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Timing and Structural Expression of the Nevadan Orogeny, Sierra Nevada, California: Discussions and Reply
Timing and structural expression of the Nevadan orogeny, Sierra Nevada, California: Discussions and reply Discussion TAPAS BHATTACHARYYA i _ „ . _ . ,, . , _ ... „ , _ _ ,., . nATi-DCAM I ^art'1 Science Board, University of California, Santa Cruz, California 95064 SCO IT R. PA [ bKSON / Prior to commenting on several aspects of the paper by Schweickert and others, 1984, can be divided into four topics: (1) the position/exist- and others, 1984, we wish to note that we have benefited from the work of ence of the "Sonora fault," (2) the "polymetamorphism and structural these authors. We also wish to note that all of our comments concern complexity" of the Calaveras Complex and Shoo Fly Formation, (3) the statements made about the southern portion of the Western Metamorphic interpretation of "Late Phase" or Cretaceous folds and possible conjugate Belt where we are presently completing an east-west transect on scales of structures, and (4) their model for "rigid body rotation of the central belt" 1:24,000 and larger. during Nevadan deformation. We will discuss each of these in turn. Our objections to observations and interpretations by Schweickert 1. Many of the age relations and positions of contacts/faults dis- cussed by Schweickert and others, 1984, are better established in the The article discussed appeared in the Bulletin, v. 95, p. 967-979. northern Sierra or the part of the southern belt which lies north of 3£ We Geological Society of America Bulletin, v. 96, p. 1346-1352, 1 fig., October 1985. Downloaded from http://pubs.geoscienceworld.org/gsa/gsabulletin/article-pdf/96/10/1349/3445091/i0016-7606-96-10-1349.pdf by guest on 02 October 2021 DISCUSSIONS AND REPLY 1347 think that similar relations are not nearly so well established in the south- Belt. -
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. -
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. -
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. -
Review of Cordilleran Tectonics
The Wacky Wonderful World of Cordilleran Tectonics Event Timing Description Transform Tectonics Middle Miocene - As North American Plate overran the divergent boundary of the Farallon and Pacific plates, change in sense of along California Coast Holocene motion from subduction to transform; birth of San Andreas Fault system; sealing off of southern entrance to Great Valley of California as sliver of crust containing Baja California and Los Angeles moves northward Half-graben Rise of Late Pliocene Large scale tilting of old plutons (emplaced in Nevadan orogeny) in eastern California, producing modern Sierra Sierra Nevada Nevada Basin-and-Range Miocene – Pliocene Large-scale extension in American Southwest, thinning continental crust and widening region by 50-100%; Extension & Volcanism associated regional volcanism Coastal Range Orogeny Late Miocene – Subduction along western coastline producing Andean-style volcanoes (Coastal Ranges of California, Cascades of Holocene Northwest); continues to operate in Northwest Flood Basalts in Miocene – Pliocene Columbia River Basalts (Miocene); Snake River Extrusives (Pliocene) Northwest Uplift of Colorado Middle Miocene Large vertical uplift of flat region in American Southwest, with little internal disturbance; downward erosion of Plateau Colorado River produces Grand Canyon Exhumation of the Early Miocene – Uplift of ~1600 m; erosion of much of the alluvium formed in the Oligocene; downward cutting action of rivers Rockies Pliocene produces “meandering” streams inside mountains Erosion of Cordillera Oligocene Erosion of Laramide uplift produces alluvium which largely fills up the intramontane basins and which spreads in large wedges into the cratonic interior; meandering rivers eventually form on these wedges. The tops of the mountains are weathered down to form broad flat surfaces confluent with the alluvial wedges. -
The Structural and Metamorphic History of the Oakhurst Roof Pendant, Mariposa and Madera Counties, California
UNLV Theses, Dissertations, Professional Papers, and Capstones 12-1972 The structural and metamorphic history of the Oakhurst roof pendant, Mariposa and Madera counties, California Lee R. Russell Texas Tech University Follow this and additional works at: https://digitalscholarship.unlv.edu/thesesdissertations Part of the Geology Commons, and the Tectonics and Structure Commons Repository Citation Russell, Lee R., "The structural and metamorphic history of the Oakhurst roof pendant, Mariposa and Madera counties, California" (1972). UNLV Theses, Dissertations, Professional Papers, and Capstones. 1443. http://dx.doi.org/10.34917/3432680 This Thesis is protected by copyright and/or related rights. It has been brought to you by Digital Scholarship@UNLV with permission from the rights-holder(s). You are free to use this Thesis in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/ or on the work itself. This Thesis has been accepted for inclusion in UNLV Theses, Dissertations, Professional Papers, and Capstones by an authorized administrator of Digital Scholarship@UNLV. For more information, please contact [email protected]. THE STRUCTURAL AND METAMORPHIC HISTORY OF THE OAKHURST ROOF PENDANT, MARIPOSA AND MADERA COUNTIES, CALIFORNIA by LEE R. RUSSELL, B.A. A THESIS IN GEOLOOY Submitted to the Graduate Faculty of Texas Tech University in Partial Fulfillment of i. the Requ~rements for .the Degree of MASTER OF SCIENCE Director December, 1972 .. ,.,... --- ----------·~ AC: £tJ5' 13 !97Z (\)o. -
Moores Et Al..Fm
International Geology Review, Vol. 44, 2002, p. 479–500. Copyright © 2002 by V. H. Winston & Son, Inc. All rights reserved. Crustal-Scale Cross-Section of the U.S. Cordillera, California and Beyond, Its Tectonic Significance, and Speculations on the Andean Orogeny E. M. MOORES,1 Department of Geology, University of California, Davis, California 95616 J. WAKABAYASHI, 1329 Sheridan Lane, Hayward, California 94544-5332 AND J. R. UNRUH William Lettis & Associates, 1777 Botelho Drive, Suite 262, Walnut Creek, California 94596 Abstract A cross-section across northern California from the San Andreas fault to central Nevada exhibits both major east- and west-vergent structures. East-vergent structures include crustal wedging and fault-propagation folds in the Coast Ranges, emplacement of the Great Valley ophiolitic basement over Sierran basement rocks, early east-vergent structures in the latter, displacement along the east- ern margin of the Sierra Nevada batholith, and thrust faults in western Nevada. West-vergent struc- tures include faults within the Franciscan complex and “retrocharriage” structures in the Sierra Nevada A model of evolution of the U.S. Pacific margin emphasizes the role of ophiolites, island arc– continental margin collisions, and subduction of a large oceanic plateau. Early Mesozoic subduction along the Pacific margin of North America was modified by a 165–176 Ma collision of a major intra- oceanic arc/ophiolite complex. A complex SW Pacific-like set of small plates and their boundaries at various times may have been present in southern California between 115 and 40 Ma. Subduction of an oceanic plateau about 85–65 Ma (remnants in the Franciscan) produced east-vergent tectonic wedging in the Coast Ranges, possible thrusting along the eastern Sierra Nevada batholith margin, and development of Rocky Mountain Laramide structures. -
Plutonism in the Central Part of the Sierra Nevada Batholith, California
Plutonism in the Central Part of the '5n«Sierra Nevada Batholith,* California *~r ._*» U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1483 Plutonism in the Central Part of the Sierra Nevada Batholith, California By PAUL C. BATEMAN U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1483 A study of the structure, composition, and pre-Tertiary history of the Sierra Nevada batholith in the Mariposa 1° by 2° quadrangle UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1992 U.S. 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 Bateman, Paul Charles, 1910- Plutonism in the central part of the Sierra Nevada batholith, California / by Paul C. Bateman p. cm. (U.S. Geological Survey professional paper ; 1483) Includes bibliographical references. 1. Batholiths Sierra Nevada Mountains (Calif, and Nev.) 2. Geology Sierra Nevada Mountains (Calif, and Nev.) I. Title. II. Series: Geological Survey professional paper ; 1483. QE11.5.U6B36 1992 91-14788 552M dc20 CIP For sale by the Books and Open-File Report Sales, U.S. Geological Survey, Federal Center, Box 25286, Denver, CO 80225 CONTENTS Page Hierarchical organization of granitic units 24 Introduction Plutons 25 Stratigraphic and structural setting Lithodemes 25 Metamorphism Late Proterozoic and Paleozoic strata of the White and Roof pendants, septa, and inclusions -
Acrobat Distiller, Job 3
Nevadan Orogeny Nevadan Orogeny • Short-lived Late Jurassic Late Jurassic deformational event (162-144 Ma) • Basis for a collided exotic arc model for Sierra Nevada-Klamath belt Reading: GNAM G3, CH. 4, pp157-168 Characteristics Josephine Ophiolite Complex • General • Best evidence for Nevadan Orogeny – Turbidite deposition across ophiolites and synchronous deformation define orogeny • Change from pelagic to flysch sedimentation • Plate edge – Fore arc basins source of ophiolites • Outer margin of basin detached & obducted • Isolated magmatism as small plutons • Process took only 10 Ma at 162 Ma ago Main Events Late Jurassic Magmatism • Final stage of fringing terrane accretion • Clusters of small plutons • Emplacement of ophiolites and arc • Zones of extension and transtension sequences • Ignimbrite fields • Turbidites deposited across ophiolite • Disruption of intrusive patterns due to: basins – Rapid growth of ophiolite basins • Synchronous deformation = Nevadan – Reversal of tangential motion orogeny patterns along plate edge 1 Strike-slip Faulting Plate Edge • Sinestral strike-slip faulting along the plate edge • Fore arc basin in California • Sinestral transpressive deformation • Great Valley • Contractile deformation in back- • Ophiolite formation arc regions Ophiolites Triassic to Middle • Late Jurassic ophiolites Jurassic • Inter-arc basin crust? • Or a loosely-coupled fore- arc domain? Ophiolite Origin Fringing Arc System • Rogue sequence • Arc basin crust between N.A. and arc system • Coast Range ophiolite • Fore arc accumulation -
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. -
Calaveras Complex Forms the Center, and the Foothills Terrane Is on the Western Side
Excerpt from Geologic Trips, Sierra Nevada by Ted Konigsmark ISBN 0-9661316-5-7 GeoPress All rights reserved. No part ofthis book may be reproduced without written permission, except for critical articles or reviews. For other geologic trips see: www.geologictrips.com 42 - Geology of the Sierra Nevada WESTERN METAMORPHIC BELT The Western Metamorphic Belt is a broad band of metamorphic rocks that lie on the west side of the Sierra Nevada batholith and extend northwest for 200 miles through the foothills of the central and northern Sierra. The south end of the belt, near Mariposa, is about 30 miles wide and the belt thickens northward to about 60 miles in the northern Sierra. The belt is divided into three major rock units that also trend northwest. The Shoo Fly Complex lies on the eastern side of the belt, the Calaveras Complex forms the center, and the Foothills Terrane is on the western side. Each of these rock units is bounded and separated from the other units by large faults. Some of these faults extend the entire length of the metamorphic belt. The rocks within each unit are also cut by numerous faults. Collectively, these faults are known as the Foothills fault system. The rocks of the Western Metamorphic Belt were deposited during Paleozoic to Jurassic time in a series of subduction zones that existed along what was then the western margin of North America. The subduction activity ended in late Jurassic time when all of the rocks of the metamorphic belt were subjected to a brief but intense period of deformation and metamorphism, referred to as the Nevadan orogeny. -
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 .