Paleoenvironmental and Tectonic Reconstruction of the Lower

Total Page:16

File Type:pdf, Size:1020Kb

Paleoenvironmental and Tectonic Reconstruction of the Lower University of New Hampshire University of New Hampshire Scholars' Repository Doctoral Dissertations Student Scholarship Spring 2006 Paleoenvironmental and tectonic reconstruction of the lower Eocene Ghazij Formation and related units, Balochistan, Pakistan: Implication for India - Asia collision Intizar Hussain Khan University of New Hampshire, Durham Follow this and additional works at: https://scholars.unh.edu/dissertation Recommended Citation Khan, Intizar Hussain, "Paleoenvironmental and tectonic reconstruction of the lower Eocene Ghazij Formation and related units, Balochistan, Pakistan: Implication for India -Asia collision" (2006). Doctoral Dissertations. 318. https://scholars.unh.edu/dissertation/318 This Dissertation is brought to you for free and open access by the Student Scholarship at University of New Hampshire Scholars' Repository. It has been accepted for inclusion in Doctoral Dissertations by an authorized administrator of University of New Hampshire Scholars' Repository. For more information, please contact [email protected]. PALEOENVIRONMENTAL AND TECTONIC RECONSTRUCTION OF THE LOWER EOCENE GHAZIJ FORMATION AND RELATED UNITS, BALOCHISTAN, PAKISTAN; IMPLICATION FOR INDIA-ASIA COLLISION BY INTIZAR HUSSAIN KHAN Bachelor of Science University of Sindh, Jamshoro, Pakistan, 1974 Master of Science University of Sindh, Jamshoro, Pakistan, 1978 DISSERTATION Submitted to the University of New Hampshire in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy in Earth Sciences - Geology May, 2006 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. UMI Number: 3217426 INFORMATION TO USERS The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleed-through, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. ® UMI UMI Microform 3217426 Copyright 2006 by ProQuest Information and Learning Company. All rights reserved. This microform edition is protected against unauthorized copying under Title 17, United States Code. ProQuest Information and Learning Company 300 North Zeeb Road P.O. Box 1346 Ann Arbor, Ml 48106-1346 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. This dissertation has been examined and approved. C. .c_____ Dissertation Director. Dr. William C_ Clyde Associate Professor of Geolog) . University of New Hampshire. Dr. Wallace A. Bothner, Jr. Professor of Geology , University of New Hampshire. Dr. Philip D. Gingerich Professor of Geological Sciences Director, Museum of Paleontology, University of Michigan, Ann Arbor, Michigan. ___________ Dr. Jo Laird Associate Professor of Geology University of New Hampshire. .... Dr. ^M a th e w Davis Associate Professor of Hydrogeology, University of New Hampshire _________ Date Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. DEDICATION Dedicated to my mother and wife iii Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. ACKNOWLEDGEMENTS I am really indebted to Dr. William C. Clyde, my dissertation advisor whose technical help, guidance and continued assistance in every phase of my work and moral and financial support made this research possible. My sincere thanks go to Dr. Philip D. Gingerich for encouraging this research and introduced me to Dr. Clyde. I would like to thank the other committee members (Dr. Jo Laird, Dr. Wallace A. Bothner, and Dr. J. Matthew Davis) for providing constant encouragement and guidance throughout my time at UNH. I am indebted for the support of the faculty and staff of the UNH Earth Sciences department, especially Sue Clark and Linda Wrighstman for their help and cooperation during my study period at UNH. I also appreciated the fruitful discussions with Dr. Peter J. Thompson. I also appreciate the help and cooperation of the USGS personnel, especially Edward Johnson and Peter Warwick. I am grateful to the Geological Survey of Pakistan for logistic support during the fieldwork in Pakistan and my extended deputation to UNH for Ph.D. studies. I am grateful to Mr. Hassan Ghour and Mirza Talib Hussain (Director Generals) as well as Syed Ghazanfar Abbas, Abdul Latif Khan from the Geological Survey of Pakistan for encouragement and support for this study. Sincere thanks are due to M. Akram Bhatti, Raza Shah, Zahid Hussain and staff of the Gelogical Survey of Pakistan who helped me during my fieldwork especially in the northwestern tribal areas of Pakistan. I am really thankful to Mashkoor Malik and his parent for taking me into their home during the last few months of my study at UNH. This research was supported by the NSF grant EAR 9902905 to William C. Clyde and by a Dissertation Fellowship grant from the University of New Hampshire. iv Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. TABLE OF CONTENTS DEDICATION....................................................................................................................... iii ACKNOWLEDGEMENTS.................................................................................................. iv TABLE OF CONTENTS...................................................................................................... v LIST OF TABLES............................................................................................................... xi LIST OF FIGURES.............................................................................................................. xii ABSTRACT.......................................................................................................................... xvii CHAPTER PAGE I. INTRODUCTION......................................................................................................... 1 Study Objectives and Methodology .................................................................... 8 Facies Analysis ....................................................................................... 8 Paleocurrent Indicators .......................................................................... 9 Provenance Analysis ...............................................................................9 Background............................................................................................................ 10 Regional Geology and Stratigraphy ....................................................... 10 Ghazij Formation .....................................................................................................15 Aerial Distribution of the Ghazij Formation ........................................ 16 Stratigraphic Nomenclature and Previous Studies of the Ghazij Formation ........................................................................ 16 Nomenclature used in this study ................................................. 21 Paleontologic Studies ............................................................................. 22 Geochronology of the Ghazij Formation ............................................ 23 v Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. Age/Biostratigraphy 23 II. FACIES ANALYSIS OF THE GHAZIJ FORMATION..................................... 25 Lower Part of the Ghazij Formation ................................................................ 26 Description and Interpretation of Facies .............................................. 26 Mudrock Facies (Lower Ghazij) ......................................................... 27 Description ................................................................................... 27 Depositional Environments ......................................................... 28 Sandstone Facies I (Lower Ghazij)....................................................... 28 Description ................................................................................... 28 Depositional Environments .......................................................... 31 Kach Sequence ......................................................................................... 31 Description ................................................................................... 31 Depositional Environments .......................................................... 32 Limestone and Marl Facies (Lower Ghazij) .......................................... 33 Description ................................................................................... 33 Depositional Environments .......................................................... 33 Middle Part of the Ghazij Formation .................................................................. 33 Description and Interpretation of Facies .............................................. 33 Mudrock Facies (Middle Ghazij) .......................................................... 34 Description ................................................................................... 34 Depositional Environments .......................................................... 35 Sandstone Facies of the Middle Ghazij ................................................ 35 Sandstone Facies
Recommended publications
  • Eocene to Miocene Composite Total Petroleum System, Irrawaddy-Andaman and North Burma Geologic Provinces, Myanmar
    Eocene to Miocene Composite Total Petroleum System, Irrawaddy-Andaman and North Burma Geologic Provinces, Myanmar By C.J. Wandrey Petroleum Systems and Related Geologic Studies in Region 8, South Asia Edited by Craig J. Wandrey U.S. Geological Survey Bulletin 2208–E U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior Gale A. Norton, Secretary U.S. Geological Survey P. Patrick Leahy, Acting Director U.S. Geological Survey, Reston, Virginia: 2006 Posted online February 2006 Version 1.0 This publication is only available online at http://www.usgs.gov/bul/2208/E/ For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Suggested citation: Wandrey, C.J., 2006, Eocene to Miocene Composite Total Petroleum System, Irrawaddy-Andaman and North Burma Geologic Provinces, Myanmar, Chapter E in Wandrey, C.J., ed., Petroleum systems and related geologic studies in Region 8, South Asia: U.S. Geological Survey Bulletin 2208-E, 26 p. iii Foreword This report describing the petroleum resources within a total petroleum system in Myan- mar was prepared as part of the World Energy Assessment Project of the U.S.
    [Show full text]
  • 1 89 Area & Population
    Table :- 1 89 AREA & POPULATION AREA, POPULATION AND POPULATION DENSITY OF PAKISTAN BY PROVINCE/ REGION 1961, 1972, 1981 & 1998 (Area in Sq. Km) (Population in 000) PAKISTAN /PROVINCE/ AREA POPULATION POPULATION DENSITY/Sq: Km REGION 1961 1972 1981 1998 1961 1972 1981 1998 Pakistan 796095 42880 65309 84254 132351 54 82 106 166 Total % Age 100.00 100.00 100.00 100.00 100.00 Sindh 140914 8367 14156 19029 30440 59 101 135 216 % Age share to country 17.70 19.51 21.68 22.59 23.00 Punjab 205345 25464 37607 47292 73621 124 183 230 358 % Age share to country 25.79 59.38 57.59 56.13 55.63 Khyber Pakhtunkhwa 74521 5731 8389 11061 17744 77 113 148 238 % Age share to country 9.36 13.37 12.84 13.13 13.41 Balochistan 347190 1353 2429 4332 6565 4 7 12 19 % Age share to country 43.61 3.16 3.72 5.14 4.96 FATA 27220 1847 2491 2199 3176 68 92 81 117 % Age share to country 3.42 4.31 3.81 2.61 2.40 Islamabad 906 118 238 340 805 130 263 375 889 % Age share to country 0.11 0.28 0.36 0.4 0.61 Source: - Population Census Organization, Government, of Pakistan, Islamabad Table :- 2 90 AREA & POPULATION AREA AND POPULATION BY SEX, SEX RATIO, POPULATION DENSITY, URBAN PROPORTION HOUSEHOLD SIZE AND ANNUAL GROWTH RATE OF BALOCHISTAN 1998 CENSUS Population Pop. Avg. Growth DIVISION / Area Sex Urban Pop. Both density H.H rate DISTRICT (Sq.km.) Male Female ratio Prop.
    [Show full text]
  • A Basal Lithostrotian Titanosaur (Dinosauria: Sauropoda) with a Complete Skull: Implications for the Evolution and Paleobiology of Titanosauria
    RESEARCH ARTICLE A Basal Lithostrotian Titanosaur (Dinosauria: Sauropoda) with a Complete Skull: Implications for the Evolution and Paleobiology of Titanosauria Rubén D. F. Martínez1*, Matthew C. Lamanna2, Fernando E. Novas3, Ryan C. Ridgely4, Gabriel A. Casal1, Javier E. Martínez5, Javier R. Vita6, Lawrence M. Witmer4 1 Laboratorio de Paleovertebrados, Universidad Nacional de la Patagonia San Juan Bosco, Comodoro Rivadavia, Chubut, Argentina, 2 Section of Vertebrate Paleontology, Carnegie Museum of Natural History, Pittsburgh, Pennsylvania, United States of America, 3 Laboratorio de Anatomía Comparada y Evolución de los Vertebrados, Museo Argentino de Ciencias Naturales, Buenos Aires, Argentina, 4 Department of Biomedical Sciences, Heritage College of Osteopathic Medicine, Ohio University, Athens, Ohio, United States of America, 5 Hospital Regional de Comodoro Rivadavia, Comodoro Rivadavia, Chubut, Argentina, 6 Resonancia Magnética Borelli, Comodoro Rivadavia, Chubut, Argentina * [email protected] OPEN ACCESS Citation: Martínez RDF, Lamanna MC, Novas FE, Ridgely RC, Casal GA, Martínez JE, et al. (2016) A Basal Lithostrotian Titanosaur (Dinosauria: Abstract Sauropoda) with a Complete Skull: Implications for the Evolution and Paleobiology of Titanosauria. PLoS We describe Sarmientosaurus musacchioi gen. et sp. nov., a titanosaurian sauropod dino- ONE 11(4): e0151661. doi:10.1371/journal. saur from the Upper Cretaceous (Cenomanian—Turonian) Lower Member of the Bajo Bar- pone.0151661 real Formation of southern Chubut Province in
    [Show full text]
  • Updated Stratigraphy and Mineral Potential of Sulaiman Basin, Pakistan
    Sindh Univ. Res. Jour. (Sci. Ser.) Vol.42 (2) 39-66 (2010) SURJ UPDATED STRATIGRAPHY AND MINERAL POTENTIAL OF SULAIMAN BASIN, PAKISTAN M. Sadiq Malkani Paleontology and Stratigraphy Branch, Geological Survey of Pakistan, Sariab Road, Quetta, Pakistan Abstract Sulaiman (Middle Indus) Basin represents Mesozoic and Cainozoic strata and have deposits of sedimentary minerals with radioactive and fuel minerals. The new coal deposits and showings, celestite, barite, fluorite, huge gypsum deposits, marble (limestone), silica sand, glauconitic and hematitic sandstone (iron and potash), clays, construction stone are being added here. Sulaiman Basin was previously ignored for updating of stratigraphy and economic mineral potential. Here most of known information on Sulaiman Basin is compiled and presented along with new economic deposits. Keywords: Stratigraphy, Mineral deposits, Sulaiman Basin, Middle Indus Basin, Pakistan. 1. Introduction metamorphic and sedimentary rocks. The study area is The Indus Basin which is a part of located in the central part of Pakistan (Fig.1a). Gondwanan lands (Southern Earth) is separated by an Previously, the Sulaiman Basin has received little Axial Belt (Suture Zone) from the Balochistan and attention, but this paper will add insights on updated Northern areas of Tethyan and Laurasian domains stratigraphy and new mineral discoveries. (northern earth). The Indus Basin (situated in the North-western part of Indo-Pakistan subcontinent) is 2. Materials and Methods located in the central and eastern part of Pakistan and The materials belong to collected field data, further subdivided in to upper (Kohat and Potwar), during many field seasons like lithology, structure, middle (Sulaiman) and Lower (Kirthar) basins. The stratigraphy and mineral commodities (Figs.
    [Show full text]
  • Himalaya to the Sea: Geology, Geomorphology and the Quaternary' by John F
    HIMALAYA, the Journal of the Association for Nepal and Himalayan Studies Volume 16 Number 1 Himalayan Research Bulletin No. 1 & Article 17 2 1996 Book review of 'Himalaya to the Sea: Geology, Geomorphology and the Quaternary' by John F. Shroder, Jr. (ed.) Daniel D. Schelling University of Utah Follow this and additional works at: https://digitalcommons.macalester.edu/himalaya Recommended Citation Schelling, Daniel D.. 1996. Book review of 'Himalaya to the Sea: Geology, Geomorphology and the Quaternary' by John F. Shroder, Jr. (ed.). HIMALAYA 16(1). Available at: https://digitalcommons.macalester.edu/himalaya/vol16/iss1/17 This Book Review is brought to you for free and open access by the DigitalCommons@Macalester College at DigitalCommons@Macalester College. It has been accepted for inclusion in HIMALAYA, the Journal of the Association for Nepal and Himalayan Studies by an authorized administrator of DigitalCommons@Macalester College. For more information, please contact [email protected]. William Fisher Harvard University Himalaya to the Sea: Geology, Geomorphology and the Quaternary. Edited by John F. Shroder, Jr. London, Routledge, 1993. Pp. xxvii + 429. $130.00 Located along the northwestern sector of the within the Himalayan region and South Asia (on which Himalayan continental-collision belt, the Kirthar­ many volumes have been published in recent years), and Sulaiman transform plate-boundary, and the eastern therefore the collection of papers in this volume will be sector of the Makran oceanic-subduction zone, Pakistan of interest to earth scientists working in a large number is one of the most tectonically active regions in the of tectonic, sedimentological and geomorphological world.
    [Show full text]
  • Geology of the Southern Gandghar Range and Kherimar Hills, Northern Pakistan
    AN ABSTRACT OF THE THESIS OF Michael D. Hylland for the degree of Master of Science in Geology presented on May 3. 1990 Title: Geology of the Southern Gandghar Range and Kherimar Hills. Northern Pakistan Abstract approved: RobeS. Yeats The Gandghar Range and Kherimar Hills, located in the Hill Ranges of northern Pakistan, contain rocks that are transitional between unmetarnorphosed foreland-basin strata to the south and high-grade metamorphic and plutonic rocks to the north. The southern Gandghar Range is composed of a succession of marine strata of probable Proterozoic age, consisting of a thick basal argillaceous sequence (Manki Formation) overlain by algal limestone and shale (Shahkot, Utch Khattak, and Shekhai formations). These strata are intruded by diabase dikes and sills that may correlate with the Panjal Volcanics. Southern Gandghar Range strata occur in two structural blocks juxtaposed along the Baghdarra fault. The hanging wall consists entirely of isoclinally-folded Manki Formation, whereas the footwall consists of the complete Manki-Shekhai succession which has been deformed into tight, northeast-plunging, generally southeast (foreland) verging disharmonic folds. Phyllite near the Baghdarra fault displays kink bands, a poorly-developed S-C fabric, and asymmetric deformation of foliation around garnet porphyroblasts. These features are consistent with conditions of dextral shear, indicating reverse-slip displacement along the fault. South of the Gandghar Range, the Panjal fault brings the Gandghar Range succession over the Kherimar Hills succession, which is composed of a basal Precambrian arenaceous sequence (Hazara Formation) unconformably overlain by Jurassic limestone (Samana Suk Formation) which in turn is unconformably overlain by Paleogene marine strata (Lockhart Limestone and Patala Formation).
    [Show full text]
  • Sibi District Education Plan (2016-17 to 2020-21)
    Sibi District Education Plan (2016-17 to 2020-21) Table of Contents LIST OF ACRONYMS 1 LIST OF FIGURES 3 LIST OF TABLES 4 1 INTRODUCTION 5 2 METHODOLOGY & PROCESS 7 2.1 METHODOLOGY 7 2.1.1 DESK RESEARCH 7 2.1.2 CONSULTATIONS 7 2.1.3 STAKEHOLDERS INVOLVEMENT 7 2.2 PROCESS FOR PLANS DEVELOPMENT: 8 2.2.1 SECTOR ANALYSIS: 8 2.2.2 IDENTIFICATION AND PRIORITIZATION OF STRATEGIES: 9 2.2.3 FINALIZATION OF DISTRICT PLANS: 9 3 SIBI DISTRICT PROFILE 10 3.1 POPULATION 11 3.2 ECONOMIC ENDOWMENTS 11 3.3 POVERTY & CHILD LABOR: 12 3.4 STATE OF EDUCATION 12 4 ACCESS & EQUITY 16 4.1 EQUITY AND INCLUSIVENESS 21 4.2 IMPORTANT FACTORS 22 4.2.1 SCHOOL AVAILABILITY AND UTILIZATION 22 4.2.2 MISSING FACILITIES AND SCHOOL ENVIRONMENT 24 4.2.3 POVERTY 24 4.2.4 PARENT’S ILLITERACY 24 4.2.5 ALTERNATE LEARNING PATH 25 4.3 OBJECTIVES AND STRATEGIES 26 5 DISASTER RISK REDUCTION 31 5.1 OBJECTIVES AND STRATEGIES 32 6 QUALITY AND RELEVANCE OF EDUCATION 33 6.1 SITUATION 33 6.2 DISTRICT LIMITATIONS AND STRENGTHS 34 6.3 OVERARCHING FACTORS FOR POOR EDUCATION 36 6.4 DISTRICT RELATED FACTORS OF POOR QUALITY 37 6.4.1 OWNERSHIP OF QUALITY IN EDUCATION 37 6.4.2 CAPACITY OF FIELD TEAMS 37 6.4.3 ACCOUNTABILITY MODEL OF HEAD TEACHERS 37 6.4.4 NO DATA COMPILATION AND FEEDBACK 37 6.4.5 CURRICULUM IMPLEMENTATION AND FEEDBACK 38 6.4.6 TEXTBOOKS DISTRIBUTION AND FEEDBACK 38 6.4.7 PROFESSIONAL DEVELOPMENT 38 6.4.8 TEACHERS AVAILABILITY 39 6.4.9 ASSESSMENTS 39 6.4.10 EARLY CHILDHOOD EDUCATION (ECE) 39 6.4.11 AVAILABILITY AND USE OF LIBRARIES & LABORATORIES 39 6.4.12 SCHOOL ENVIRONMENT 40
    [Show full text]
  • Mcdermott on Schaflechner, 'Hinglaj Devi: Identity, Change, and Solidification at a Hindu Temple in Pakistan'
    H-Asia McDermott on Schaflechner, 'Hinglaj Devi: Identity, Change, and Solidification at a Hindu Temple in Pakistan' Review published on Monday, July 15, 2019 Jürgen Schaflechner. Hinglaj Devi: Identity, Change, and Solidification at a Hindu Temple in Pakistan. Oxford: Oxford University Press, 2017. 360 pp. $99.00 (cloth), ISBN 978-0-19-085052-4. Reviewed by Rachel McDermott (Barnard College)Published on H-Asia (July, 2019) Commissioned by Sumit Guha (The University of Texas at Austin) Printable Version: http://www.h-net.org/reviews/showpdf.php?id=52255 I leapt at the chance to review this book. How many people study Hindu goddess traditions in Pakistan and in Balochistan? The photograph on the book jacket, of a family walking in the unending gray desert—one presumes, to Hinglaj Devi—conjures up inaccessibility, arduousness, and complete unfamiliarity. What might one learn about this goddess, claimed as one of the fifty-one Śākta pīṭhas, and what must it have been like to do the six years of fieldwork, 2009-15, that went into this study? Jürgen Schaflechner’s monograph and associated film are a magisterial, evocative achievement, and, as a Hindu goddesses scholar unlikely to travel to Pakistan, I feel profoundly grateful to him for his research. Hinglaj Devi: Identity, Change, and Solidification at a Hindu Temple in Pakistan is a book about change, meaning, contest, and hope, and one of the larger aims of the project is to challenge and undercut common assumptions about the Islamic Republic as being inimical to Hindus and Hindu spaces. As nineteenth-century colonial accounts attest, pilgrimage to the temple, which is north of the coast and west of Karachi, used to be a strenuous, punishing journey on foot, and the merit of the pilgrimage was commensurate with the austerity involved.
    [Show full text]
  • A Solar Developer's Guide to Pakistan
    A Solar Developer’s Guide to Pakistan IN PARTNERSHIP WITH: Acknowledgements This Guide was developed as part of the IFC Middle East and North Africa (MENA) Renewable Energy Development Support Advisory program, funded by AusAid, Japan, and The Netherlands for activities in Pakistan. The overall goal of this multi-year program is to enhance the scale up and development of renewable and clean energy in MENA by supporting developers and investors in MENA markets, increasing overall market awareness and understanding, and facilitating public-private dialogue. The Guide was prepared under the overall guidance of Bryanne Tait, IFC’s Regional Lead for Energy and Resource Efficiency Advisory, Middle East and North Africa. We acknowledge the significant contributions of Sohail Alam, IFC Energy Specialist and Alice Cowman, Renewable Energy Specialist, who has been commissioned by IFC to carry out the desk research, drafting and interviews. We would like to thank the Pakistan Alternative Energy Development Board, National Electric Power Regulatory Authority, National Transmission and Distribution Company, the Province of Punjab and the Province of Sindh, who contributed greatly to the research and study for this guide through interviews and provision of information and documents. IFC would also like to express its sincere appreciation to RIAA Barker Gillette, Ernst & Young, and Eversheds, who contributed to the drafting of the guide. Solar resource maps and GIS expertise were kindly provided by AWS Truepower and colleagues from the World Bank respectively, including support from the Energy Sector Management Assistance Program (ESMAP). Certain mapping data was obtained from OpenStreetMap, and copyright details for this can be found at http://www.openstreetmap.org/copyright.
    [Show full text]
  • Project Title to Be Centred
    Environmental Assessment Report Initial Environmental Examination Project Number: 37192 August 2009 PAK: Multitranche Financing Facility Power Transmission Enhancement Investment Program, Tranche 1 Sub Project No. 20 220 kV Dera Ghazi Khan - Loralai Double Circuit Transmission Line Subproject Prepared by National Transmission and Despatch Company for the Asian Development Bank (ADB). The initial environmental examination is a document of the borrower. The views expressed herein do not necessarily represent those of ADB’s Board of Directors, Management, or staff, and may be preliminary in nature. CURRENCY EQUIVALENTS (as of 30 May 2009) Currency Unit – Pakistan rupee/s (Pre/PRs) PRe1.00 = $.0080 $1.00 = PRs79.80 ABBREVIATIONS ADB – Asian Development Bank dB(decibel) – sound level measure EIA – environmental impact assessment EMP – environmental management plan IEC – International environmental consultants IEE – initial environmental examination LARP – land acquisition and resettlement plan MFF – Multitranche Financing Facility PCB – Polychlorinated biphenyls PEPA – Punjab Environmental Protection Agency PEPAct – Pakistan Environmental Protection Act 1997 (as regulated and amended) PMU – project management unit ROW – right of way WMP – waste management plan DEFINITIONS Barren Land – Land which has not been cultivated and was lying barren at the time of field survey for this IEE Cropped land – Land which was under agricultural crops at the time of field survey for this IEE. Landowner – Person(s) holding legal title to property on the electric transmission line route from whom the Company is seeking, or has obtained, a temporary or permanent easement, or any person(s) legally authorized by a landowner to make decisions regarding the mitigation or restoration of agricultural impacts to such landowner(s) property.
    [Show full text]
  • A New Giant Basal Titanosaur Sauropod in the Upper Cretaceous (Coniacian) of the Neuquen Basin, Argentina
    Cretaceous Research 100 (2019) 61e81 Contents lists available at ScienceDirect Cretaceous Research journal homepage: www.elsevier.com/locate/CretRes A new giant basal titanosaur sauropod in the Upper Cretaceous (Coniacian) of the Neuquen Basin, Argentina * Leonardo S. Filippi a, , Leonardo Salgado b, c, Alberto C. Garrido d, e a Museo Municipal Argentino Urquiza, Jujuy y Chaco s/n, 8319 Rincon de los Sauces, Neuquen, Argentina b CONICET, Argentina c Instituto de Investigacion en Paleobiología y Geología, Universidad Nacional de Río Negro-Conicet, Av. Gral. J. A. Roca 1242, 8332 General Roca, Río Negro, Argentina d Museo Provincial de Ciencias Naturales “Profesor Dr. Juan A. Olsacher”, Direccion Provincial de Minería, Etcheluz y Ejercito Argentino, 8340 Zapala, Neuquen, Argentina e Departamento Geología y Petroleo, Facultad de Ingeniería, Universidad Nacional del Comahue, Buenos Aires 1400, Neuquen 8300, provincia del Neuquen, Argentina article info abstract Article history: A new basal sauropod titanosaur, Kaijutitan maui gen. et sp. nov., is described. The holotype of this Received 21 November 2018 species, which comes from the Sierra Barrosa Formation (upper Coniacian, Upper Cretaceous), consists of Received in revised form cranial, axial, and appendicular elements presenting an unique combination of plesiomorphic and 3 February 2019 apomorphic characters. The most notable characteristic observed in Kaijutitan is the presence of anterior Accepted in revised form 9 March 2019 cervical vertebrae with bifid neural spines, a condition that would have evolved several times among Available online 28 March 2019 sauropods. The phylogenetic analysis places Kaijutitan as a basal titanosaur, the sister taxon of Epachthosaurus þ Eutitanosauria. The new species supports the coexistence, in the Late Cretaceous Keywords: Sauropoda (Turonian-Santonian), of basal titanosaurs and eutitanosaurian sauropods, at least in Patagonia.
    [Show full text]
  • The Situation of Religious Minorities
    writenet is a network of researchers and writers on human rights, forced migration, ethnic and political conflict WRITENET writenet is the resource base of practical management (uk) e-mail: [email protected] independent analysis PAKISTAN: THE SITUATION OF RELIGIOUS MINORITIES A Writenet Report by Shaun R. Gregory and Simon R. Valentine commissioned by United Nations High Commissioner for Refugees, Status Determination and Protection Information Section May 2009 Caveat: Writenet papers are prepared mainly on the basis of publicly available information, analysis and comment. All sources are cited. The papers are not, and do not purport to be, either exhaustive with regard to conditions in the country surveyed, or conclusive as to the merits of any particular claim to refugee status or asylum. The views expressed in the paper are those of the author and are not necessarily those of Writenet or UNHCR. TABLE OF CONTENTS Acronyms ................................................................................................... i Executive Summary ................................................................................. ii 1 Introduction........................................................................................1 2 Background.........................................................................................4 3 Religious Minorities in Pakistan: Understanding the Context......6 3.1 The Constitutional-Legal Context..............................................................6 3.2 The Socio-Religious Context .......................................................................8
    [Show full text]