Geochemistry) University of Arizona, May 1990, Advisor: P
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Vol 8, Issue 2, June 2009
mag30.qxd 05/05/2009 17:46 Page 1 MAGAZINE OF THE GEOLOGISTS’ ASSOCIATION Volume 8 No. 2 June 2009 Appeal for the Archives WSGS Study Tour of Guernsey Meetings July/October ROCKWATCH News Awards Proceedings of the GA Bernard Leake Retires Getting the most from the PGA Dates for your Diary Presidential Address/Lecture Reports GA Trip to Chafford Hundred Book Reviews CIRCULAR 979 mag30.qxd 05/05/2009 17:45 Page 2 Magazine of the Geologists’ Association From the President Volume 8 No.2, 2009 In writing the June presidential report, I am reminded of the vital role that the GA Published by the plays in upholding the importance of geology on a range of scales, from local Geologists’ Association. to international. For example, the GA can serve as a point of contact to provide Four issues per year. CONTENTS critical information on key geological ISSN 1476-7600 sequences that are under threat from 3. The Association insensitive development plans - in short, Production team: JOHN CROCKER, acting as an expert witness. This does Paula Carey, John Cosgrove, New GA Awards not necessarily entail opposing develop- Vanessa Harley, Bill French 4. GA Meetings July/October ment but rather looking for opportunities to enhance geological resources for 5. Awards Printed by City Print, Milton Keynes future study while ensuring that they are 6. Bernard Leake Retires appropriately protected. In addition, a major part of our national earth heritage The GEOLOGISTS’ ASSOCIATION 7. Dates for your Diary is preserved within our museums and in does not accept any responsibility for 8. -
Detrital Zircon Provenance and Lithofacies Associations Of
geosciences Article Detrital Zircon Provenance and Lithofacies Associations of Montmorillonitic Sands in the Maastrichtian Ripley Formation: Implications for Mississippi Embayment Paleodrainage Patterns and Paleogeography Jennifer N. Gifford 1,*, Elizabeth J. Vitale 1, Brian F. Platt 1 , David H. Malone 2 and Inoka H. Widanagamage 1 1 Department of Geology and Geological Engineering, University of Mississippi, Oxford, MS 38677, USA; [email protected] (E.J.V.); [email protected] (B.F.P.); [email protected] (I.H.W.) 2 Department of Geography, Geology, and the Environment, Illinois State University, Normal, IL 61790, USA; [email protected] * Correspondence: jngiff[email protected]; Tel.: +1-(662)-915-2079 Received: 17 January 2020; Accepted: 15 February 2020; Published: 22 February 2020 Abstract: We provide new detrital zircon evidence to support a Maastrichtian age for the establishment of the present-day Mississippi River drainage system. Fieldwork conducted in Pontotoc County,Mississippi, targeted two sites containing montmorillonitic sand in the Maastrichtian Ripley Formation. U-Pb detrital zircon (DZ) ages from these sands (n = 649) ranged from Mesoarchean (~2870 Ma) to Pennsylvanian (~305 Ma) and contained ~91% Appalachian-derived grains, including Appalachian–Ouachita, Gondwanan Terranes, and Grenville source terranes. Other minor source regions include the Mid-Continent Granite–Rhyolite Province, Yavapai–Mazatzal, Trans-Hudson/Penokean, and Superior. This indicates that sediment sourced from the Appalachian Foreland Basin (with very minor input from a northern or northwestern source) was being routed through the Mississippi Embayment (MSE) in the Maastrichtian. We recognize six lithofacies in the field areas interpreted as barrier island to shelf environments. Statistically significant differences between DZ populations and clay mineralogy from both sites indicate that two distinct fluvial systems emptied into a shared back-barrier setting, which experienced volcanic ash input. -
Lithics, Landscape and People: Life Beyond the Monuments in Prehistoric Guernsey
UNIVERSITY OF SOUTHAMPTON FACULTY OF HUMANITIES Department of Archaeology Lithics, Landscape and People: Life Beyond the Monuments in Prehistoric Guernsey by Donovan William Hawley Thesis for the degree of Doctor of Philosophy April 2017 UNIVERSITY OF SOUTHAMPTON ABSTRACT FACULTY OF HUMANITIES Archaeology Thesis for the degree of Doctor of Philosophy Lithics, Landscape and People: Life Beyond the Monuments in Prehistoric Guernsey Donovan William Hawley Although prehistoric megalithic monuments dominate the landscape of Guernsey, these have yielded little information concerning the Mesolithic, Neolithic and Early Bronze Age communities who inhabited the island in a broader landscape and maritime context. For this thesis it was therefore considered timely to explore the alternative material culture resource of worked flint and stone archived in the Guernsey museum. Largely ignored in previous archaeological narratives on the island or considered as unreliable data, the argument made in this thesis is for lithics being an ideal resource that, when correctly interrogated, can inform us of past people’s actions in the landscape. In order to maximise the amount of obtainable data, the lithics were subjected to a wide ranging multi-method approach encompassing all stages of the châine opératoire from material acquisition to discard, along with a consideration of the landscape context from which the material was recovered. The methodology also incorporated the extensive corpus of lithic knowledge that has been built up on the adjacent French mainland, a resource largely passed over in previous Channel Island research. By employing this approach, previously unknown patterns of human occupation and activity on the island, and the extent and temporality of maritime connectivity between Guernsey and mainland areas has been revealed. -
Detrital Zircon Ages and Nd Isotopic Data from the Southern Appalachian
Geological Society of America Memoir 197 2004 Detrital zircon ages and Nd isotopic data from the southern Appalachian crystalline core, Georgia, South Carolina, North Carolina, and Tennessee: New provenance constraints for part of the Laurentian margin Brendan R. Bream* Robert D. Hatcher Jr. Department of Earth and Planetary Sciences, University of Tennessee, Knoxville, Tennessee 37996-1410, USA Calvin F. Miller Department of Geology, Vanderbilt University, Nashville, Tennessee 37235, USA Paul D. Fullagar Department of Geological Sciences, University of North Carolina, Chapel Hill, North Carolina 27599-3315, USA ABSTRACT Sedimentary and metasedimentary rocks within the southern Appalachian Blue Ridge and Inner Piedmont contain a valuable record of Late Proterozoic Laurentian margin evolution following the breakup of Rodinia. Paleogeographic reconstructions and increasing amounts of geochronologic and isotopic data limit the derivation of these paragneisses to the Laurentian and/or west Gondwanan craton(s). Southern ε Appalachian crystalline core paragneiss samples have Nd values between –8.5 and –2.0 at the time of deposition and contain abundant 1.1–1.25 Ga zircon cores with Grenville 1.0–1.1 Ga metamorphic rims. Less abundant detrital zircons are pre-Grenvillian: Mid- dle Proterozoic 1.25–1.6 Ga, Early Proterozoic 1.6–2.1 Ga, and Late Archean 2.7–2.9 ε Ga. Blue Ridge Grenvillian basement has almost identical Nd values and displays the same dominant magmatic core and metamorphic rim zircon ages. Based on our data, nonconformable basement-cover relationships, and crustal ages in eastern North Amer- ica, we contend that the extensive sedimentary packages in the southern Appalachian ε Blue Ridge and western Inner Piedmont are derived from Laurentia. -
Transactions Lists.Xls
La Société Guernesiaise Papers appearing in the Transactions In chronological order For author order or subject order click on tab at bottom of page. Annual Section reports are not included. Complete printed indexes covering the years 1882 to 1980 can be purchased from the office of La Société. Many issues of the Transactions and reprints of papers are also available for purchase. Decade: 1880 1890 1900 1910 1920 1930 1940 1950 1960 1970 1980 1990 2000 2010 YEAR PAGE VOL PART TITLE AUTHOR 1882-1889 35 I 1 The geology of Guernsey Hill, E 1882-1889 45 I 1 The ferns of Guernsey Derrick, G T 1882-1889 61 I 1 The butterflies of Guernsey and Sark Luff, W A 1882-1889 74 I 1 On the occurrence of calcite in Guernsey Collenette, A 1882-1889 78 I 1 An excursion to Icart Point Derrick, G T 1882-1889 83 I 1 On changes in the relative level of sea and land Derrick, G T 1882-1889 89 I 1 List of flowering plants found in Guernsey Derrick, G T 1889 123 I 2 On the Genus Isoetes Marquand, E D 1889 128 I 2 Excursion to Herm Derrick, G T 1889 133 I 2 The Flora of Herm Marquand, E D 1889 139 I 2 History of Herm Lee, G E 1889 143 I 2 Excursion to Lihou Randell, J B 1889 148 I 2 Crustacea Sinel, J The Nocturnal Macro-Lepidoptera of Guernsey, Alderney, 1889 155 I 2 Luff, W A Sark, and Herm Return to top YEAR PAGE VOL PART TITLE AUTHOR On the correlation and relative ages of the rocks of the 1890 30 II 1 de la Mare, C G Channel Islands 1890 37 II 1 A dredging excursion off Guernsey Spencer, R L 1890 41 II 1 Some notable oral equipments in the vertebrata Rose, -
Detrital Zircon Provenance and Correlation of Two Newly Discovered Ripley Formation Bentonites: Pontotoc County, Mississippi
University of Mississippi eGrove Electronic Theses and Dissertations Graduate School 2019 Detrital Zircon Provenance and Correlation of Two Newly Discovered Ripley Formation Bentonites: Pontotoc County, Mississippi Elizabeth Jayne Vitale University of Mississippi Follow this and additional works at: https://egrove.olemiss.edu/etd Part of the Geology Commons Recommended Citation Vitale, Elizabeth Jayne, "Detrital Zircon Provenance and Correlation of Two Newly Discovered Ripley Formation Bentonites: Pontotoc County, Mississippi" (2019). Electronic Theses and Dissertations. 1707. https://egrove.olemiss.edu/etd/1707 This Thesis is brought to you for free and open access by the Graduate School at eGrove. It has been accepted for inclusion in Electronic Theses and Dissertations by an authorized administrator of eGrove. For more information, please contact [email protected]. DETRITAL ZIRCON PROVENANCE AND CORRELATION OF TWO NEWLY DISCOVERED RIPLEY FORMATION BENTONITES: PONTOTOC COUNTY, MISSISSIPPI A Thesis Presented in partiAl fulfillment of requirements for the degree of MAster of Science in the Department of Geology and GeologicAl Engineering The University of Mississippi by ELIZABETH J. VITALE MAy 2019 Copyright © 2019 ElizAbeth J VitAle ALL RIGHTS RESERVED ABSTRACT TWo neWly discovered bentonite deposits in northern and southern Pontotoc County, Mississippi occur in the Upper CretAceous outcrop in a banded pattern on the northeAstern mArgin of the Mississippi Embayment (MSE). The entire Ripley FormAtion (Fm) consists of ~73 m of fossiliferous clAy, sAnd, and cAlcAreous sAnd beds. The bentonites are locAted stratigraphicAlly within the ChiWApa SAndstone Member (CSM) at the top of the Ripley Fm and stratigraphicAlly lie above previously mined bentonites in central Pontotoc County. Since the northern and southern bentonites differ stratigraphicAlly from the previously mined bentonites, it is possible that there are other unknown bentonite deposits throughout Pontotoc County. -
Magmatic Enclaves and Evidence for Magma Mixing in the Oak Point Granite, Deer Isle, Maine, USA Ben Johnston
The University of Maine DigitalCommons@UMaine Electronic Theses and Dissertations Fogler Library 12-2001 Magmatic Enclaves and Evidence for Magma Mixing in the Oak Point Granite, Deer Isle, Maine, USA Ben Johnston Follow this and additional works at: http://digitalcommons.library.umaine.edu/etd Part of the Geology Commons, and the Tectonics and Structure Commons Recommended Citation Johnston, Ben, "Magmatic Enclaves and Evidence for Magma Mixing in the Oak Point Granite, Deer Isle, Maine, USA" (2001). Electronic Theses and Dissertations. 603. http://digitalcommons.library.umaine.edu/etd/603 This Open-Access Thesis is brought to you for free and open access by DigitalCommons@UMaine. It has been accepted for inclusion in Electronic Theses and Dissertations by an authorized administrator of DigitalCommons@UMaine. MAGMATIC ENCLAVES AND EVIDENCE FOR MAGMA MIXING IN THE OAK POINT GRANITE, DEER ISLE, MAINE, U.S.A. BY Ben Johnston B.S. University of Cincinnati, 1998 A THESIS Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Science (in Geological Sciences) The Graduate School The University of Maine December, 200 1 Advisory Committee: Daniel R. Lux, Professor of Geological Sciences, Advisor David Gibson, Professor of Geological Sciences, University of Maine at Fannington Martin G. Yates, Associate Scientist, Geological Sciences MAGMATIC ENCLAVES AND EVIDENCE FOR MAGMA MIXING IN THE OAK POINT GRANITE, DEER ISLE, MAINE, U.S.A. By Ben Johnston Thesis Advisor: Dr. Daniel R. Lux An Abstract of the Thesis Presented in Partial Fulfillment of the Requirements for the Degree of Master of Science (in Geological Sciences) December, 200 1 The Coastal Maine Magmatic Province (CMMP) consists of over 100 post tectonic plutons with ages varying from Silurian to Carboniferous. -
Geochemistry of Volcanic Rocks of the Carolina and Augusta Terranes in Central South Carolina: an Exotic Rifted Volcanic Arc?
SP304-14.QXD 5/15/96 04≈42 PM Page 219 Geological Society of America Special Paper 304 1996 Geochemistry of volcanic rocks of the Carolina and Augusta terranes in central South Carolina: An exotic rifted volcanic arc? John W. Shervais, Suzanne A. Shelley*, and Donald T. Secor, Jr. Department of Geological Sciences, University of South Carolina, Columbia, South Carolina 29208 ABSTRACT This chapter presents new whole-rock, major- and trace-element geochemical data from the Carolina and Augusta terranes in South Carolina. Geochemical data from the Persimmon Fork and Richtex Formations strongly confirm the interpreta- tion of previous workers that the Carolina terrane is a remnant of a subduction- related volcanic arc. These data further suggest that the arc developed either on top of an older arc or on a thinned section of continental crust. Geochronological data from the southern Appalachians indicate that the subduction-related arc in the Carolina terrane developed simultaneously with the initial opening of Iapetus, the “Proto- Atlantic” Ocean. Therefore, the arc could not have formed in the Iapetus Ocean basin, and must be exotic relative to cratonic North America. INTRODUCTION The southern Appalachian Piedmont is widely interpreted as a collage of tectonostratigraphic terranes (Fig. 1) accreted to Laurentia (North America) during the Paleozoic (Williams and Hatcher, 1982, 1983; Horton et al., 1989, 1991). The paleogeo- graphic histories of most of the terranes are uncertain because Paleozoic penetrative deformation and regional metamorphism have erased fossils and primary paleomagnetism that might oth- erwise yield paleogeographic information. However, the Caro- lina terrane has been interpreted as exotic with respect to Laurentia because it contains an Atlantic Province trilobite fauna of Middle Cambrian age (Secor et al., 1983). -
Proceedings of the Ussher Society
Proceedings of the Ussher Society Research into the geology and geomorphology of south-west England Volume 6 Part 3 1986 Edited by G.M Power The Ussher Society Objects: To promote research into the geology and geomorphology of south- west England and the surrounding marine areas; to hold Annual Conferences at various places in South West England where those engaged in this research can meet formally to hear original contributions and progress reports and informally to effect personal contacts; to publish, proceedings of such Conferences or any other work which the Officers of the Society may deem suitable. Officers: Chairman Dr. C.T. Scrutton Vice-Chairman Dr. E. B. Selwood Secretary Mr M.C. George Treasurer Mr R.C. Scrivener Editor Dr. G.M. Power Committee Members Dr G. Warrington Mr. C. R. Morey Mr. C.D.N. Tubb Mr. C. Cornford Mr D. Tucker Membership of the Ussher Society is open to all on written application to the Secretary and payment of the subscription due on January lst each year. Back numbers may be purchased from the Secretary to whom correspondence should be directed at the following address: Mr M. C. George, Department of Geology, University of Exeter, North Park Road, Exeter, Devon EX4 4QE Proceedings of the Ussher Society Volume 6 Part 3 1986 Edited by G.M. Power Crediton, 1986 © Ussher Society ISSN 0566-3954 1986 Typeset, printed and bound bv Phillips & Co., The Kyrtonia Press, 115 High Street, Crediton, Devon EXl73LG Set in Baskerville and Printed by Photolithography Proceedings of the Ussher Society Volume 6, Part 3, 1986 Papers D.L. -
Paleozoic Evolution of Pre-Variscan Terranes: from Gondwana to the Variscan Collision
Geological Society of America Special Paper 364 2002 Paleozoic evolution of pre-Variscan terranes: From Gondwana to the Variscan collision Gérard M. Stamp×i Institut de Géologie et Paléontologie, Université de Lausanne, CH-1015 Lausanne, Switzerland Jürgen F. von Raumer Institut de Minéralogie et Pétrographie, Université de Fribourg, CH-1700 Fribourg, Switzerland Gilles D. Borel Institut de Géologie et Paléontologie, Université de Lausanne, CH-1015 Lausanne, Switzerland ABSTRACT The well-known Variscan basement areas of Europe contain relic terranes with a pre-Variscan evolution testifying to their peri-Gondwanan origin (e.g., relics of Neo- proterozoic volcanic arcs, and subsequent stages of accretionary wedges, backarc rift- ing, and spreading). The evolution of these terranes was guided by the diachronous subduction of the proto-Tethys oceanic ridge under different segments of the Gond- wana margin. This subduction triggered the emplacement of magmatic bodies and the formation of backarc rifts, some of which became major oceanic realms (Rheic, paleo- Tethys). Consequently, the drifting of Avalonia was followed, after the Silurian and a short Ordovician orogenic event, by the drifting of Armorica and Alpine domains, ac- companied by the opening of the paleo-Tethys. The slab rollback of the Rheic ocean is viewed as the major mechanism for the drifting of the European Variscan terranes. This, in turn, generated a large slab pull force responsible for the opening of major rift zones within the passive Eurasian margin. Therefore, the µrst Middle Devonian Variscan orogenic event is viewed as the result of a collision between terranes detached from Gondwana (grouped as the Hun superterrane) and terranes detached from Eurasia. -
Kings Mountain National Military Park Geologic Resources Inventory Report
National Park Service U.S. Department of the Interior Natural Resource Program Center Kings Mountain National Military Park Geologic Resources Inventory Report Natural Resource Report NPS/NRPC/GRD/NRR—2009/129 THIS PAGE: The Centennial Monument erected in 1880 was the result of a massive effort by descendents and state governments to recognize those who fought at the Battle of Kings Mountain. ON THE COVER: The monadnock known as Kings Mountain was the scene of the 1780 Battle of Kings Mountain. The rocky slopes helped provide cover for the patriot forces as they enciencircledrcled the loyalist forces under Major Patrick Ferguson. NPS Photos courtesy Chris Revels (Kings Moun- tain NMP) Kings Mountain National Military Park Geologic Resources Inventory Report Natural Resource Report NPS/NRPC/GRD/NRR—2009/129 Geologic Resources Division Natural Resource Program Center P.O. Box 25287 Denver, Colorado 80225 September 2009 U.S. Department of the Interior National Park Service Natural Resource Program Center Denver, Colorado The Natural Resource Publication series addresses natural resource topics that are of interest and applicability to a broad readership in the National Park Service and to others in the management of natural resources, including the scientific community, the public, and the NPS conservation and environmental constituencies. Manuscripts are peer-reviewed to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and is designed and published in a professional manner. Natural Resource Reports are the designated medium for disseminating high priority, current natural resource management information with managerial application. The series targets a general, diverse audience, and may contain NPS policy considerations or address sensitive issues of management applicability. -
Geological Setting of the Reed Gold Mine, North Carolina
GEOLOGICAL SETTING OF THE REED GOLD MINE, NORTH CAROLINA By Stephen Challener* [email protected] James Hibbard** [email protected] Dept. of Marine, Earth and Atmospheric Sciences, North Carolina State University, Raleigh, North Carolina 27695 *now at: 705 Hunting Ridge Rd., Raleigh, NC 27615, **Emeritus, now at 1916 Lost Cove Lane, Raleigh, NC 27603 NORTH CAROLINA GEOLOGICAL SURVEY SPECIAL PUBLICATION 13 23 December 2020 Suggested citation: Challener, S. and Hibbard, J., 2020, Geological setting of the Reed Gold Mine, North Carolina, North Carolina Geological Survey Special Publication 13, 40p. CONTENTS FOREWORD …………………………………………………………………………4 ABSTRACT …………………………………………………………………………4 INTRODUCTION …………………………………………………………………………4 Historical Context …………………………………………………………………6 Regional Geological Context …………………………………………………8 Previous Work at the Reed Gold Mine ………………………………………..10 SCOPE OF STUDY ………………………………………………………………..10 Mapping Observations ………………………………………………………..11 Unseparated Albemarle Group ………………………………………..13 Laminated argillite ………………………………………………..13 Tuffaceous argillite ………………………………………………..13 Massive argillite ………………………………………………..14 Slaty argillite ………………………………………………..14 Chloritic argillite ………………………………………………..15 Volcaniclastic conglomerate ………………………………………..15 Reed Gold Mine Gabbro ………………………………………………..16 Distribution ………………………………………………………..17 Description ………………………………………………………..18 Age ………………………………………………………..18 Geochemistry of the Reed Gold Mine Gabbro ………………………………..19 Sampling and Preparation ………………………………..19 Analytical Methods