DOCSLIB.ORG

A Petrographic, Geochemical and Geochronological

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
A Petrographic, Geochemical and Geochronological A petrographic, geochemical and geochronological investigation of deformed granitoids from SW Rajasthan: Neoproterozoic age of formation and evidence of Pan-African imprint By ANIKA M. SOLANKI Supervisor: PROF. L. D. ASHWAL DISSERTATION Submitted in fulfilment of the requirements for the degree MAGISTER SCIENTAE in GEOLOGY in the SCHOOL OF GEOSCIENCES, FACULTY OF SCIENCE at the UNIVERSITY OF THE WITWATERSRAND JOHANNESBURG JUNE, 2011 DECLARATION I, Anika. M. Solanki, declare that this dissertation thesis is my own, unaided work. It is being submitted for the degree of Master of Science in the University of the Witwatersrand, Johannesburg. It has not been submitted before for any degree or examination in any other university. (Signature of candidate) 21 day of June 2011 ii Page ABSTRACT Granitoid intrusions are numerous in southwestern Rajasthan and are useful because they can provide geochronological constraints on tectonic activity and geodynamic conditions operating as the time of intrusion, as well as information about deeper crustal sources. The particularly voluminous Neoproterozoic felsic magmatism in the Sirohi region of Rajasthan is of particular interest as it may have implications for supercontinental (Rodinia and Gondwana) geometry. The Mt. Abu granitoid pluton is located between two major felsic suites, the older (~870-800 Ma) Erinpura granite and the younger (~751-771 Ma) Malani Igneous Suite (MIS). The Erinpura granite is syn- to late- orogenic and formed during the Delhi orogeny, while the MIS is classified as alkaline, anorogenic and either rift- or plume-related. This tectonic setting is contentious, as recent authors have proposed formation within an Andean-type arc setting. The Mt. Abu granitoid pluton has been mapped as partly Erinpura (deformed textural variant) and partly younger MIS (undeformed massive pink granite). As the tectonic settings of the two terranes are not compatible, confusion arises as to the classification of the Mt. Abu granitoid pluton. Poorly-constrained Rb-Sr age dating place the age of formation anywhere between 735 ± 15 and 800 ± 50 Ma. The older age is taken as evidence that the Mt. Abu intrusion was either a late phase of the Erinpura granite. However, U-Pb zircon geochronology clearly indicates that the Mt. Abu felsic pluton is not related to- or contiguous with- the Erinpura granite suite. The major results from this study indicate that the all textural variants within the Mt. Abu pluton were formed coevally at ~765 Ma. Samples of massive pink granite, mafic-foliated granite and augen gneiss from the pluton were dated using U-Pb zircon ID-TIMS at 766.0 ± 4.3 Ma, 763.2 ± 2.7 Ma and 767.7 ± 2.3 Ma, respectively. The simple Mt. Abu pluton is considered as an enriched intermediate I- to A-type intrusion. They are not anorogenic A-types, as, although these felsic rocks have high overall alkali and incompatible element enrichment, no phase in the Mt. Abu pluton contains alkali rich amphibole or pyroxene, nor do REE diagrams for the most enriched samples show the gull-wing shape typical of highly evolved alkaline phases. The alkali-enriched magma may be explained by partial melting of a crustal source such as the high-K meta- igneous (andesite) one suggested by Roberts & Clemens (1993), not derivation from a mantle-derived mafic magma. The fairly restricted composition of Mt. Abu granitoids suggests that partial melting and a degree of assimilation/mixing may have been the major factors affecting the evolution of this granitoid pluton; fractional crystallization was not the major control on evolution of these granitoids. Revdar Rd. granitoids that are similar in outcrop appearance and petrography to Mt. Abu granitoids also conform to Mt. Abu granitoids geochemically and are classified as part of the Mt. Abu felsic pluton. Mt. Abu samples from this study have a maximum age range of 760.5-770 Ma, placing the Mt. Abu pluton within the time limits of the Malani Igneous Suite (MIS) as well as ~750 Ma granitoids from the Seychelles. Ages of the Sindreth-Punagarh Groups are also similar. These mafic-ultramafic volcanics are thought to be remnants of an ophiolitic mélange within a back-arc basin setting at ~750-770 Ma. The three Indian terranes are spatially and temporally contiguous. The same contiguity in space and time has been demonstrated by robust paleomagnetic data for the Seychelles and MIS. These similarities imply formation within a common geological event, the proposed Andean-type arc (Ashwal et al., 2002) on the western outboard of Rodinia. The implications are that peninsular India did not become a coherent entity until after this Neoproterozoic magmatism; Rodinia was not a static supercontinent that was completely amalgamated by 750 Ma, as subduction was occurring here simultaneous with rifting elsewhere. iii Page The Mt. Abu pluton has undergone deformation, with much of the pluton having foliated or augen gneiss textures. The timing of some of the deformation, particularly the augen gneiss and shear zone deformation, is thought to have occurred during intrusion. The Mt. Abu and Erinpura granitoids have experienced a common regional metamorphic event, as hornblende (Mt. Abu) and biotite (Erinpura) give 40 Ar/ 39 Ar ages of 508.7 ± 4.4 Ma and 515.7 ± 4.5 Ma, respectively. This event may have reactivated older deformatory trends as well. The temperature of resetting of argon in hornblende coincides with temperatures experienced during upper-greenschist to lower-amphibolite facies metamorphism. These late Pan-African ages are the first such ages reported for the Sirohi region and southern part of the Aravalli mountain range. They offer evidence for the extension of Pan-African amalgamation tectonics (evidence from southern India) into NW India. The age of formation of the Erinpura augen gneiss magma is 880.5 ± 2.1 Ma, thus placing the Erinpura granitoids within the age limits of the Delhi orogeny (~900-800 Ma; Bhushan, 1995). Most deformation observed here would have been caused by compression during intrusion. The Erinpura granitoids are S-type granitoids due to their predominantly peraluminous nature, restricted SiO 2-content, normative corundum and the presence of Al-rich muscovite and sillimanite in the mode. Weathered argillaceous metasedimentary material may also have been incorporated in this magma, while the presence of inherited cores suggests relatively lower temperatures of formation for these granitoids as compared to the Mt. Abu granitoids. The age of inheritance (1971 ± 23 Ma) in the Erinpura augen gneiss is taken as the age of the source component, which coincides with Aravalli SG formation. The Sumerpur granitoids differ from the Erinpura granitoids in terms of macroscopic and microscopic texture (undeformed, rarely megaporphyritic) but conform geochemically to the Erinpura granitoid characteristics and may thus be related to the Erinpura granitoid suite.The Revdar Rd. granitoids that are similar in macroscopic appearance to Erinpura granitoids also conform geochemically, and may similarly belong to the Erinpura granite suite. A Revdar Rd. mylonite gneiss with the Erinpura granitoids’ geochemical signature was dated at ~841 Ma, which does not conform to the age of the type-locality Erinpura augen gneiss dated here, but later intrusion within the same event cannot be ruled out because of the uncertainty in the age data (~21 Ma). The presence of garnet in one Revdar Rd. (Erinpura-type) sample implies generation of these granitoids at depth and/or entrainment from the source, similar to the S-type Erinpura granitoids. The Ranakpur granitoids differ significantly from both the Erinpura and Mt. Abu intrusives due to their low SiO 2-content and steep REE profiles (garnet present in the source magma); they are thought to have been generated under higher pressures from a more primitive source. The deeper pressure of generation is confirmed by the absence of a negative Eu-anomaly. The Ranakpur quartz syenite dated at 848.1 ± 7.1 Ma is younger by ~30 m.y. than the Erinpura augen gneiss. It is within the same time range as numerous other granitoids from this region as well as the Revdar Rd. granitoid dated in this study. The prevalence of 830- 840 Ma ages may indicate that a major tectonic event occurred at this time. The Ranakpur quartz syenite may have been generated near a subduction or collision zone, where thickened crust allows for magma generation at depth. The deeply developed Nb-anomaly in the spider diagram also implies a larger subduction component to the magma. The Swarupganj Rd. monzogranite is interpreted to have formed by high degrees of partial melting from a depleted crustal source and is dissimilar to other granitoids from this study. More sampling, geochemical and geochronological work needs to be done in order to characterize this intrusion. iv Page The Kishengarh nepheline syenite gneiss is situated in the North Delhi Fold Belt and is the oldest sample dated within this study. The deformation in this sample is due to arc- or continental- collision during a Grenvillian-type orogeny related to the amalgamation of the Rodinia supercontinent (and peninsular India), dated by the highly reset zircons at ~990 Ma. This is considered a DARC (deformed alkaline rock and carbonatite) and represents a suture zone (Leelanandam et al., 2006). The primary age of formation of this DARC is older than 1365 ± 99 Ma, which is the age of xenocrystic titanites from the sample. The granitoid rocks from this study area (Sirohi region) range widely in outcrop appearance, petrography
Load more

Recommended publications
  • Ethano-Medicinal Use of Plants of Mount Abu Region
    Ethano-medicinal use of plants of Mount Abu Region 1Ashwini Kumar Sharma and 2 G.S. Indoriya 1Associate Professor, P.G.Department of Dravyaguna M.M.M. Government Ayurvedic College, Udaipur, Rajasthan Email: [email protected] 2Dean and Principal Madhav Ayurvedic Medical College, Madhav University, Abu Road, Distt. Sirohi, Rajasthan Abstract The highest peak of Mount Abu is Guru Shikhar at 1722 m (5,650 ft) above sea level. The area is botanically the most important part of the Rajasthan. Here the climate is more humid and environmental conditions are quite favorable for the growth of natural vegetation. The slopes and base (Foot hills) including the plateau are covered with mixed deciduous forest, sprinkled with evergreen species. The main tribes of the study area are Bhil, Meena, Garasia and Kathodi, which form 12% of the total population of the state. The paper reviews the ethano medicinal uses of 15 plant species of Mount Abu, Rajasthan, used by the traditional practitioners. These hill ranges possess an abundant population of various tribes. Keywords: Abu, Evergreen Species, Ethno medicine. Introduction Abu varies greatly from the foot hills to high altitude. Average rainfall in Mount Abu is 1500 mm (2). Collection of medicinal plants from different Mount Abu Southern region of Rajasthan includes mainly Mt. Abu, regions has been a common practice among indigenous Sirohi, Kumbalgarh, Dungarpur, Parasramji, Udaipur people and medical practitioners. The vegetation of and Banswara(1). Mount Abu is referred to as 'an oasis Mount Abu supports dry deciduous, semi-deciduous and in the desert' as its heights are home to rivers, lakes, evergreen species, which changes with the increase in waterfalls and evergreen forests .The climate of Mount altitude (3).
    [Show full text]
  • Csc Project in Rajasthan
    Nov. 18, 2011 FINAL RFP DOCUMENT FOR THE SELECTION OF SCAs FOR CSC PROJECT IN RAJASTHAN Request for Proposal (RFP) Document for the Selection of Service Centre Agencies (SCAs) for Common Service Centre (CSC) Project in the State of Rajasthan [Reference No. F4.2 (03)/RISL/Tech/2011] Place of submission of the bid proposal RajCOMP Info Services Ltd., Jaipur (Raj.) Date & Time of Pre‐bid meeting 02/11/2011 at 1500 hrs. Last Date & Time of Submission of Bid 16/12/2011 up to 1430 hrs. Date & Time of Opening of Technical Bids 16/12/2011 at 1600 hrs. Cost of Tender Document: Rs. 5,000/-(Rupees Five Thousand Only) Name of the Company/ Firm: Address for the Correspondence: Telephone No.: Fax No.: E‐Mail: Issued By RajCOMP Info Services Limited (RISL) C‐Block, Yojana Bhawan, Tilak Marg, C‐Scheme, Jaipur‐302005 (Raj), INDIA Phone: 91(141) Fax: 91(141) Web: http://www.rajcomp.net, Email: [email protected] On Behalf Of Department of Information Technology & Communications (DoIT&C) Government of Rajasthan Page: 1 of 189 RajCOMP Info Services Limited (RISL) Bidder’s Seal & Signature Nov. 18, 2011 FINAL RFP DOCUMENT FOR THE SELECTION OF SCAs FOR CSC PROJECT IN RAJASTHAN TABLE OF CONTENTS S.No. Chapter Page 1. Abbreviations & Definitions 3 2. Invitation for Bids 5 3. Eligibility Criteria 9 4. Project Profile 12 5. Stakeholder’s Roles & Responsibilities 24 6. Overview of Suggested IT Architecture 34 7. Operational Guidelines for SCA 45 8. Time Schedule & Payment Terms 52 9. Service Level Standards 61 10. Bidding Process 69 11.
    [Show full text]
  • THE LOCUS Kumbharia Is a Small Sleepy Place Nestling in the Ridges
    KUiyiBHARIA - THE LOCUS Kumbharia is a small sleepy place nestling in the ridges of Aravallis as they terminate towards the south. Apart from the natural beauty that its location endows upon it, the Jaina shrines located there make it attractive and important. Culturally too the region is significant. This is the region where the two cultures Gujarati and Rajasthani meet and mingle. And Kumbharia, is in a manner of speaking, presided over by yet another trend-Jainism. It is this location, this openness to intermingling that makes the temples of Kumbharia interesting. There is a fourth dimension as well. The region comprising of Ambaji (Abu Road) and Kumbharia was known as Arasana in medieval times. This name is obviously derived from the huge marble hills in which it abounds. 'Aras' is the name by which marble is known in Gujarati. This stone w^is exported from here and almost every struc- ture of note here is built of marble-it being the locally available stone. Mythological literature offers a number of explanations regarding the origin of the name but most of them are far-fetched and there is no reason why the most logical derivation from geographical and geological peculiari- ties should be set aside. So it is a 'Land of marble' - Arasana. Fig. 1 Kumbharia, called Arasana as stated above, lies in the modem Banaskantha district of Gujarat. It is situated about 22 km. southeast of Abu Railway station on the Ajmer- Ahmedabad section of the Western Railway. From Abu Road this distance of 22 km. can be covered up by buses, taxis which ply' between Abu Road Ambaji and Ambaji Koteswar via Kumbharia temples.
    [Show full text]
  • Green Energy Corridor and Grid Strengthening Project
    Initial Environmental Examination (Draft) September 2015 IND: Green Energy Corridor and Grid Strengthening Project Prepared by Power Grid Corporation of India Limited for the Asian Development Bank. This 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. Your attention is directed to the “terms of use” section on ADB’s website. In preparing any country program or strategy, financing any project, or by making any designation of or reference to a particular territory or geographic area in this document, the Asian Development Bank does not intend to make any judgments as to the legal or other status of any territory or area. Initial Environmental Examination (Draft) for Project 44426-016 (IND): Green Energy Corridor and Grid Strengthening Project 03 September 2015 Prepared by Power Grid Corporation of India Ltd. for the Asian Development Bank 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. Table of Contents S.No. Page No. EXECUTIVE SUMMARY 1 1.0 INTRODUCTION 3 1.1 BACKGROUND 3 1.2 THE PROJECT 3 2.0 POLICY, LEGAL AND ADMINISTRATIVE FRAMEWORK 6 2.1 NATIONAL ENVIRONMENTAL REQUIREMENTS 6 2.2 POWERGRID’S ENVIRONMENTAL AND SOCIAL AND POLICY AND 8 PROCEDURES (ESPP) 2.3 ASIAN DEVELOPMENT BANK’S ENVIRONMENTAL REQUIREMENTS 9
    [Show full text]
  • District Survey Report of Jalore District 1.0 Introduction
    District Survey report of Jalore District 1.0 Introduction The district derives its name from the town of Jalore, which is the headquarters of the district administration. District is located between latitudes 24º 37’ 00” to 25º 49’ 00” and longitudes 71º 11’00” to 73º 05’00” with an area of 10,640 Sq. kms (3.11% of the State). The district is part of Jodhpur Division. The district is composed of five sub-divisions viz. Jalore, Ahore, Bhinmal, Sanchore, Raniwara which cover seven tehsils viz: Jalore, Ahore, Bhinmal, Sanchore, Raniwara, Sayala, Bagora and seven blocks viz: Jalore, Ahore, Bhinmal, Sanchore, Raniwara, Sayala & Jaswantpura. Total number of villages in the district is 802 and it also has 3 urban towns. Total population of the district as per Census 2011 is 1828730 with male and female population of 936634 and 892096 respectively. Administrative divisions of Jalore district are depicted in the index map (Fig. 1). 2.0 Rainfall & Climate Average annual rainfall (1971-2012) of the district is 445.4 mm. However normal rainfall for the period 1901 to 1970 is 400.6 mm. The annual rainfall gradually decreases from southeastern part to northwestern part. Climate of the district is dry except during SW monsoon season. The cold season is from December to February and is followed by summer from March to June. Period from mid of September to end of November constitutes post monsoon season. The district experiences either mild or normal drought once in two years. Severe type of drought has been recorded at Ahore block. Most severe type of drought has been recorded at Bhinmal, Sanchore & Jaswantpura blocks.
    [Show full text]
  • Hydro-Geology, Groundwater Resources and Analysis of Potential Aquifers in Malani Igneous Suite- a Case Study of Sirohi District of Rajasthan
    International Journal of Civil Engineering and Technology (IJCIET) Volume 7, Issue 6, November-December 2016, pp. 106–114, Article ID: IJCIET_07_06_012 Available online at http://iaeme.com/Home/issue/IJCIET?Volume=7&Issue=6 ISSN Print: 0976-6308 and ISSN Online: 0976-6316 © IAEME Publication HYDRO-GEOLOGY, GROUNDWATER RESOURCES AND ANALYSIS OF POTENTIAL AQUIFERS IN MALANI IGNEOUS SUITE- A CASE STUDY OF SIROHI DISTRICT OF RAJASTHAN Sen Hemant Research Scholar Department of Geology, M.L.S. University, Udaipur, Rajasthan, India Nagori M. L. Professor, Department of Geology, M.L.S. University, Udaipur, Rajasthan, India ABSTRACT Sustainable Groundwater Resources Management is t he need of the time and this aspect become crucial i n t h e w estern desertic t er rain o f R ajasthan which w itness s ca nty r ainfall. Sirohi district i s a lso a p art o f Ma lani I gneous S uite ( MIS ) a nd i n t h e d istrict MIS i s r epresented by Granites, Rhyolites and Igneous tuffs. The Main litho-units exposed in the district are Phyllites, Schists, Granite, Rhyolite, Gneisses and Alluvium. The Potential aquifers in the district are Rhyolite, Granite, Erinpura Granite, Gneisses, Phyllite and Schists. Analysis of rainfall pattern between the periods (year 2011 to 2013) reveals that there is significant year wise fluctuation in rainfall which affect groundwater recharge. Moreover t he a reas co vered w ith f air veg etation r eceive m ore r ains a s co mpared to non- vegetation portions. This is clearly witness in Mt.
    [Show full text]
  • Tom Abstraktow 6B-Ost Ver Publ.Pdf
    Cover photo: A euhedral, oscillatory zoned, primary monazite has been altered at the rims and along cracks to an allanite-apatite-xenotime assemblage. The host mineral is feldspar. Granite, Strzegom Massif. Workshop on accessory minerals, University of Warsaw, September 2014 Editors of Volume Bogusław BAGIŃSKI, Oliwia GRAFKA Witold MATYSZCZAK, Ray MACDONALD Institute of Geochemistry, Mineralogy and Petrology, University of Warsaw Al. Żwirki i Wigury 93, 02-089 Warszawa [email protected] Language correction: Ray MACDONALD Institute of Geochemistry, Mineralogy and Petrology, University of Warsaw Al. Żwirki i Wigury 93, 02-089 Warszawa [email protected] 1 Organizing committee: Bogusław BAGIŃSKI Ray MACDONALD Michał RUSZKOWSKI Financial support: Workshop on accessory minerals was financially supported by the Polish Ministry of Science and Higher Education subvention and research grant No N N307634040, Faculty of Geology University of Warsaw and PIG-PIB. 2 Workshop on accessory minerals, University of Warsaw, September 2014 Preface The progress made over the past two decades in our understanding of accessory minerals containing HFSE has been remarkable. Even when “fresh-minted”, minerals such as monazite, xenotime, allanite and zircon are compositionally and structurally complex. The complexity increases many times during low-temperature alteration processes, such as interaction with hydrothermal fluids and weathering. Progress has, of course, been expedited by the introduction of a range of exciting new technologies, especially in structure determinations. On re-reading the excellent 2002 review of accessory mineral research by Poitrasson et al., one is struck by how far the subject area has advanced in 12 years. We felt that this was an opportune time to bring together a group of Earth scientists with special expertise in accessory minerals to outline their current research interests, to share ideas and to consider productive future research directions.
    [Show full text]
  • Jalore Forest Division Management
    72°30'0"E 72°35'0"E 72°40'0"E 72°45'0"E 2 AHORE Bhagli 9 JALORE FOREST DIVISION 3 Dhavala Madalpura Rewat Khejarra Ka Dhani 10 Mera Uparla MANAGEMENT MAP 4 8 y a Bairath w h g i H N " e 0 t ' a 5 t N " 1 S ° Kolapura 0 ' 5 5 5 2 1 ° 5 Narnawas 2 Dakatra 7 y wa Narnawas gh Hi RAJANWADI AICHRANA e at St 6 Dhanpur Mank Bakra Road BAAGRA 1 Chunra Devda Gualpa Dhani Bagra 1 Maylawas BHETALA I Sarat Nabi Takhtpura NABI 1 1TAKHATPURA BHETALA JALOR Digaon Bhetala Santhu BHETALA II Dundsi 1 Nagni N " 0 ' 0 N " 1 ° 0 ' 5 0 2 1 Nun ° 5 2 1 Akoli AADWADA Arwara CHANDNA 1 1 Siyana SIYANA B Chandna Tatol Sargaro Ka Khera Gola SIYANA C Deldari 1 45/C/12 SIYANA A Bara Goga 1 BIBALSAR Bibalsar Umedgarh Lotiwara chhota Lotiwara mota y a w Kandar N SHEOGANJ h " Dewara g 0 i ' 5 H N " ° 0 5 e t ' 2 Chandna 5 a t ° 5 S 2 Naradra Satapura Raipuriya Sumergarh Siwana Sikwara Mondoli Bhutwas Manora WORKING CIRCLES LEGEND FOR MANAGEMENT MAP PROTECTED AREA / OTHER AREA NOT INCLUDED Varara BHINMAL GRASS & GRAZING WORKING CIRCLE PLANTATION WORKING CIRCLE Deldar Bhutgaon SOIL CONSERVATION & REHABILITATION WORKING CIRCLE DHOK IMPROVEMENT WORKING CIRCLE Ratpura Jhak Mandwariya MINING AREA IMPROVEMENT WORKING CIRCLE Jamotra OTHER WORKING CIRCLES Ramsin N " 0 ' 0 N " ° 0 5 ' 2 Legend 0 Barlut ° 5 2 Settlement points Sujapura Kolar Punag Kalan Drainge Line Jawal Jawal Railway Line Punag Khurd SIROHI S District Road ta te H ig h National Highway w Nawara a Bugaon Bawli y RECORDED State Highway BLOCK LEGAL STATUS TOPOSHEET Gurha AREA (HA) AADWADA PROTECTED 133.29 45C12 Ud District Boundary Bithan BAAGRA PROTECTED 99.43 45C12 Rivers/Waterbodies BHETALA I PROTECTED 108 45C12 BHETALA II PROTECTED 86 45C12 SOURCE INFORMATION Marwara Tehsil Boundary BIBALSAR PROTECTED 20.17 45C12 Baitarna BLOCK BOUNDARIES BASED ON STOCK MAPS CHANDNA PROTECTED 16.76 45C12 BLOCK BOUNDARIES BASED ON CADASTRAL MAPS ! ! ! ! ! ! ! ! SOI Sheet No.
    [Show full text]
  • C1-27072018-Section
    TATA CHEMICALS LIMITED LIST OF OUTSTANDING WARRANTS AS ON 27-08-2018. Sr. No. First Name Middle Name Last Name Address Pincode Folio / BENACC Amount 1 A RADHA LAXMI 106/1, THOMSAN RAOD, RAILWAY QTRS, MINTO ROAD, NEW DELHI DELHI 110002 00C11204470000012140 242.00 2 A T SRIDHAR 248 VIKAS KUNJ VIKASPURI NEW DELHI 110018 0000000000C1A0123021 2,200.00 3 A N PAREEKH 28 GREATER KAILASH ENCLAVE-I NEW DELHI 110048 0000000000C1A0123702 1,628.00 4 A K THAPAR C/O THAPAR ISPAT LTD B-47 PHASE VII FOCAL POINT LUDHIANA NR CONTAINER FRT STN 141010 0000000000C1A0035110 1,760.00 5 A S OSAHAN 545 BASANT AVENUE AMRITSAR 143001 0000000000C1A0035260 1,210.00 6 A K AGARWAL P T C P LTD AISHBAGH LUCKNOW 226004 0000000000C1A0035071 1,760.00 7 A R BHANDARI 49 VIDYUT ABHIYANTA COLONY MALVIYA NAGAR JAIPUR RAJASTHAN 302017 0000IN30001110438445 2,750.00 8 A Y SAWANT 20 SHIVNAGAR SOCIETY GHATLODIA AHMEDABAD 380061 0000000000C1A0054845 22.00 9 A ROSALIND MARITA 505, BHASKARA T.I.F.R.HSG.COMPLEX HOMI BHABHA ROAD BOMBAY 400005 0000000000C1A0035242 1,760.00 10 A G DESHPANDE 9/146, SHREE PARLESHWAR SOC., SHANHAJI RAJE MARG., VILE PARLE EAST, MUMBAI 400020 0000000000C1A0115029 550.00 11 A P PARAMESHWARAN 91/0086 21/276, TATA BLDG. SION EAST MUMBAI 400022 0000000000C1A0025898 15,136.00 12 A D KODLIKAR BLDG NO 58 R NO 1861 NEHRU NAGAR KURLA EAST MUMBAI 400024 0000000000C1A0112842 2,200.00 13 A RSEGU ALAUDEEN C 204 ASHISH TIRUPATI APTS B DESAI ROAD BOMBAY 400026 0000000000C1A0054466 3,520.00 14 A K DINESH 204 ST THOMAS SQUARE DIWANMAN NAVYUG NAGAR VASAI WEST MAHARASHTRA THANA
    [Show full text]
  • Land Bank Report
    RAW LAND BANK REPORT Rajasthan State Industrial Development & Investment Corporation Ltd. Udyog Bhawan, Tilak Marg, Jaipur, Rajasthan, INDIA Phone : 91-141-5113200 (Office) Email : [email protected]. 30-Sep-2021 Disclaimer : The information contained on this site is not to be construed or used as a "legal descriprion". Map Information is believed to be accurate but accuracy is not guaranteed. Any errors or omissions should be reported to RIICO through email: [email protected] or Telephone: +91-141-5113366. In no event will RIICO be liable for any damages, including loss of data, lost profits, business interruption, loss of business information or other pecuniary loss that might arise from the use of the maps or information on this web site. page 1 / 4 District Unit Office Raw Land Bank Name Total Area( Hectares ) AJMER AJMER Raghunathpura (Arai) 21.97 Bewanja 72.12 District - AJMER Total Area - 2 Industrial Area(s) 94.09 Unit Office AJMER Total Area 94.09 Ajmer Ajmer Onkarpura (kekri) 13.77 District - Ajmer Total Area - 1 Industrial Area(s) 13.77 Unit Office Ajmer Total Area 13.77 BHILWARA Bhilwara Fatehpura 64.77 District - Bhilwara Total Area - 1 Industrial Area(s) 64.77 Unit Office BHILWARA Total Area 64.77 BUNDI Kota Kharayata 16.47 District - Kota Total Area - 1 Industrial Area(s) 16.47 Unit Office BUNDI Total Area 16.47 Banswara Banswara Kundiya 46.86 Bawaliyapada 25.83 District - Banswara Total Area - 2 Industrial Area(s) 72.69 Unit Office Banswara Total Area 72.69 Bundi Kota Talabgaon 26.07 Deroli 45.42 District - Kota Total
    [Show full text]
  • Hydrogeological Atlas of Rajasthan Pali District
    Pali District ` Hydrogeological Atlas of Rajasthan Pali District Contents: List of Plates Title Page No. Plate I Administrative Map 2 Plate II Topography 4 Plate III Rainfall Distribution 4 Plate IV Geological Map 6 Plate V Geomorphological Map 6 Plate VI Aquifer Map 8 Plate VII Stage of Ground Water Development (Block wise) 2011 8 Location of Exploratory and Ground Water Monitoring Plate VIII 10 Stations Depth to Water Level Plate IX 10 (Pre-Monsoon 2010) Water Table Elevation Plate X 12 (Pre-Monsoon 2010) Water Level Fluctuation Plate XI 12 (Pre-Post Monsoon 2010) Electrical Conductivity Distribution Plate XII 14 (Average Pre-Monsoon 2005-09) Chloride Distribution Plate XIII 14 (Average Pre-Monsoon 2005-09) Fluoride Distribution Plate XIV 16 (Average Pre-Monsoon 2005-09) Nitrate Distribution Plate XV 16 (Average Pre-Monsoon 2005-09) Plate XVI Depth to Bedrock 18 Plate XVII Map of Unconfined Aquifer 18 Glossary of terms 19 2013 ADMINISTRATIVE SETUP DISTRICT – PALI Location: Pali district is located in the central part of Rajasthan. It is bounded in the north by Nagaur district, in the east by Ajmer and Rajsamand districts, south by Udaipur and Sirohi districts and in the West by Jalor, Barmer and Jodhpur districts. It stretches between 24° 44' 35.60” to 26° 27' 44.54” north latitude and 72° 45' 57.82’’ to 74° 24' 25.28’’ east longitude covering area of 12,378.9 sq km. The district is part of ‘Luni River Basin’ and occupies the western slopes of Aravali range. Administrative Set-up: Pali district is administratively divided into ten blocks.
    [Show full text]
  • Open-File Report 2005-1235
    Prepared in cooperation with the Idaho Geological Survey and the Montana Bureau of Mines and Geology Spatial databases for the geology of the Northern Rocky Mountains - Idaho, Montana, and Washington By Michael L. Zientek, Pamela Dunlap Derkey, Robert J. Miller, J. Douglas Causey, Arthur A. Bookstrom, Mary H. Carlson, Gregory N. Green, Thomas P. Frost, David E. Boleneus, Karl V. Evans, Bradley S. Van Gosen, Anna B. Wilson, Jeremy C. Larsen, Helen Z. Kayser, William N. Kelley, and Kenneth C. Assmus Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government Open-File Report 2005-1235 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 2005 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS 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 Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. Contents Abstract .......................................................................................................................................................... 1 Introduction
    [Show full text]