DOGAMI Open-File Report O-89-10, Bibliography of Oil and Gas

Total Page:16

File Type:pdf, Size:1020Kb

DOGAMI Open-File Report O-89-10, Bibliography of Oil and Gas STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES 910 State Office Building 1400 SW Fifth Avenue Portland, Oregon 97201 OPEN-FILE REPORT 0-89-10 BIBLIOGRAPHY OF OIL AND GAS EXPLORATION AND DEVELOPMENT IN OREGON, 1896-1989 by Dennis L. Olmstead Oregon Department of Geology and Mineral Industries GOVERNING BOARD STATE GEOLOGIST Donald A. Hull Donald A. Haagensen, Chair Portland Sidney R. Johnson Baker DEPUTY STATE GEOLOGIST Ronald K. Culbertson Myrtle Creek John D. Beaulieu The Oregon Department of Geology and Mineral Industries is publishing this paper because the subject matter is consistent with the mission of the Depart- ment. To facilitate timely distribution of information, this report has not been edited to our usual standards. CONTENTS Page Introduction ........................................1 Bibliography of oil and gas exploration and development ... 3 County index to the bibliography ......................... 35 iii INTRODUCTION This bibliography was compiled in connection with the preparation of Hydrocarbon Exploration and Occurrences in Oregon, published by the Oregon Department of Geology and Mineral Industries (DOGAMI) as Oil and Gas Investigation 15 (OGI-15), and is being released concurrently as a supplement to that report. Whereas DOGAMI OGI-15 contains a list of only the references cited, this bibliography is an effort to provide a comprehensive listing of references relevant to oil and gas exploration in Oregon. It is not intended to be exhaust- ive but includes most of the relevant citations in the literature that are known to the author. The bibliography consists of two parts: an author list and a county index. To help locate references for a specific area, pertinent citations are listed under the respective county in an abbreviated form that refers back to the author list. Entries covering large or diverse areas are not listed in the county index. BIBLIOGRAPHY OF OIL AND GAS EXPLORATION AND DEVELOPMENT IN OREGON, 1896-1989 Addicott, W.O., 1976, Neogene molluscan stages of American Gas Association Monthly, 1965, Underground Oregon and Washington, & Fritsche, A.E., and storage, a good neighbor: American Association others, eds., Neogene Symposium: Society of Monthly, v. 47, no. 19. Economic Paleontologists and Mineralogists, Amoco Production Company, 1982, Palynology and Pacific Section, San Francisco, Calif., April stratigraphy from selected wells in Oregon: 1976, p. 95-115. Unpublished report on file at Oregon Depart- Ahmad, R., 1981, Stratigraphy, structure, and ment of Geology and Mineral Industries (DOGAMI petrology of the Lookingglass and Roseburg Oil and Gas Contract 6). Formations, Agness-Illahe area, southwestern Anderson, F.M., 1938, Lower Cretaceous deposits in Oregon: Eugene, Oreg., University of Oregon California and Oregon: Geological Society of master's thesis, 150 p. America Special Paper 16, 339 p. ------ 1982, Comment on "Provenance of Eocene Anderson, R.W., 1963, Geology of the northwest graywackes of the Flournoy Formation near quarter of the Brownsville Quadrangle, Oregon: Agness, Oregon--a geochemical approach": Eugene, Oreg., University of Oregon master's Geology, v. 10, no. 6, p.. 333-334. thesis, 62 p. Al-Azzaby, F.A., 1980, Stratigraphy and sedimen- Annentrout, J.M., 1967, The Tarheel and Empire tation of the Spencer Formation in Yamhill and Formations, geology and paleontology of the Washington Counties, Oregon: Portland, Oreg., type sections, Coos Bay, Oregon: Eugene, Portland State University master's thesis, Oreg., University of Oregon master's thesis, 104 p. 155 p. Alemi, M., 1979, A gravity survey of Coos Bay, ------1973, Molluscan biostratigraphy and pa- Oregon: Eugene, Oreg., University of Oregon leontology of the Lincoln Creek Formation master's thesis, 72 p. (late Eocene-Oligocene), southwestern Wash- Allen, J.E., and Baldwin, E.M., 1944, Geology and ington: Seattle, Wash., University of coal resources of the Coos Bay Quadrangle, Washington doctoral dissertation, 479 p. Oregon: Oregon Department of Geology and Min- ------1980, Field trip road log for the Cenozoic eral Industries Bulletin 27, 157 p, 1 pl., stratigraphy of Coos Bay and Cape Blanco, scale 1:96,500. southwestern Oregon, & Oles, K.F., Johnson, Allen, J.E., and Beaulieu, J.D., 1976, Plate- J.G., Niem, A.R., and Niem, W.A., eds., Geo- tectonic structures in Oregon: Oregon Depart- logic field trips in western Oregon and ment of Geology and Mineral Industries, Ore southwestern Washington: Oregon Department of Bin, v. 38, no. 6, p. 87-99. Geology and Mineral Industries Bulletin 101, Allison, I.S., 1953, Geology of the Albany Quad- p. 177-216. rangle, Oregon: Oregon Department of Geology ------ 1981, Correlation and ages of Cenozoic and Mineral Industries Bulletin 37, 18 p, 1 chronostratigraphic units in Oregon and Wash- pl., scale 1:62,500. ington, & Armentrout, J.M., ed., Pacific American Association of Petroleum Geologists, Northwest Cenozoic biostratigraphy: Geological Pacific Section, 1941, Possible future oil Society of America Special Paper 184, p. 137- provinces in Pacific Coast states: AAPG 148. Bulletin, v. 25, no. 8, p. 1475-1468. Annentrout, J.M., Cole, M.R., and TerBest, H., Jr., American Association of Petroleum Geologists and eds., 1979, Cenozoic paleogeography of the U.S. Geological Survey, 1967, Basement map of western United States: Pacific Coast Paleo- North America between latitudes 24O and 60' geography Symposium 3, Anaheim, Calif., N.: U.S. Geological Survey Special Map, scale Society of Economic Paleontologists and Min- 1:500,000. eralogists, Pacific Section, Publication 9, 335 p. Armentrout, J.M., Echols, R.J., and Ingle, J.C., ------ 1966, Some revisions of the geology of the Jr., 1984, Neogene biostratigraphic-chronos- Coos Bay area, Oregon: Oregon Department of tratigraphic scale for the northeastern Geology and Mineral Industries, Ore Bin, v. Pacific margin, & Ikebe, N., and Tuschi, 28, no. 11, p. 189-203. R., Pacific Neogene datum planes: Contribu- ------ 1974, Eocene stratigraphy of southwestern tions to biostratigraphy and chronology: Oregon: Oregon Department of Geology and Min- Tokyo, Japan, University of Tokyo Press, p. eral Industries Bulletin 83, 40 p. 171-177. ------1975, Revision of the Eocene stratigraphy Armentrout, J.M., Hull, D.A., Beaulieu, J.D., and of southwestern Oregon, & Weaver, D.W., Rau, W.W., 1983, Correlation of Cenozoic Hornaday, G.R., and Tipton, A., eds., Paleo- stratigraphic units of western Oregon and gene symposium and selected technical papers: Washington: Oregon Department of Geology and 50th Annual Meeting, Pacific Sections, AAPG, Mineral Industries Oil and Gas Investigation SEPM, SEG, Long Beach, Calif., April 1975, p. 7, 90 p. 49-64. Armentrout, J.M., McDougall, K., Jefferis, P.T., ------1981, Geology of Oregon, 3rd. ed.: Dubuque, and Nesbitt, E., 1980, Geologic field trip Iowa, KendallIHunt Publishing Company, 170 p. guide for the Cenozoic stratigraphy and late Baldwin, E.M., Beaulieu, J.D., Ramp, L., Gray, Eocene paleoecology of southwestern Washing- J.J., Newton, V.C., Jr., and Mason, R.S., ton: Oles, K.F., Johnson, J.G., Niem, 1973, Geology and mineral resources of Coos A.R., and Niem, W.A., eds., Geologic field County, Oregon: Oregon Department of Geology trips in western Oregon and southwestern and Mineral Industries Bulletin 80, 82 p. Washington: Oregon Department of Geology and Baldwin, E.M., Brown, R.D., Jr., Gair, J.E., and Mineral Industries Bulletin 101, p. 79-119. Pease, M.H., Jr., 1955, Geology of the Sheri- Armentrout, J.M., and Suek, D.H., 1982, Hydro- dan and McMinnville Quadrangles, Oregon: U.S. carbon exploration in western Oregon and Geological Survey Oil and Gas Investigations Washington [abs.]: AAPG Bulletin, v. 66, no. Map OM-155, scale 1:62,500. 5, p. 544. Baldwin, E.M., and Roberts, A.E., 1952, Geology ------ 1985, Hydrocarbon exploration in western of the Spirit Mountain Quadrangle, northwest- Oregon and Washington: AAPG Bulletin, v. 69, ern Oregon: U.S. Geological Survey Oil and no. 4, p. 627-643. Gas Investigations Map OM-129, scale Armentrout, J.M., and Ulrich, A.F., 1983, Tec- 1:48,000. tonic control of Eocene arkosic sediment de- Bales, W.E., and Kulm, L.D., 1969, Structure of position, Oregon and Washington [abs.]: AAPG the continental shelf off southern Oregon Bulletin, v. 67, no. 3,.p. 413-414. [abs.]: AAPG Bulletin, v. 53, no. 2, p. 471. Atwater, T., 1970, Implications of plate tecton- Barlow, J.L., 1955, The geology of the central ics for the Cenozoic tectonic evolution of third of the Lyons Quadrangle, Oregon: Eu- western North America: Geological Society of gene, Oreg., University of Oregon master's America Bulletin, v. 81, no. 12, p. 3513- thesis, 79 p. 3535. Barnes, T.J., 1978, Geology of the Sand Mountain Axelrod, D.I., 1968, Tertiary floras and topo- area, western Wheeler County, Oregon: Corval- graphic history of the Snake River basin, lis, Oreg., Oregon State University master's Idaho: Geological Society of America Bul- thesis, 119 p., map scale 1:24,000. letin, v. 79, no 6, p. 713-733. Barrash, W., Bond, J.G., and Venkatakrishnan, R., Baldwin, E.M., 1945, Some revisions of the late 1983, Structural evolution of the Columbia Cenozoic stratigraphy of the southern Oregon Plateau in Washington and Oregon: American coast: Journal of Geology, v. 53, no. 1, p. Journal of Science, v. 283, no. 9, p. 897- 35-46. 935. ------ 1955, Geology of the Marys Peak and Alsea Bateman, R.L., 1961, The geology of the south- Quadrangles, Oregon: U.S. Geological Survey central part of the Sawtooth Creek Quadran- Oil and Gas Investigations Map OM-162, scale gle, Oregon: Eugene, Oreg., University of 1:62,500. Oregon master's thesis, 97 p., map scale - -----1956, Geologic map of the lower Siuslaw 1:24,000. River area, Oregon: U.S. Geological Survey Beaulieu, J.D., 1971, Geologic formations of Oil and Gas Investigations Map OM-186, scale western Oregon (west of longitude 121'30'): 1:62,500. Oregon Department of Geology and Mineral - ----- 1961, Geologic map of the lower Umpqua Industries Bulletin 70, 72 p.
Recommended publications
  • Redbeds of the Upper Entrada Sandstone, Central Utah
    Brigham Young University BYU ScholarsArchive All Theses and Dissertations 2016-12-01 Redbeds of the Upper Entrada Sandstone, Central Utah: Facies Analysis and Regional Implications of Interfingered Sabkha and Fluvial Terminal Splay Sediments Jeffery Michael Valenza Brigham Young University Follow this and additional works at: https://scholarsarchive.byu.edu/etd Part of the Geology Commons BYU ScholarsArchive Citation Valenza, Jeffery Michael, "Redbeds of the Upper Entrada Sandstone, Central Utah: Facies Analysis and Regional Implications of Interfingered Sabkha and Fluvial Terminal Splay Sediments" (2016). All Theses and Dissertations. 6112. https://scholarsarchive.byu.edu/etd/6112 This Thesis is brought to you for free and open access by BYU ScholarsArchive. It has been accepted for inclusion in All Theses and Dissertations by an authorized administrator of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. Redbeds of the Upper Entrada Sandstone, Central Utah: Facies Analysis and Regional Implications of Interfingered Sabkha and Fluvial Terminal Splay Sediments Jeffery Michael Valenza A thesis submitted to the faculty of Brigham Young University in partial fulfillment of the requirements for the degree of Master of Science Thomas H. Morris, Chair Jani Radebaugh Sam Hudson Scott M. Ritter Department of Geological Sciences Brigham Young University Copyright © 2016 Jeffery Michael Valenza All Rights Reserved ABSTRACT Redbeds of the Upper Entrada Sandstone, Central Utah: Facies Analysis and Regional Implications of Interfingered Sabkha and Fluvial Terminal Splay Sediments Jeffery Michael Valenza Department of Geological Sciences, BYU Master of Science First distinguished from other sedimentary successions in 1928, the Entrada Sandstone has been the subject of numerous studies.
    [Show full text]
  • Geologic Formations of Western Oregon
    BULLETIN 70 GEOLOGIC fORMATION§ OF WESTERN OREGON WEST OF LONGITUDE 121° 30' STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES 1971 STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES 1069 Stal·e Office Building Portland, Oregon 97201 BULLETIN 70 GEOLOGIC FORMATIONS OF WESTERN OREGON (WEST OF LONGITUDE 12 1 °30') By John D. Beaulieu 1971 GOVERNING BOARD Fayette I. Bristol, Rogue River, Chairman R. W. deWeese, Portland Harold Banta, Baker STATE GEOLOGIST R. E. Corcoran CONTENTS Introduction . Acknowledgements 2 Geologic formations 3 Quadrang I es. 53 Corre I ation charts. 60 Bibliography. 63 ii GE OLOGIC FORMA T IONS OF WESTERN OR EGON (W E ST OF LONG ITUD E 12 1°30') By John D. Beaulieu* INTRODUCTION It is the purpose of th is publi cation to provide a concise , yet comprehensive discussion of the for­ mations of western Oregon. It is the further aim that the data for each of the formations be as current as possi ble. Consequently, the emphasis has been placed on th e recent literature . Although this paper should not be viewed as a discussion of the historical development of each of the fo rmations, the original reference for each of the units is given . Also, in cases where the historical development of the formation has a direct bearing on present-day problems it is included in the discussion . A wide variety of published literature and unpublished reports , theses, and dissertations was con­ sul ted and several professional opin ions regarding specific problems were so licited . In recent years re­ search has been concentrated in the Klamath Mountains and the southern Coast Range and for these regions literature was volumi nous.
    [Show full text]
  • Cambrian Shelf Deposits of the King Square Formation, Saint John Group, Southern New Brunswick Saifullah K
    Document generated on 09/26/2021 6:59 p.m. Atlantic Geology Cambrian shelf deposits of the King Square Formation, Saint John Group, southern New Brunswick Saifullah K. Tanoli and Ron K. Pickerill Volume 25, Number 2, August 1989 Article abstract The upper Middle Cambrian to early Late Cambrian King Square Formation, URI: https://id.erudit.org/iderudit/ageo25_2art03 Saint John Group, southern New Brunswick, is an approximately 380 m thick silicilastic sequence of interbedded fine-grained sandstones and siltstones and See table of contents shales. On the basis of sandstone to shale/siltstone ratios, bed thickness and characteristics, sedimentary structures and degree of bioturbation three lithofacies are recognized. These are facies KS1, thin bedded sandstone and Publisher(s) shale lithofacies; KS2, thick bedded sandstone lithofacies; and KS3, bioturbatcd shale and siltstone with interbedded sandstone lithofacies. These lithofacies Atlantic Geoscience Society are interpreted to havebeen deposited on a wave- and storm-influenced marine subtidal shelf. Facies KS 1 was deposited essentially below wave base ISSN though in its upper horizons, deposition may have occurred above storm wave base. Facies KS2 was essentially deposited in a shallower subtidal inner- to 0843-5561 (print) mid-shelf environment above storm wave base and facies KS3 initially above 1718-7885 (digital) and latterly below storm wave base. The exact nature of the currents responsible for transportation and deposition of the storm-related sandstones Explore this journal (geostrophic flows or turbidity currents) is impossible to determine and therefore palaeocurrent data must be interpreted with caution. The stratigraphic arrangement of the lithofacies, with facies KS1 being the oldest Cite this article and KS3 the youngest, suggests that the King Square Formation represents a regressive-transgressive sequence.
    [Show full text]
  • Us Department of the Interior
    U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Preliminary map of selected post-Nevadan geologic features of the Klamath Mountains and adjacent areas, California and Oregon Compiled by William P. Irwin1 Geologist Emeritus Open-File Report 97-465 1997 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1Menlo Park, California 94025 This map of selected post-Nevadan features is in a sense supplementary to Map I-2148 (Geologic map of the Klamath Mountains, compiled by W.P. Irwin, 1994). The map of selected post-Nevadan geologic features is in large part a compilation of the published work of many geologists (see Fig. 1--Index map showing sources of data). The principal new data are the outlines of remnants of old upland surfaces (unit "os" on the map) that are present mainly in a north-trending zone in the western Klamath Mountains and in a sub-parallel zone nearby in the Coast Ranges. The old upland surfaces were drawn mainly by interpretation of standard USGS topographic maps--mostly 1:62,500-scale but in some instances 1:100,000-scale maps. Old upland surfaces in the Coast Ranges west of the Klamath Mountains in Oregon, although present, are not shown. The principal focus of Map I-2148 concerned the assemblage of terranes that constitute the principal bedrock of the Klamath Mountains.
    [Show full text]
  • DOGAMI Bulletin 83, Eocene Stratigraphy of Southwestern Oregon
    EOCENE STRATIGRAPHY OF SOUTHWESTERN OREGON 1974 STATE OF OREGON DEPARTMENT OF GEOLOGY AND MI NERAL INDUSTRIES l 069 State Office Building , Portland, Oregon 97201 BULLETIN 83 EOCENE STRATIGRAPHY OF SOUTHWEST ERN OREGON Ew art M. Baldwin Department of Geology University of Oregon GOVERNING BOARD R. W. deWeese, Chairman, Port land Wil liam E. Mil ler Bend H. Lyle Van Gordon Grants Pass STATE GEOLOGIST R. E. Corcoran 1974 FOREWORD So uthwestern Oregon has had a long history of mineral production dating back to the 1850's. Coal was discovered in Eocene marine sediments of the southern Coast Ra nge near Coos Bay in 1854. By 1880, when records were first kept, production was about 40, 000 tons a year, and for 15 years annua I production ranged between 30, 000 and 75, 000 tons. Sh ortly after th e turn of the century , pe troleum discoveries in Cal­ ifornia caused most rai lroad and steamship lines on the West Coast to switch to fuel oil, and coalmining at Coos Bay declined rapidly. The first detai I ed survey of the Coos County coo Is was made in 1896 for the U.S. Geological Su rvey by J. S. Dil ler. In the course of his studies, Dil ler compi led sev­ eral geologic maps and reports showing the exten t of the Eocene rocks and named and described many of the stratigraph ic units. His work forms the basis of all subsequent investigations on the Tertiary stratigraphy of the Coast Range and encouraged subse­ quent search for oi I and gas in western Oregon .
    [Show full text]
  • Geology of Oregon Orr Orr.Pdf
    Fifth Edition Geology of Oregon Elizabeth L. Orr William N. Orr University of Oregon Cover: Ripple-marked sand dunes on the Oregon Coast resemble a gigantic fingerprint (photo by Gary Tepfer). Copyright ® 1964 by Ewart M. Baldwin Copyright ® 1976, 1981, 1992, 2000 by Kendall/Hunt Publishing Company ISBN 0-7872-6608-6 All rights reserved. No part of this publication may be reproduced, stored in a retrieval system, or transmitted, in any form or by any means, electronic, mechanical, photocopying, recording, or otherwise, without the prior written permission of the copyright owner. Printed in the United States of America 10 98765432 Table of Contents Introduction 1 History of geologic study in Oregon 9 Blue Mountains 21 Klamath Mountains 51 Basin and Range 79 High Lava Plains 103 Deschutes-Columbia Plateau 121 Cascade Mountains 141 Coast Range 167 Willamette Valley 203 Bibliography 223 Glossary 245 Index 251 iii Dedicated to the graduates Acknowledgments Between the fourth and fifth editions of Geology of Oregon, the importance of global tectonics to the state has been ingrained even deeper. Riding on the leading edge of the moving North American plate, Oregon reflects the underlying mecha- nism of the plate collision boundary in virtually all aspects of its geology. In the seven years since the fourth edition was written, an irregular but continuing drumbeat of earthquakes reminds us of the forces beneath our feet and the need to prepare for catastrophic changes be they quakes, volcanoes, tsunamis, floods, or massive earth movements. Most profound is the discovery of irrefutable evidence that these catastrophes have been visited on the state quite regularly over the past few thousands of years as well as the absolute surety that similar disasters will oc- cur in the near and distant future.
    [Show full text]
  • Depositional Environments of the Pictured Cliffs Sandstone, Late Cretaceous, Near Durango, Colorado1
    Depositional Environments of the Pictured Cliffs Sandstone, Late Cretaceous, near Durango, Colorado1 FRANK J. TOKAR JR. AND JAMES E. EVANS, Department of Geology, Bowling Green State University, Bowling Green, OH 43403 ABSTRACT. The Pictured Cliffs Sandstone was deposited in the northwestern part of the San Juan Basin (Colorado-New Mexico) during the last regression of the Cretaceous Interior Seaway. The unit is generally interpreted as deltaic or marginal marine; however, outcrops near Durango, CO, consist of repetitive sequences of hummocky stratified (HS) sandstone. Each HS sequence consists of a scoured surface overlain by hummocky-stratified, fine-grained sandstone 20-50 cm thick, overlain by ripple- to planar- laminated, bioturbated, very fine-grained sandstone to mudstone. Amalgamated HS sequences are as much as 7 m thick. Hummocky stratification is an important sedimentary structure indicating storm deposits (tempestites) in the geological record. Rocks containing HS have been found throughout the world, including Ohio. The goal of this research was to apply field and laboratory methods to the re-interpretation of the Pictured Cliffs Sandstone in recognition of the significance of HS. In this region, the Pictured Cliffs Sandstone was deposited on a storm-dominated, sandy shelf at depths between fair-weather and storm-weather wavebase (about 10 m). Individual storm events are represented by a single HS sequence. Some HS sequences are amalgamated because of either bioturbation or erosion of the upper part of the sequence by subsequent storm events. The thick sand bodies suggest that significant amounts of sediment were transported along the shelf during progradation of the shoreline. During storm events these sediments were resuspended and re-deposited, creating the HS sequences.
    [Show full text]
  • Stratigraphy of the Cretaceous Hornbrook Formation, Southern Oregon and Northern California
    Stratigraphy of the Cretaceous Hornbrook Formation, Southern Oregon and Northern California U.S. GEOLOaieAk SURVEY PROFESSI0 JJAl FAFER Stratigraphy of the Cretaceous Hornbrook Formation, Southern Oregon and Northern California By TOR H. NILSEN U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1521 A stratigraphic division of the Hornbrook Formation into five nonmarine and marine members UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1993 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, 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 Illustrations edited by Dale Russell and prepared by Michelle Coveau Library of Congress Cataloging in Publication Data Nilsen, Tor Helge. Stratigraphy of the Cretaceous Hornbrook Formation, southern Oregon and northern California / by Tor H. Nilsen. p. cm. (U.S. Geological Survey professional paper ; 1521) Includes bibliographical references. Supt. of Docs, no.: I 19.16:1521 1. Geology, Stratigraphic Cretaceous. 2. Geology California. 3. Geology Oregon. 4. Hornbrook Formation (Calif, and Or.) I. Title. II. Series. QE685.N55 1993 551.7'7'097952 dc20 , 93-3585 CIP For sale by Book and Open-File Report Sales, U.S. Geological Survey, Federal Center, Box 25286, Denver, CO 80225 CONTENTS Page Page Abstract________________________________ __ 1 Stratigraphic subdivisions of the Hornbrook Formation Introduction 1 Continued Previous work 5 Rocky Gulch Sandstone
    [Show full text]
  • Geology of the Green Mountain-Young's River Area, Clatsop County, Northwest Oregon Recicted for Privacy Abstract Approved: (Alan R
    AN ABSTRACT OF THE THESIS OF Carolyn Pugh Peterson for the degree of Master of Science in Geology presented on December 12, 1983 Title: Geology of the Green Mountain-Young's River Area, Clatsop County, Northwest Oregon Recicted for Privacy Abstract Approved: (Alan R. Niem) The upper Eocene to lower Oligocene Oswald West mudstone is the oldest formation (informal) in the Green Mountain-Young's River area. This 1,663 meter thick hemipelagic sequence was depos- ited in a low-energy lower to upper slope environment in the Coast Range forearc basin. The formation ranges from the late Narizian to the early Zemorrian(?) in age and consists of thick-bedded bio- turbated foraminiferal claystone and tuffaceous siltstone. Rare glauconitic sandstone beds also occur. In the eastern part of the study area, the upper part of the Oswald West mudstone is inter- bedded with the upper Refugian Klaskanine siltstone tongue. This informal unit consists of thick bioturbated sandy siltstone and silty sandstone that is a lateral deep-marine correlative of the deltaic to shallow-marine Pittsburg Bluff Formation in the north- eastern Coast Range. Discontinuous underthrusting of the Juan de Fuca oceanic plate at the base of the continental slope of the North American plate caused extensive uplift and subsidence along the Oregon continental margin throughout the Cenozoic (Snavely et al., 1980). Initiation of Oregon Coast Range uplift and accompanying erosion in the early Miocene, coupled with a global low stand of sea level (Vail and Mitchum, 1979), stripped most of the Oligocene (Zemor- rian) Oswald West strata and in places much of the uppermost Eocene (upper Refugian) Oswald West strata in the field area, cre- ating an unconformity.
    [Show full text]
  • Bourgeois 1980 Trans
    TransactionNumber: 172487 1111111111111111111111111111111111111111 Call #: QE420 .JG per Location: Article Information Journal Title: Journal of Sedimentary Petrology Volume: 50 Issue: 3 S Month/Year: 1980Pages: 681-702 n ~ Article Author: ~ ~ Article Title: A transgressive shelf sequence exhibiting hummocky stratification; The Cape Q) Sebastian Sandstone (Upper Cretaceous), southwestern Oregon ;:j O" Q) Loan Information ~ Loan Title: Loan Author: Publisher: Place: Date: Imprint: Customer Information A TRANSGRESSIVE SHELF SEQUENCE EXHIBITING HUMMOCKY STRATIFICATION: THE CAPE SEBASTIAN SANDSTONE (UPPER CRETACEOUS), SOUTHWESTERN OREGON 1 JOANNE BOURGEOIS Department of Geology and Geophy sics University of Wisconsin, Madison , Wisconsin 53706 ABSTRA CT: In the tectonically active Circum-Pacific Belt, thick transgressive sequences are not uncom­ mon, in contrast with their rarity in the Cretaceous of the Western Interior. Thick transgressive sediment packages reflect rapid sedimentation rates but even more rapid rates of relative sea-level rise . A well-exposed example is the Cape Sebastian Sandstone, a 200-m thick , fining-upward sequence representing foreshore to offshore deposition. Progressively increasing depth of deposition is indicated by both physical and biogenic sedimentary structures in the Cape Sebastian Sandstone. Four facies make up the Cape Sebastian Sandstone. The lowest unit is a basal, shelly, boulder conglomerate overlain by trough cross-bedded pebbly sandstone, plane-laminated coarse sandstone, and crudely graded conglomerates. A single type of subvertical trace fo ssil is locally abundant. These sediments represent beach to nearshore deposition. The middle and thickest part of the formation comprises hummocky-bedded sandstone, divided into a lower hummocky-bedded facies and an upper hummocky-bedded and burrowed facies. Grain size, frequency of pebble lenses, and thickness of hummocky laminae all decrease upward through this part of the sequence.
    [Show full text]
  • DOGAMI Bulletin 69, Geology of the Southwestern Oregon Coast West of the 124Th Meridian
    BULLETIN 69 - GEOLOGY OF THE SOUTHWESTERN OREGON COAST WEST OF THE 124!!!. MERIDIAN STATE OF OREGON DEPARTMENT 01-' GEOLOGY AND MINERAL INDUSTRIES 1971 BULLETIN 69 STATE OF OREGON DEPA RTMENT OF GEOLOGY AND MINERAL INDUSTRIES 1069 Stote OHiee Building Portland, Oregon 97201 BULLETIN 69 GEOLOGY OF THE SOUTHWESTERN OREGON COAST WEST OF THE 124th MERIDIAN By R. H. Oou, Jr. University of Wisconsin, Modison, Wisconsin 1971 GOVERNING BOARD Foyelte 1. Bristol, Rogue River, Choirmon R. W. deWeese, Portlond Harold 6onto, Boker STATE GEOLOGIST R. E. Corcoran FOREWORD The Klamath Mountains Province of southwestern Oregon is probably one of the mOre geologically inter .. esting regions in the state. Historically1 it was in this pcwt of Oregon, near the present town of Jocks:on­ ville, that gold was discovered in 1850. Since that time, several million dollars in precious metals, copper, mercury, chromium, and nickel hove been mined from this highly mineralized region. Mineral exploration is still being carried on in the Klamath Mountains byprivate COR1>onies in the hope of finding new- deposits. One of the primory functions of the State of Oregon Deportment of Geology and Mineral Industries is to encouroge development of our mineral resources in OC"der to enhance the economy of the state and to provide the row mote.-iols required by our technological society. At the present time, yearly per-c:opito demand for minerals is obovt SISO. The U.S. Bureau of Mines believes that by the yeor 2000ovr require­ ment will be approximately S420. In order to corry out o mining-exploration program in the most efficient monnet, it is necessory to utilize all ovailable geologic mopping.
    [Show full text]
  • Stratigraphy and Depositional Environments of the Fox Hills Formation (Upper Cretaceous), Bowman County, North Dakota Daniel J
    University of North Dakota UND Scholarly Commons Theses and Dissertations Theses, Dissertations, and Senior Projects 1984 Stratigraphy and depositional environments of the Fox Hills Formation (Upper Cretaceous), Bowman County, North Dakota Daniel J. Daly University of North Dakota Follow this and additional works at: https://commons.und.edu/theses Part of the Geology Commons Recommended Citation Daly, Daniel J., "Stratigraphy and depositional environments of the Fox Hills Formation (Upper Cretaceous), Bowman County, North Dakota" (1984). Theses and Dissertations. 67. https://commons.und.edu/theses/67 This Thesis is brought to you for free and open access by the Theses, Dissertations, and Senior Projects at UND Scholarly Commons. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of UND Scholarly Commons. For more information, please contact [email protected]. STRATIGRAPHY AND DEPOSITIONAL ENVIRONMENTS OF THE FOX HILLS FORMATION (uPPER CRETACEOUS), BOWMAN COUNTY, NORTH DAKOTA by Daniel J. Daly Bachelor of Arts, New Mexico Highlands University, 1974 A Thesis Submitted to the Graduate Faculty of the University of North Dakota in partial fulfillment of the requirements for the degree of Master of Science Grand Forks, North Dakota May 1984 GED~-· -< 1 ~ "1,d 1 : I ' , '.,,~_i)' 1•11., . This thesis submitted by Daniel J. Daly in partial fulfillment of the requirements for the Degree of Master of Science from the University of North Dakota is hereby approved by the Faculty Advisory Committee
    [Show full text]