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Country Geological
NEWSLETTER No. 44 - April, 1984 : Editorial : Over the years, pen poised over blank paper, I have sometimes had a wicked urge to write an ed- itorial on the problems of writing an editorial. For this issue I was asked to consider something on the low attendances at a few recent meetings and this would have been a sad topic. In the lic1^ meantime we have had two meetings with large at- tvndances, further renewed subscriptions, and various other problems solved. This leaves your Country editor much happier, and quite willing to ask you to keep it up = Geological This issue has been devoted mainly to the two long articles on the local limestone and its n !''} Q problems, so for this time the feature "From the Papers" is omitted. Next Meeting : Sunday April 15th : Field trip led by Tristram Besterman to Warwick and Nuneaton. Meet 10.00 a.m. at the Museum, Market Place, Warwick, The Museum will be open, allowing us to see the geological displays, some of the reserve collections, and the Geological Locality Record Centre. This will be followed by a visit to a quarry exposing the Bromsgrove Sandstone (Middle Triassic). In the afternoon it is proposed to visit the Nuneaton dis- trict to examine the Precambrian-Cambrian geology, and to see examples of site conservation. Meetings are held in the Allied Centre, Green Ilan Entry, Tower Street, Dudley, behind the Malt Shovel pub. Indoor meetings commence at 8 p.m. with coffee and biscuits (no charge) from 7.15 p.m. Field meetings will commence from outside the Allied Centre unlegs otherwise arranged. -
U–Pb Zircon (SHRIMP) Ages for the Lebombo Rhyolites, South Africa
Journal of the Geological Society, London, Vol. 161, 2004, pp. 547–550. Printed in Great Britain. 2000) and the ages corroborate and further strengthen the SPECIAL chronology of the Lebombo stratigraphy. The rapid eruption of the Karoo succession is thought to have been responsible for trigger- U–Pb zircon (SHRIMP) ing the early Toarcian extinction event (Hesselbo et al. 2000). Geological setting. The Karoo Supergroup succession along the ages for the Lebombo Lebombo monocline is highlighted in Figure 1. The oldest phase of Karoo volcanism is marked by the Mashikiri nephelinites, rhyolites, South Africa: which unconformably overlie Jurassic Clarens Formation sand- stones (Fig. 2). The nephelinites have been dated at 182.1 Æ refining the duration of 1.6 Ma (40Ar/39Ar plateau age; Duncan et al. 1997) and form a lava succession up to 170 m thick (Bristow 1984). These rocks Karoo volcanism are confined to the northern part of the Lebombo rift and are absent along the central and southern sections. The nephelinites T. R. RILEY1,I.L.MILLAR2, are conformably overlain by picrites and picritic basalts of the 3 1 Letaba Formation, although in the southern Lebombo the picrites M. K. WATKEYS ,M.L.CURTIS, directly overlie the Clarens Formation. The picrites overlap in 1 3 P. T. LEAT , M. B. KLAUSEN & age (182.7 Æ 0.8 Ma; Duncan et al. 1997) with the Mashikiri C. M. FANNING4 nephelinites and are believed to form a succession up to 4 km in thickness. 1British Antarctic Survey, High Cross, Madingley Road, The Letaba Formation picrites are in turn overlain by a major Cambridge, CB3 0ET, UK (e-mail: [email protected]) succession (4–5 km thick) of low-MgO basalts, termed the Sabie 2British Antarctic Survey c/o NERC Isotope Geosciences River Basalt Formation (Cleverly & Bristow 1979). -
Meso-Archaean and Palaeo-Proterozoic Sedimentary Sequence Stratigraphy of the Kaapvaal Craton
Marine and Petroleum Geology 33 (2012) 92e116 Contents lists available at SciVerse ScienceDirect Marine and Petroleum Geology journal homepage: www.elsevier.com/locate/marpetgeo Meso-Archaean and Palaeo-Proterozoic sedimentary sequence stratigraphy of the Kaapvaal Craton Adam J. Bumby a,*, Patrick G. Eriksson a, Octavian Catuneanu b, David R. Nelson c, Martin J. Rigby a,1 a Department of Geology, University of Pretoria, Pretoria 0002, South Africa b Department of Earth and Atmospheric Sciences, University of Alberta, Canada c SIMS Laboratory, School of Natural Sciences, University of Western Sydney, Hawkesbury Campus, Richmond, NSW 2753, Australia article info abstract Article history: The Kaapvaal Craton hosts a number of Precambrian sedimentary successions which were deposited Received 31 August 2010 between 3105 Ma (Dominion Group) and 1700 Ma (Waterberg Group) Although younger Precambrian Received in revised form sedimentary sequences outcrop within southern Africa, they are restricted either to the margins of the 27 September 2011 Kaapvaal Craton, or are underlain by orogenic belts off the edge of the craton. The basins considered in Accepted 30 September 2011 this work are those which host the Witwatersrand and Pongola, Ventersdorp, Transvaal and Waterberg Available online 8 October 2011 strata. Many of these basins can be considered to have formed as a response to reactivation along lineaments, which had initially formed by accretion processes during the amalgamation of the craton Keywords: Kaapvaal during the Mid-Archaean. Faulting along these lineaments controlled sedimentation either directly by Witwatersrand controlling the basin margins, or indirectly by controlling the sediment source areas. Other basins are Ventersdorp likely to be more controlled by thermal affects associated with mantle plumes. -
F Makwara (PDF)
CHROMITE GEOLOGY OF ZIMBABWE AND RELATED MINING CHALLENGES PRESENTATION GREAT DYKE : MUTORASHANGA AUGUST 2017 2 WORLD CHROME RESOURCE Estimate World Chromite Resource : +-12 Billion Tonnes • South Africa : 72% of world Resource - Stratiform • Zimbabwe: 12% -Stratiform & podiform • Kazakhstan: 4% - Podiform • Finland : 2% -Podiform • India : 1% -Podiform • Turkey and others : 9% -Largely podiform But Zimbabwe companies producing at full capacity is not in the top 5 producing companies . STRATIFORM & PODIFORM GEOLOGY LOCATION GEOLOGY MAP - ZIMBABWE MASHONALAND CENTRAL MASHONALAND WEST CHIRUMANZU MIDLANDS MASVINGO MBERENGWA 5 LOCATION OF STRATIFORM CHROMITE RESOURCE • Mashonaland Central: North Dyke Tengenenge Impinge Birkdale Mutorashanga • Mashonaland West: Middle Dyke Ngezi Darwendale Maryland Lembe/Mapinga Mutorashanga • Midlands: South Dyke Lalapanzi Mapanzure Bannockburn CSC LOCATION OF PODIFORM CHROMITE RESOURCES • Midlands: Valley Nhema Chirumanzu Mberengwa • Masvingo: Mashava THE GREAT DYKE AND PODIFORMS GEOLOGY • THE GREAT DYKE • Tengenenge to Mberengwa, Location • Stretches for 550km and is 4-11km wide. • PODIFORM • Isolated chrome resources in Shurugwi,Mashava ,Nhema ,Valley, Chirumanzu and Mberengwa • THE DYKE : STRATIFORM • Chromite hosts rocks are :Harzburgite, dunite, serpentinite and pyroxenite Host Rock • PODIFORM • Chromite host rocks are: Serpentinite ,Silicified Talc Carbonate and Talc Carbonate • 10 known seams, The 11 th seam is poorly exposed in the North Dyke • 8cm to 40cm thickness Chrome Seams • Average vertical spacing of seams is 30-40m • Geotechnical Parameters considered fore seams are: Seam Widths, quality, dip, friability, & continuity • Platinum Group Metals Known Minerals in • Chrome the Dyke • Asbestos • Nickel 8 CHROMITE RESOURCES • The dyke intruded as an ultramafic sill ,estimated age 2.7 Ga . STRATIFORM • 11 seams are known to exist on the Great Dyke, but not evenly distributed through out the dyke. -
Murchison in the Welsh Marches: a History of Geology Group Field Excursion Led by John Fuller, May 8 – 10 , 1998
ISSN 1750-855X (Print) ISSN 1750-8568 (Online) Murchison in the Welsh Marches: a History of Geology Group field excursion led by John Fuller, May 8th – 10th, 1998 John Fuller1 and Hugh Torrens2 FULLER, J.G.C.M. & TORRENS, H.S. (2010). Murchison in the Welsh Marches: a History of Geology Group field excursion led by John Fuller, May 8th – 10th, 1998. Proceedings of the Shropshire Geological Society, 15, 1– 16. Within the field area of the Welsh Marches, centred on Ludlow, the excursion considered the work of two pioneers of geology: Arthur Aikin (1773-1854) and Robert Townson (1762-1827), and the possible train of geological influence from Townson to Aikin, and Aikin to Murchison, leading to publication of the Silurian System in 1839. 12 Oak Tree Close, Rodmell Road, Tunbridge Wells TN2 5SS, UK. 2Madeley, Crewe, UK. E-mail: [email protected] "Upper Silurian" shading up into the Old Red Sandstone above, and a "Lower Silurian" shading BACKGROUND down into the basal "Cambrian" (Longmynd) The History of Geology Group (HOGG), one of below. The theoretical line of division between his the specialist groups within the Geological Society Upper and Lower Silurian ran vaguely across the of London, has organised a number of historical low ground of Central Shropshire from the trips in the past. One was to the area of the Welsh neighbourhood of the Craven Arms to Wellington, Marches, based at The Feathers in Ludlow, led by and along this line the rocks and faunas of the John Fuller in 1998 (8–10 May). -
Investigating Sexual Dimorphism in Ceratopsid Horncores
University of Calgary PRISM: University of Calgary's Digital Repository Graduate Studies The Vault: Electronic Theses and Dissertations 2013-01-25 Investigating Sexual Dimorphism in Ceratopsid Horncores Borkovic, Benjamin Borkovic, B. (2013). Investigating Sexual Dimorphism in Ceratopsid Horncores (Unpublished master's thesis). University of Calgary, Calgary, AB. doi:10.11575/PRISM/26635 http://hdl.handle.net/11023/498 master thesis University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Downloaded from PRISM: https://prism.ucalgary.ca UNIVERSITY OF CALGARY Investigating Sexual Dimorphism in Ceratopsid Horncores by Benjamin Borkovic A THESIS SUBMITTED TO THE FACULTY OF GRADUATE STUDIES IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE DEPARTMENT OF BIOLOGICAL SCIENCES CALGARY, ALBERTA JANUARY, 2013 © Benjamin Borkovic 2013 Abstract Evidence for sexual dimorphism was investigated in the horncores of two ceratopsid dinosaurs, Triceratops and Centrosaurus apertus. A review of studies of sexual dimorphism in the vertebrate fossil record revealed methods that were selected for use in ceratopsids. Mountain goats, bison, and pronghorn were selected as exemplar taxa for a proof of principle study that tested the selected methods, and informed and guided the investigation of sexual dimorphism in dinosaurs. Skulls of these exemplar taxa were measured in museum collections, and methods of analysing morphological variation were tested for their ability to demonstrate sexual dimorphism in their horns and horncores. -
Momentum Health Attakwas Presented by Biogen Finishers to Date (003).Xlsx
FINISHERS BY NAMES 2007 - 2018 RIDER 2007 2008 2009 2010 2011 2012 2013 2014 2015 2016 2017 2018 Total A Eksteen 1 1 Aaron Adler 1 1 Aaron Borrill 1 1 Aaron David 1 1 Abdallah Salie 1 1 Abdul-Gameed Salie 1 1 1 1 4 Abdullah Jaffar 11 2 Abraham Meyer 11 Abrie Du Plessis 11 Abrie Fouche 111 3 Abrie Van Tonder 11 Abu Veldsman 11 Adam Foster 1 1 Adam Pike 1 1 Adam Rampf 1 1 Adam Wooldridge 1 1 Adele Drake 1 1 Adele Niemand 1 1 Adele Zurnamer 1 1 Adiel Mohamed 1 1114 Adnan Essop 1 1 Adniaan Solomon 11 Adohan Van Den Berg 1 1 Adraain Lourens 1 1 Adriaan De Bruyn 1 1 Adriaan Jansen Van Vuuren 1 1 2 Adriaan Louw 11 11 4 Adriaan Pearson 1 1 Adriaan Steyn 11 Adriaan Strauss 1 1 Adrian Cooney 1 1 Adrian De Jonge 1 1 1 1 1 1 1 7 Adrian Enthoven 11 2 Adrian Fogg 11 2 Adrian Harris 11 Adrian Haupt 112 Adrian Hegerty 1 1 Adrian Hobbs 1 1 Adrian Smit 1 1 Adrian Vardy 1 1 2 Adriano Bertoncello 1 1 Adrien Niyonshuti 1 1 AHMED ZAID Mahomed 1 1 1 1 1 1 1 7 Aidan Van Niekerk 1 1 2 Aileen Anderson 11 2 Al Botha 1 1 Alan Botten 1 1 Alan Cotton 11 2 RIDER 2007 2008 2009 2010 2011 2012 2013 2014 2015 2016 2017 2018 Total Alan Crossley 1 1 Alan Dawson 1 1 Alan Haupt 1 1 Alan Macintosh 1 113 Alan Rees 11 2 Alan Rosewall 1 1 Alan Thomas 1 1 Alan Van Den Handel 1 1 Alan Van Schoor 1 1 Alana Smit 1 1 Alasdair Sholto-Douglas 1 1 Alastair Haarhoff 1 1 Alastair Hops 1111 4 Alastair Sellick 112 Albe Geldenhuys 1 1 2 Albert Bester 11 2 Albert Coetzee 1 1 Albert Kleynhans 11 Albert Pretorius 11 Albert Retief 1 1 2 Albert Rust 1 1 2 Albert Van Zyl 11 2 Alberto Prins 11 2 -
Zimbabwe (Sera) Program Mining Sector Policy Study
USAID STRATEGIC ECONOMIC RESEARCH AND ANALYSIS – ZIMBABWE (SERA) PROGRAM MINING SECTOR POLICY STUDY CONTRACT NO. AID-613-C-11-00001 This report was produced by Nathan Associates Inc. for review by the United States Agency for International Development (USAID). DECEMBER 2012 USAID STRATEGIC ECONOMIC RESEARCH AND ANALYSIS – ZIMBABWE (SERA) PROGRAM MINING SECTOR POLICY STUDY CONTRACT NO. AID-613-C-11-00001 Program Title: USAID Strategic Economic Research & Analysis – Zimbabwe (SERA) Sponsoring USAID Office: USAID/Zimbabwe Contract Number: AID-613-C-11-00001 Contractor: Nathan Associates Inc. Date of Publication: December 2012 Author: Paul Jourdan, Consultant Gibson Chigumira, ZEPARU Executive Director Isaac Kwesu, Zimbabwe Chamber of Mines Chief Economist Erina Chipumho, ZEPARU Senior Research Fellow DISCLAIMER This document is made possible by the support of the American people through USAID. Its contents are the sole responsibility of the author or authors and do not necessarily reflect the views of USAID or the United States government. Mining Sector Policy Study Paul Jourdan1 Gibson Chigumira Isaac Kwesu Erina Chipumho December 2012 1 Dr. Paul Jourdan was the lead researcher and principal author of this study. ZEPARU Figure 1: Map of Zimbabwe 1 ZEPARU CONTENTS Tables ................................................................................................................................................................... 4 Figures ................................................................................................................................................................. -
Proposed Black Country UNESCO Global Geopark
Great things to see and do in the Proposed Black Country UNESCO Global Geopark Black Country UNESCO Global Geopark Project The layers lying above these are grey muddy Welcome to the world-class rocks that contain seams of ironstone, fireclay heritage which is the Black and coal with lots of fossils of plants and insects. These rocks tell us of a time some 310 million Country years ago (called the Carboniferous Period, The Black Country is an amazing place with a named after the carbon in the coal) when the captivating history spanning hundreds of Black Country was covered in huge steamy millions of years. This is a geological and cultural rainforests. undiscovered treasure of the UK, located at the Sitting on top of those we find reddish sandy heart of the country. It is just 30 minutes from rocks containing ancient sand dunes and Birmingham International Airport and 10 minutes pebbly river beds. This tells us that the landscape by train from the city of Birmingham. dried out to become a scorching desolate The Black Country is where many essential desert (this happened about 250 million years aspects of the Industrial Revolution began. It ago and lasted through the Permian and Triassic was the world’s first large scale industrial time periods). landscape where anything could be made, The final chapter in the making of our landscape earning it the nick-name the ‘workshop of the is often called the’ Ice Age’. It spans the last 2.6 world’ during the Industrial Revolution. This million years of our history when vast ice sheets short guidebook introduces some of the sites scraped across the surface of the area, leaving and features that are great things to see and a landscaped sculpted by ice and carved into places to explore across many parts of The the hills and valleys we see today. -
Challenges in the Mining Industry in Zimbabwe, CAPITAL, CAPITAL
Leveraging on the Mining Sector for Economic Stimulation in Zimbabwe Godknows Njowa Pr Eng Venmyn Deloitte Contents of the Presentation The mining sector will be the centrepiece of our economic recovery and growth. It should generate growth spurts across sectors, reignite that economic miracle which must now happen… Quote from the President’s speech • Introduction • Geology of Zimbabwe • Zimbabwe’s Mineral Wealth • Contribution of the Mining Industry to the National GDP • Key Issues in Mining (Africa Focus) • Economic Development & Competitiveness Model • Way Forward • Conclusions and Recommendations 2 © 2013 Deloitte Touche Tohmatsu Limited Geology of Zimbabwe 3 Zimbabwean Mineral Wealth • 4 A perspective on attracting the right investment for mining companies in Zimbabwe © 2012 Deloitte Touche Tohmatsu Limited Zimbabwean Minerals Industry Industrial minerals include tantalite, tungsten and mica among many other minerals The Great Dyke is a phenomenal geological Industrial feature which is Chromite Minerals being well-mined and exploited PGMs Copper More than 6000 discoveries, 15 Mineral of which have commodities that delivered +1Moz Coal & have historically of gold Coke been produced Gold Great coal (USGS, 2012) reserves, with significant Iron & Silver opportunities Steel Relatively good infrastructure Cobalt Nickel 5 © 2012 Deloitte Touche Tohmatsu Limited Exploration and Geological Information (Critical Success Factor) Building an exploration sector in Zimbabwe Zimbabwe - proud history in exploration and mining Historically dominated -
Open Kosei.Pdf
The Pennsylvania State University The Graduate School Department of Geosciences GEOCHEMISTRY OF ARCHEAN–PALEOPROTEROZOIC BLACK SHALES: THE EARLY EVOLUTION OF THE ATMOSPHERE, OCEANS, AND BIOSPHERE A Thesis in Geosciences by Kosei Yamaguchi Copyright 2002 Kosei Yamaguchi Submitted in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy May 2002 We approve the thesis of Kosei Yamaguchi Date of Signature ____________________________________ _______________________ Hiroshi Ohmoto Professor of Geochemistry Thesis Advisor Chair of Committee ____________________________________ _______________________ Michael A. Arthur Professor of Geosciences ____________________________________ _______________________ Lee R. Kump Professor of Geosciences ____________________________________ _______________________ Raymond G. Najjar Associate Professor of Meteorology ____________________________________ _______________________ Peter Deines Professor of Geochemistry Associate Head for Graduate Program and Research in Geosciences iii ABSTRACT When did the Earth's surface environment become oxic? The timing and mechanism of the rise of atmospheric pO2 level in the early Precambrian have been long debated but no consensus has been reached. The oxygenation of the atmosphere and oceans has significant impacts on the evolution of the biosphere and the geochemical cycles of redox-sensitive elements. In order to constrain the evolution of the atmosphere, oceans, biosphere, and geochemical cycles of elements, a systematic and multidisciplinary -
Application Dossier for the Proposed Black Country Global Geopark
Application Dossier For the Proposed Black Country Global Geopark Page 7 Application Dossier For the Proposed Black Country Global Geopark A5 Application contact person The application contact person is Graham Worton. He can be contacted at the address given below. Dudley Museum and Art Gallery Telephone ; 0044 (0) 1384 815575 St James Road Fax; 0044 (0) 1384 815576 Dudley West Midlands Email; [email protected] England DY1 1HP Web Presence http://www.dudley.gov.uk/see-and-do/museums/dudley-museum-art-gallery/ http://www.blackcountrygeopark.org.uk/ and http://geologymatters.org.uk/ B. Geological Heritage B1 General geological description of the proposed Geopark The Black Country is situated in the centre of England adjacent to the city of Birmingham in the West Midlands (Figure. 1 page 2) .The current proposed geopark headquarters is Dudley Museum and Art Gallery which has the office of the geopark coordinator and hosts spectacular geological collections of local fossils. The geological galleries were opened by Charles Lapworth (founder of the Ordovician System) in 1912 and the museum carries out annual programmes of geological activities, exhibitions and events (see accompanying supporting information disc for additional detail). The museum now hosts a Black Country Geopark Project information point where the latest information about activities in the geopark area and information to support a visit to the geopark can be found. Figure. 7 A view across Stone Street Square Dudley to the Geopark Headquarters at Dudley Museum and Art Gallery For its size, the Black Country has some of the most diverse geology anywhere in the world.