundaries, suggesting that Editor: A. Yin zones of localized shear on sub-vertical planes extend through the crust and into the upper mantle. Keywords: Converted waves originating at the Moho and at a shallower discontinuity are interpreted to define a Tibetan Plateau partially eclogitized layer that extends 200 km north of the Indus–Yarlung Suture Zone, beneath the Moho segmentation entire Lhasa block at depths of between 50 and 70 km. -
Research Article Triassic-Jurassic Granitoids and Pegmatites From
GeoScienceWorld Lithosphere Volume 2020, Article ID 7282037, 22 pages https://doi.org/10.2113/2020/7282037 Research Article Triassic-Jurassic Granitoids and Pegmatites from Western Kunlun-Pamir Syntax: Implications for the Paleo-Tethys Evolution at the Northern Margin of the Tibetan Plateau 1,2 1 3,4 1 1 Xiao-Qiang Liu , Chuan-Lin Zhang , Haibo Zou, Qian Wang, Xiao-Shu Hao, 5 1 Hai-Xiang Zhao, and Xian-Tao Ye 1College of Oceanography, Hohai University, Nanjing 210098, China 2School of Geology and Mining Engineering, Xinjiang University, Urumqi 830046, China 3Department of Geosciences, Auburn University, Auburn, AL 36849, USA 4State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi’an 710069, China 5School of Earth Sciences and Engineering, Hohai University, Nanjing 210098, China Correspondence should be addressed to Chuan-Lin Zhang; [email protected] Received 7 March 2020; Accepted 5 December 2020; Published 31 December 2020 Academic Editor: Alexander R. Simms Copyright © 2020 Xiao-Qiang Liu et al. Exclusive Licensee GeoScienceWorld. Distributed under a Creative Commons Attribution License (CC BY 4.0). The Western Kunlun-Pamir-Karakorum (WKPK) at the northwestern Tibetan Plateau underwent long-term terrane accretion from the Paleozoic to the Cenozoic. Within this time span, four phases of magmatism occurred in WKPK during the Early Paleozoic, Triassic-Jurassic, Early Cretaceous, and Cenozoic. These voluminous magmatic rocks contain critical information on the evolution of the Tethys Oceans. In this contribution, we provide field observations, petrography, ages, whole-rock elemental and Sr-Nd isotopic compositions, and zircon in situ Lu-Hf isotopes of the Triassic-Jurassic granitoids and pegmatites from the Dahongliutan in Western Kunlun and Turuke area at the Pamir Plateau, in an attempt to constrain their petrogenesis and to decipher a more detailed Paleo-Tethys evolution process. -
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). -
“BEING INSTITUTIONAL” Pg
Spine to be adjusted by printer ANNUAL REPORT 2014 -15 TELEVISION Developing Strong Brand Equity Pg. 42 Collaborating Creatively Pg. 44 “BEING world.com INSTITUTIONAL” Pg. 16 Ekta Kapoor dickenson MOVIES www. Optimising Pg. 52 dickenson Creative Strengths Creating an Exciting Pipeline Pg. 54 C-13, Balaji House, IPR Dalia Industrial Estate, Opposite Laxmi Industrial Estate, New Link Road, Andheri (West) Mumbai - 400 053. Monetising Current Assets Pg. 38 www.balajitelefilms.com Adding New Properties Pg. 39 Spine to be adjusted by printer Spine to be adjusted by printer 9 6 8 10 2 5 7 1 4 1. Ms. Ekta Kapoor 2. Mr. Sameer Nair The ‘Balaji’ brand is getting bigger each day. 3. Ms. Tanusri Dasgupta 4. Mr. Shubhodip Pal We have a strong visibility of our TV and movies 5. Mr. Ketan Gupta slate for 2016 and 2017 which underpins a 6. Mr. Tushar Hiranandani positive outlook. Our key drivers in FY2016 will 7. Ms. Coralie Ansari be great ideas, packaging and marketing. We 8. Mrs. Simmi Singh Bisht 9. Mr. Tanveer Bookwala will continue to focus on building strong brand 10. Ms. Ruchikaa Kapoor franchises to better connect with our TV and 11. Mr. Sanjay Dwivedi 3 film audiences. 12. Mr. Vimal Doshi 13. Mr. Ayan Roy Chowdhury Spine to be adjusted by printer 13 12 11 A transformational change is currently underway at the Balaji House. As a promoter driven company, Balaji has travelled a great journey of growth, stature and maturity. Thanks to the love, passion and hard work of the Kapoor family, Balaji now stands at the forefront of the entertainment industry and has the opportunity to travel into new orbits of growth. -
Former President Pranab Mukherjee Passes Away
C M Y K Former President Pranab Mukherjee passes away 90-yr-old Corona ‘winner’ dots the day NEW DELHI, Aug 31: rum to every post held by State records 78 cases, 63 recover too Former President Pranab him, during his long and dis- Mukherjee passed away on tinguished public service. ITANAGAR, Aug 31: The lang eight and Tawang sev- In East Kameng, three are Lohit one is an ITBP person- Monday at Army's Research Prime Minister Narendra mental heroics of a nonage- en. Papum Pare contracted IRBn personnel returnees nel also detected in QF. and Referral Hospital here, Modi, in a series of tweets, narian, who beat the novel six cases, East Kameng five from ICR and two are also Of the total infections, 72 informed his son and Con- said he had left an indelible Coronavirus today, marked and four each came from returnees from ICR. The East are asymptomatic and six are gress leader Abhijit Mukher- mark on the development tra- the day in which the State East Siang and Lower Siang. Siang cases comprised two symptomatic, as per the bul- jee. He was 84. jectory of the nation. recorded a total of 78 Covid- Two cases each were found detections (driver & handy- letin. “With a Heavy Heart, this ''As India's President, Shri 19 cases and also discharged in West Siang, Lower Dibang man) from Ruksin check Of the 63 positive cases is to inform you that my fa- Pranab Mukherjee made 63 patients following their Valley, Tirap and Shi-Yomi. gate, one is an APP person- released today in nine dis- ther Shri #PranabMukherjee Rashtrapati Bhavan even recovery from the virus, tak- One each was detected in nel returnee from ICR and tricts, Papum Pare was has just passed away inspite more accessible to common ing its tally of confirmed cas- Lower Subansiri, Namsai, one is a caretaker from Juve- placed first with 18 recover- of the best efforts of Doctors citizens. -
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Spine to be adjusted by printer C-13, Balaji House, Dalia Industrial Estate, Opposite Laxmi Industrial Estate, New Link Road, Andheri (West) Mumbai - 400 053. www.balajitelefilms.com world.com dickenson www. dickenson Spine to be adjusted by printer Spine to be adjusted by printer Spine to be adjusted by printer We are content innovators, creators and producers of unmatched credentials and long-standing success. We operate as a vertically integrated studio model, which allows us to create, distribute and monetise content, not only in ways that are best aligned with viewer preferences, but in ways in which we can capture the maximum value stream. With a focus on chasing quality growth, we continue to create gripping content – content that is relevant to As global viewership diverse sets of audiences and accessible across multiple platforms. continues to evolve, we have With geographical boundaries disappearing in the seamless world of the anticipated future trends and internet, we aim to make our content seamlessly available. Improvement in created new entertainment mobile broadband infrastructure, gradual reduction in cost of internet and paradigms. Today, we increase in smartphone screen sizes is driving consumer preferences. straddle across all the three The Subscription Video on Demand (SVOD) market in India is on the cusp distinct platforms through of a meteoric take-off. As Over The Top (OTT) video consumption continues which people consume to grow tremendously, we are leveraging our capabilities to create content entertainment – across platforms. Our motive is vertical integration across the value chain by Television, offering our own OTT services. We are making our delivery channels more closely aligned to the emerging needs and creating entertainment-on-the-go Movies and for our dynamic audiences. -
(West Tibet) Mafic Rocks and Granite Resulting from Cretaceous Jinsha Subduction
*Highlights • Lungmu Co (west Tibet) mafic rocks and granite resulting from Cretaceous Jinsha subduction. • Cooling in the early Upper Cretaceous and final exhumation in Paleocene. • Paleocene NW Tibet uplift as a far field effect of India/Eurasia collision. *Graphical Abstract Section A Field observations S 7000 K1C11 Active LMC fault K1C21 6500 LMC fault zone Mangtsa leucogranite K1C20 80°E8 81°E 116.9±1 Ma 6000 0°E 50 km ? Altitude (m) Tianshuihai 5500 N 5000 Aksai Gozha L. 35°N Chin KUNLUN BLOCK 2 km ult a fa ozh GGozha fault Mafic rocks geochemistry 35°N 1000.0 B 100.0 Lo e qzung Rang 10.0 KunKun LLunun BBlocklock 1.0 TianshuihaiTianshuihai terraneterrane Lungmu Co samples/MOR 0.1 Ba Rb K Th Ta Nb La Ce P Nd Sm Zr Hf Eu Ti Tb Dy Y Y b Cretaceous supra subduction setting lt fau QiangQQiangQiaianngg TangT TangTaanngg BlockB BlockBlolockck u Co FIg.2a gm K1L38 -50 LungmuLunLungmu Co LungmuCo fault fault Co Range 900 Upper Cretaceous magmatism andcoolingK1L26 K1L25 K1L24 800 Cooling history34°N QIANGTANG BLOCKU/Pb zircon - volcanic rock U/Pb zircon - plutonic rock 700 Ar/Ar muscovite biotite K-feldsparPaleocene cooling K1L17 K1C21 6 00 U/He zircon apatite linked with Tibet uplift Quaternary K89G181 500Fault Ice cap K1C11 slow cooling since ~55 Ma East LungmuCenozoic Co range 400 Lake K1C20 Temperature (°C) structural K1C20 Cretaceous 300 mu Northwest Tibet trend Jurassic 200 K1L24 River1 K1C21 Triasic 100granite K1L23 2 Road India-Asia Deformationin Paleozoic Carboniferous-Permian 0 collision northernTibet 0 5 0152025303540 45 50 55 60 65 70 75 80 85 90 95 100 105110120 KunLun bock QiangTang block Time (Ma) *Manuscript Click here to view linked References p.1 1 1 Successive deformation episodes along the Lungmu Co zone, west-central 2 3 2 Tibet.