1 STEPHEN T. HASIOTIS, Ph.D. Curriculum Vitae Updated 112213 EDUCATION University of Colorado, Boulder Geological Science
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Post-Carboniferous Stratigraphy, Northeastern Alaska by R
Post-Carboniferous Stratigraphy, Northeastern Alaska By R. L. DETTERMAN, H. N. REISER, W. P. BROSGE,and]. T. DUTRO,JR. GEOLOGICAL SURVEY PROFESSIONAL PAPER 886 Sedirnentary rocks of Permian to Quaternary age are named, described, and correlated with standard stratigraphic sequences UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1975 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Detterman, Robert L. Post-Carboniferous stratigraphy, northeastern Alaska. (Geological Survey Professional Paper 886) Bibliography: p. 45-46. Supt. of Docs. No.: I 19.16:886 1. Geology-Alaska. I. Detterman, Robert L. II. Series: United States. Geological Survey. Professional Paper 886. QE84.N74P67 551.7'6'09798 74-28084 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-02687-2 CONTENTS Page Page Abstract __ _ _ _ _ __ __ _ _ _ _ _ _ _ _ _ _ _ _ __ __ _ _ _ _ _ _ __ __ _ _ __ __ __ _ _ _ _ __ 1 Stratigraphy__:_Continued Introduction __________ ----------____ ----------------____ __ 1 Kingak Shale ---------------------------------------- 18 Purpose and scope ----------------------~------------- 1 Ignek Formation (abandoned) -------------------------- 20 Geographic setting ------------------------------------ 1 Okpikruak Formation (geographically restricted) ________ 21 Previous work and acknowledgments ------------------ 1 Kongakut Formation ---------------------------------- -
Triassic- Jurassic Stratigraphy Of
Triassic- Jurassic Stratigraphy of the <JF C7 JL / Culpfeper and B arbour sville Basins, VirginiaC7 and Maryland/ ll.S. PAPER Triassic-Jurassic Stratigraphy of the Culpeper and Barboursville Basins, Virginia and Maryland By K.Y. LEE and AJ. FROELICH U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1472 A clarification of the Triassic--Jurassic stratigraphic sequences, sedimentation, and depositional environments UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1989 DEPARTMENT OF THE INTERIOR MANUEL LUJAN, Jr., Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government Library of Congress Cataloging in Publication Data Lee, K.Y. Triassic-Jurassic stratigraphy of the Culpeper and Barboursville basins, Virginia and Maryland. (U.S. Geological Survey professional paper ; 1472) Bibliography: p. Supt. of Docs. no. : I 19.16:1472 1. Geology, Stratigraphic Triassic. 2. Geology, Stratigraphic Jurassic. 3. Geology Culpeper Basin (Va. and Md.) 4. Geology Virginia Barboursville Basin. I. Froelich, A.J. (Albert Joseph), 1929- II. Title. III. Series. QE676.L44 1989 551.7'62'09755 87-600318 For sale by the Books and Open-File Reports Section, U.S. Geological Survey, Federal Center, Box 25425, Denver, CO 80225 CONTENTS Page Page Abstract.......................................................................................................... 1 Stratigraphy Continued Introduction... .......................................................................................... -
Submarine Carbonate Breccia Beds-A
University of Calgary PRISM: University of Calgary's Digital Repository Science Science Research & Publications 1979-01 Submarine carbonate breccia beds-a depositional model for two-layer, sediment gravity flows from the Sekwi Formation (Lower Cambrian), Mackenzie Mountains, Northwest Territories, Canada Krause, Federico F.; Oldershaw, A. E. National Research Council Canada Krause, F. F. and Oldershaw, A. E.. (1979). "Submarine carbonate breccia beds-a depositional model for two-layer, sediment gravity flows from the Sekwi Formation (Lower Cambrian), Mackenzie Mountains, Northwest Territories, Canada". Canadian Journal of Earth Sciences, 16: 189-199. http://hdl.handle.net/1880/44462 journal article Downloaded from PRISM: https://prism.ucalgary.ca 189 ine carbonate breccia beds-a depositional model for two-layer, sediment gravity ow from the Sekwi Formation (Lower Cambrian), Mackenzie Mountains, Northwest Territories, Canada F. F. KRAUSEAND A. E. OLDERSHAW I)~,portrm,rltc!f'GcoIo~y. Urli~.rrsityc!f'Crrl,<*rrr:\.. Ct11gtrr.v. Altcc.. Crrr~rrtltrT2N IN4 Received September 5. 1978 Revision accepted Septemher 22. 1978 in the Sekwi Formation. cxbonate breccia beds interhedded with slope sediments are inter- p~c~cd;I\ \uhnl:~rine sediment gravity flow\ that formed a two-layer deposit during n single II.,II\~VIevent. They are intermediate between true slump and turbidites and may initiate by \I~~nip~ng;~nvwhereon the continental slope and rise. Textural characteristics of the deposits are ;I limc~ionofttowndope transport distance. Ihm 1;1 formation de Sekwi, on interprete les cowhe\ de carbonates hl-echique\ interstratifies .,\N dc\ \idinlent\ de talus comme des coulees par gravite de sediments sousmarins qui ont Irh~r~lC(In &pOt hicouche durant un seul Cpiwcle de tran\pol-t. -
The Pathway Towards Sustainable Europe“
EU Land Policy “The Pathway Towards Sustainable Europe“ Anna Bandlerová – Pavol Bielek - Pavol Schwarcz - Lucia Palšová NITRA 2016 Title: EU Land Policy “The Pathway Towards Sustainable Europe“ Authors: prof. JUDr. Anna Bandlerová, PhD. (2 AH), chapter 10 Slovak University of Agriculture in Nitra prof. RNDr. Pavol Bielek, DrSc. (12,72 AH), chapter 4, 5, 6, 7, 8, 9; Slovak University of Agriculture in Nitra prof. Ing. Pavol Schwarcz, PhD. (1,35 AH), chapter 2; Slovak University of Agriculture in Nitra JUDr. Lucia Palšová, PhD. (2,57 AH), chapter 3, 11; Slovak University of Agriculture in Nitra Reviewers: prof. Ing. Dušan Húska, PhD. prof. Dr. Edward Pierzgalski, PhD. © Slovak University of Agriculture in Nitra Approved by the Rector of the Slovak University of Agriculture in Nitra on 25.4.2016 as a scientific monograph. This scientific monograph was created with the support of the following international projects: Jean Monet Centre of Excelence, DECISION n. 2013-2883/001-001 Project No: 54260o-LLP-1-2013-1-SK-AJM-P, EU Land Policy “The Pathway Towards Sustainable Europe“ "This project has been funded with support from the European Commission. This publication reflects the views only of the author, and the Commission cannot be held responsible for any use which may be made of the information contained therein." "With the support of the Lifelong Learning Programme of the European Union" ISBN 978-80-552-1499-3 2 Look deep in to nature and than you will understand everything better. Albert Einstein 3 CONTENTS PREFACE ................................................................................................................................. 7 1 INTRODUCTION ............................................................................................................. 7 2 EU AGRICULTURAL POLICY (CAP) ......................................................................... 8 2.1 Introduction to CAP .................................................................................................... -
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Chronology and Faunal Evolution of the Middle Eocene Bridgerian North American Land Mammal “Age”: Achieving High Precision Geochronology Kaori Tsukui Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the Graduate School of Arts and Sciences COLUMBIA UNIVERSITY 2016 © 2015 Kaori Tsukui All rights reserved ABSTRACT Chronology and Faunal Evolution of the Middle Eocene Bridgerian North American Land Mammal “Age”: Achieving High Precision Geochronology Kaori Tsukui The age of the Bridgerian/Uintan boundary has been regarded as one of the most important outstanding problems in North American Land Mammal “Age” (NALMA) biochronology. The Bridger Basin in southwestern Wyoming preserves one of the best stratigraphic records of the faunal boundary as well as the preceding Bridgerian NALMA. In this dissertation, I first developed a chronological framework for the Eocene Bridger Formation including the age of the boundary, based on a combination of magnetostratigraphy and U-Pb ID-TIMS geochronology. Within the temporal framework, I attempted at making a regional correlation of the boundary-bearing strata within the western U.S., and also assessed the body size evolution of three representative taxa from the Bridger Basin within the context of Early Eocene Climatic Optimum. Integrating radioisotopic, magnetostratigraphic and astronomical data from the early to middle Eocene, I reviewed various calibration models for the Geological Time Scale and intercalibration of 40Ar/39Ar data among laboratories and against U-Pb data, toward the community goal of achieving a high precision and well integrated Geological Time Scale. In Chapter 2, I present a magnetostratigraphy and U-Pb zircon geochronology of the Bridger Formation from the Bridger Basin in southwestern Wyoming. -
Hydrogeology of the Chinle Wash Watershed, Navajo Nation Arizona, Utah and New Mexico
Hydrogeology of the Chinle Wash Watershed, Navajo Nation Arizona, Utah and New Mexico Item Type Thesis-Reproduction (electronic); text Authors Roessel, Raymond J. Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 07/10/2021 19:50:22 Link to Item http://hdl.handle.net/10150/191379 HYDROGEOLOGY OF THE CHINLE WASH WATERSHED, NAVAJO NATION, ARIZONA, UTAH AND NEW MEXICO by Raymond J. Roessel A Thesis Submitted to the Faculty of the DEPARTMENT OF HYDROLOGY AND WATER RESOURCES In Partial Fulfillment of the Requirements For the Degree of MASTER OF SCIENCE WITH A MAJOR IN HYDROLOGY In the Graduate College THE UNIVERSITY OF ARIZONA 1994 2 STATEMENT BY AUTHOR This thesis has been submitted in partial fulfillment of requirements for an advanced degree at The University of Arizona and is deposited in the University Library to be made available to borrowers under rules of the Library. Brief quotations from this thesis are allowable without special permission, provided that accurate acknowledgment of source is made. Requests for permission for extended quotation from or reproduction of this manuscript in whole or in part may be granted by the head of the major department or the Dean of the Graduate College when in his or her judgment the proposed use of the material is in the interests of scholarship. In all other instances, however, permission must be obtained from the author. -
Appendix D Paleontological Resources Technical Report
Kassab Travel Center Project Appendix D Paleontological Resources Technical Report PALEONTOLOGICAL RESOURCES TECHNICAL REPORT FOR THE KASSAB TRAVEL CENTER PROJECT, CITY OF LAKE ELSINORE, CALIFORNIA Prepared for: Josh Haskins Environmental Advisors 2400 E. Katella Avenue, Suite 800 Anaheim, CA 92806 Principal Investigator: Kim Scott, Principal Paleontologist August 2017 Project Number: 4083 Type of Study: Paleontological Resources Assessment Localities: None within five miles of the project in late Pleistocene alluvium USGS Quadrangle: Elsinore 7.5’ Area: 2.39 acres Key Words: modern artificial fill (PFYC 1), Holocene to late Pleistocene axial channel deposits (PFYC 2 at surface, PFYC 3a at more than 8 feet deep), early Pleistocene very old alluvial fan (PFYC 3b); negative survey 1518 West Taft Avenue Branch Offices cogstone.com Orange, CA 92865 San Diego – Riverside – Morro Bay – San Francisco Toll free (888) 333-3212 Office (714) 974-8300 Federal Certifications 8(a), SDB, EDWOSB State Certifications DBE, WBE, SBE, UDBE Kassab Travel Center Paleontology Assessment TABLE OF CONTENTS SUMMARY OF FINDINGS .................................................................................................................................... III INTRODUCTION ....................................................................................................................................................... 1 PURPOSE OF STUDY ................................................................................................................................................... -
Revision of the Lower Part of the Tertiary System in the Central and \Vestern Uinta Basin, Utah______
Revision of the Lower Part of the Tertiary System in the Central and \Vestern Uinta Basin, Utah_____ __________ GEOLOGICAL SURVEY BULLETIN 1405G Revision of the Lower Part of the Tertiary System in the Central and \Vfestern Uinta Basin, Utah By THOMAS D. FOUCH CONTRIBUTIONS TO STRATIGRAPHY GEOLOGICAL SURVEY BULLETIN 1405-C Correlation of lower Tertiary stratigraphic units recently penetrated in northeastern Utah UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1976 UNITED STATES DEPARTMENT OF THE INTERIOR THOMAS S. KLEPPE, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Fouch, Thomas D. Revision of the lower part of the Tertiary system in the central and western Uinta Basin, Utah. (Contributions to stratigraphy) (Geological Survey Bulletin 1405-C) Bibliography: p. Supt. of Docs, no.: I 19.3:1405-C 1. Geology, Stratigraphic Tertiary. 2. Geology, Stratigraphic Nomenclature Utah Uinta Basin. I. Title. II. Series. III. Series: United States Geological Survey Bulletin 1405-C. QE75.B9 No. 1405-C [QE691] 557.3'08s [ 551.7'8'0979221] 75-619374 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D. C. 20402 Stock Number 024-001-02770-4 CONTENTS Page Abstract....................................................................................................................... Cl Introduction................................................................................................................ 1 North Horn Formation ............................................................................................. -
Carbonate-Hosted Zn-Pb Mineralization in the Lower
Carbonate-hosted Zn-Pb mineralization in the Lower Cambrian Sekwi Formation, Mackenzie Mountains, NWT: Stratigraphic, structural, and lithologic controls, and constraints on ore fluid characteristics by Beth J. Fischer Thesis submitted in partial fulfillment of the requirements for the degree of Master of Science (M.Sc.) in Geology School of Graduate Studies Laurentian University Sudbury, Ontario © Beth Fischer, 2012 Library and Archives Bibliotheque et Canada Archives Canada Published Heritage Direction du 1+1 Branch Patrimoine de I'edition 395 Wellington Street 395, rue Wellington Ottawa ON K1A0N4 Ottawa ON K1A 0N4 Canada Canada Your file Votre reference ISBN: 978-0-494-87713-5 Our file Notre reference ISBN: 978-0-494-87713-5 NOTICE: AVIS: The author has granted a non L'auteur a accorde une licence non exclusive exclusive license allowing Library and permettant a la Bibliotheque et Archives Archives Canada to reproduce, Canada de reproduire, publier, archiver, publish, archive, preserve, conserve, sauvegarder, conserver, transmettre au public communicate to the public by par telecommunication ou par I'lnternet, preter, telecommunication or on the Internet, distribuer et vendre des theses partout dans le loan, distrbute and sell theses monde, a des fins commerciales ou autres, sur worldwide, for commercial or non support microforme, papier, electronique et/ou commercial purposes, in microform, autres formats. paper, electronic and/or any other formats. The author retains copyright L'auteur conserve la propriete du droit d'auteur ownership and moral rights in this et des droits moraux qui protege cette these. Ni thesis. Neither the thesis nor la these ni des extraits substantiels de celle-ci substantial extracts from it may be ne doivent etre imprimes ou autrement printed or otherwise reproduced reproduits sans son autorisation. -
Geology and Coal Resources of Atarque Lake Quadrangle, Cibola
GEOLOGY AND COAL RESOURCESOF THE ATARQUE LAKEQUADRANGLE, CIBOLA COUNTY, NEW MEXICO NEW MEXICO BUREAU OF MINES AND MINERALRESOURCES OPEN-FILEREPORT 167 bY ORIN J. ANDERSON June, 1982 (revised,1983) Contents: (1) Discussion of Geology and CoalResources (attached) (2) Geologic map with cross sesction (accompanying) Table of Contents GEOLOGY General P. Study Area P. Structure P. Stratigraphy P. COAL RESOURCES p. 22 REFERENCES p. 23 Figures 1 - Measured section of Zuni and Dakota SS. p. 11 2 - Measured section of Atarque and Moreno Hill Fms. p. 18 GEOLOGY General The Atarque Lake quadrangle lies in the southwestern part of the Zuni Basin, a broad,shallow structural element that extends southwestward from the Zuni Mountains of New Mexico into east- central Arizona. As such it liesnear the southeastern margin ofthe Colorado Plateau. The regionaldip in the study area is very gently northeastward toward the Gallup Sag which comprises thenortheastern part of the Basin. There are, however, broad, gentle NW-SE trending folds which result in local southwestward dips, and at least twoabrupt monoclinal flexures, up on the northeastside, (opposed to regional dip) that clearly define the NW-SE structural grain of the area, as well as minor faulting. These structural trends parallel the axis of the Zuni Uplift, but perhaps more importantly they appear to represent the southeastward extension of the structural axes that wrap aroundthe southern end of the Defiance Uplift, as shown by Davis andKiven (1975), and theyalso align very well with the northwest-trendingdike system in the Fence Lake (the Dyke quadrangle),Techado, Adams Diggings,and Pietown areas. Of the three structural features mentioned - broadfolds, monoclines and faulting - monoclinesare the most pronounced and significantnot only locally, but in a much broadercontext. -
Technical Report Mackenzie Mountains
TECHNICAL REPORT MACKENZIE MOUNTAINS IRON-COPPER PROPERTY, NORTHWEST TERRITORIES, CANADA NTS: 106F/01, 02 Mackenzie Mining District, Northwest Territories, Canada 65° 12’ N and 132° 27’ E PREPARED FOR: Metallis Resources Inc. And Seahawk Ventures Inc. PREPARED BY: Aurora Geosciences Ltd. TECHNICAL REPORT MACKENZIE MOUNTAINS IRON-COPPER PROPERTY Northwest Territories, Canada Effective Date: June 01, 2016 Prepared for METALLIS RESOURCES INC. 515 – 850 West Hastings Street Vancouver, British Columbia Canada, V6C 1E1 Phone 604.688.5077 Fax 604.688.5017 And SEAHAWK VENTURES INC. 909 Bowron Street Coquitlam, B.C. Canada, V3J 7W3 (p) 604.936.2701 (f) 604.936.2701 Prepared by: AURORA GEOSCIENCES LTD. Main Office: 3506 McDonald Drive, Yellowknife, NT, X1A 2H1 Phone: (867) 902.2729 Fax: (867) 920-2739 www.aurorageosciences.com Author: Gary Vivian, M.Sc., P. Geol. QP Metallis Resources Inc. & Seahawk Ventures Inc. Aurora Geosciences Ltd. Table of Contents 1 SUMMARY ..................................................................................................................................................... 1 2 INTRODUCTION ............................................................................................................................................. 3 3 RELIANCE ON OTHER EXPERTS ....................................................................................................................... 4 4 PROPERTY LOCATION AND DESCRIPTION ..................................................................................................... -
Geology of the Maudina Mine Area, Northern Santa Catalina Mountains, Pinal County, Arizona
Geology of the Maudina Mine area, northern Santa Catalina Mountains, Pinal County, Arizona Item Type text; Thesis-Reproduction (electronic); maps Authors Bromfield, Calvin Stanton, 1923- Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 28/09/2021 04:41:04 Link to Item http://hdl.handle.net/10150/553781 GEOLOGY OF THE MAUDINA MINE AREA, NORTHERN SANTA CATALINA MOUNTAINS, PINAL COUNTY, ARIZONA by Calvin S. Bromfleld M A Thesis submitted to the faculty of the Department of Geology in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE in the Graduate College, University of Arizona 1950 Approved: Director of Thesis aniM AHIOT'Ah 2HT TC TBCJOaO A8 51. Xfl t) \ bi °itnio*!t? .2 «JLvl/,D alaoriT & edcr c j AaJiimcfu# ad Of 4^ 5" ' % Nt. A / tTR^A osejc !6* voiacA iigsw w ^ r m s ----- - £ <H1C\\ CONTENTS Page H H H m Introduction...................... Location..................... Previous Investigations...... Field Work and Acknowledgments Climate...................... Topography................... General Geology.................................. 9 General Statement........................... 9 Sedimentary RocKs......................... 12 Cambrian System...................... 12 Middle Cambrian................. 12 Troy quartzite............. 12 Santa Catalina formation.... 14 Southern Belle quartzite.... 17 Upper Cambrian.................. 18 . Abrigo formation........... 18 Peppersauce sandstone...... 20 Devonian System...................... 22 Upper Devonian................. 22 Martin limestone.......... 22 Lower Ouray formation..... 25 Misslssippian System................ 27 Lower Misslssippian............ 27 Escabrosa limestone....... 27 Cretaceous System................... 31 Cretaceous Strata.............