A Methodology for Studying Tectonic Subsidence Variations: Insights from the Fernie Formation of West-Central Alberta
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Stratigraphy and Paleontology of Mid-Cretaceous Rocks in Minnesota and Contiguous Areas
Stratigraphy and Paleontology of Mid-Cretaceous Rocks in Minnesota and Contiguous Areas GEOLOGICAL SURVEY PROFESSIONAL PAPER 1253 Stratigraphy and Paleontology of Mid-Cretaceous Rocks in Minnesota and Contiguous Areas By WILLIAM A. COBBAN and E. A. MEREWETHER Molluscan Fossil Record from the Northeastern Part of the Upper Cretaceous Seaway, Western Interior By WILLIAM A. COBBAN Lower Upper Cretaceous Strata in Minnesota and Adjacent Areas-Time-Stratigraphic Correlations. and Structural Attitudes By E. A. M EREWETHER GEOLOGICAL SURVEY PROFESSIONAL PAPER 1 2 53 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1983 UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress Cataloging in Publication Data Cobban, William Aubrey, 1916 Stratigraphy and paleontology of mid-Cretaceous rocks in Minnesota and contiguous areas. (Geological Survey Professional Paper 1253) Bibliography: 52 p. Supt. of Docs. no.: I 19.16 A. Molluscan fossil record from the northeastern part of the Upper Cretaceous seaway, Western Interior by William A. Cobban. B. Lower Upper Cretaceous strata in Minnesota and adjacent areas-time-stratigraphic correlations and structural attitudes by E. A. Merewether. I. Mollusks, Fossil-Middle West. 2. Geology, Stratigraphic-Cretaceous. 3. Geology-Middle West. 4. Paleontology-Cretaceous. 5. Paleontology-Middle West. I. Merewether, E. A. (Edward Allen), 1930. II. Title. III. Series. QE687.C6 551.7'7'09776 81--607803 AACR2 For sale by the Distribution Branch, U.S. -
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 ---------------------------------- -
Polyphase Laramide Tectonism and Sedimentation in the San Juan Basin, New Mexico Steven M
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/54 Polyphase Laramide tectonism and sedimentation in the San Juan Basin, New Mexico Steven M. Cather, 2003, pp. 119-132 in: Geology of the Zuni Plateau, Lucas, Spencer G.; Semken, Steven C.; Berglof, William; Ulmer-Scholle, Dana; [eds.], New Mexico Geological Society 54th Annual Fall Field Conference Guidebook, 425 p. This is one of many related papers that were included in the 2003 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States. -
THE JOURNAL of GEOLOGY March 1990
VOLUME 98 NUMBER 2 THE JOURNAL OF GEOLOGY March 1990 QUANTITATIVE FILLING MODEL FOR CONTINENTAL EXTENSIONAL BASINS WITH APPLICATIONS TO EARLY MESOZOIC RIFTS OF EASTERN NORTH AMERICA' ROY W. SCHLISCHE AND PAUL E. OLSEN Department of Geological Sciences and Lamont-Doherty Geological Observatory of Columbia University, Palisades, New York 10964 ABSTRACT In many half-graben, strata progressively onlap the hanging wall block of the basins, indicating that both the basins and their depositional surface areas were growing in size through time. Based on these con- straints, we have constructed a quantitative model for the stratigraphic evolution of extensional basins with the simplifying assumptions of constant volume input of sediments and water per unit time, as well as a uniform subsidence rate and a fixed outlet level. The model predicts (1) a transition from fluvial to lacustrine deposition, (2) systematically decreasing accumulation rates in lacustrine strata, and (3) a rapid increase in lake depth after the onset of lacustrine deposition, followed by a systematic decrease. When parameterized for the early Mesozoic basins of eastern North America, the model's predictions match trends observed in late Triassic-age rocks. Significant deviations from the model's predictions occur in Early Jurassic-age strata, in which markedly higher accumulation rates and greater lake depths point to an increased extension rate that led to increased asymmetry in these half-graben. The model makes it possible to extract from the sedimentary record those events in the history of an extensional basin that are due solely to the filling of a basin growing in size through time and those that are due to changes in tectonics, climate, or sediment and water budgets. -
Tectonic Setting of the Lower Fernie Formation
Tectonic setting of the lower Fernie Formation: insights from subsidence analysis Tannis McCartney*, Department of Geoscience, University of Calgary, Calgary, Alberta, Canada [email protected] and Andrew Leier, Department of Geoscience, University of Calgary, Calgary, Alberta, Canada Introduction In this study, the Fernie Formation in west-central Alberta is informally divided into upper and lower Fernie. The lower Fernie contains the Nordegg, Gordondale, Red Deer, Poker Chip and Rock Creek Members. These are separated from the Upper Fernie shales by many unconformities, simplified here as a single regional unconformity (Figure 1). Figure 1: Simplified stratigraphic column of the Fernie Formation. In this study, the Fernie Formation is divided into the Upper Fernie (shales) and the lower Fernie (Rock Creek, Poker Chip Shale, and Nordegg). The unconformities separating the Upper Fernie from the lower Fernie are here represented as a single, regional unconformity. The Nordegg and Gordondale Members of the Fernie Formation were deposited during the early stages of tectonic loading in the Cordillera to the west. These members, along with the Poker Chip and Rock Creek Members, were studied to look for evidence of this tectonic activity in the sedimentary record. The results give new insights into current understandings of the lower Fernie Formation. Theory and Method Tectonic subsidence measures the tectonically controlled vertical movement of a basin. Calculating the amount of tectonic subsidence the basin has undergone involves accounting for sediment compaction, paleobathymetry, sea-level changes and post-depositional sediment compaction. GeoConvention 2012: Vision 1 In basin analysis, tectonic subsidence plotted on a depth vs. age chart is used to classify the type of basin the sediments were deposited in. -
Organic Carbon Isotope Chemostratigraphy of Late Jurassic Early Cretaceous Arctic Canada
University of Plymouth PEARL https://pearl.plymouth.ac.uk Faculty of Science and Engineering School of Geography, Earth and Environmental Sciences Finding the VOICE: organic carbon isotope chemostratigraphy of Late Jurassic Early Cretaceous Arctic Canada Galloway, JM http://hdl.handle.net/10026.1/15324 10.1017/s0016756819001316 Geological Magazine Cambridge University Press (CUP) All content in PEARL is protected by copyright law. Author manuscripts are made available in accordance with publisher policies. Please cite only the published version using the details provided on the item record or document. In the absence of an open licence (e.g. Creative Commons), permissions for further reuse of content should be sought from the publisher or author. Proof Delivery Form Geological Magazine Date of delivery: Journal and vol/article ref: geo 1900131 Number of pages (not including this page): 15 This proof is sent to you on behalf of Cambridge University Press. Please check the proofs carefully. Make any corrections necessary on a hardcopy and answer queries on each page of the proofs Please return the marked proof within 2 days of receipt to: [email protected] Authors are strongly advised to read these proofs thoroughly because any errors missed may appear in the final published paper. This will be your ONLY chance to correct your proof. Once published, either online or in print, no further changes can be made. To avoid delay from overseas, please send the proof by airmail or courier. If you have no corrections to make, please email [email protected] to save having to return your paper proof. If corrections are light, you can also send them by email, quoting both page and line number. -
Palaeontological Spitsbergen Studies
POLISH ACADEMY OF SCIENCES INSTITU'TE OF PALEOBIOLOGY PALAEONTOLOGIA POLONICA - NO. 43, 1982 PALAEONTOLOGICAL I SPITSBERGEN STUDIES - Part I (PALEONTOLOGICZNE BL4DANIA SPITSBERGENU - CzeSC I) GERTRUDA BIERNAT- and WANDA SZYMA~~SKA DAWNICTWO NAUKOWE KRZYSZTOF BIRKENMAJER, HALINA PUGACZEWSKA and ANDRZEJ WIERZBOWSKI THE JANUSFJELLET FORMATION (JURASSIC-LOWER CRETACEOUS) AT MYKLEGARDFJELLET, EAST SPITSBERGEN BIRKENMAJER,K; PU~ACZEWSKA,H. and WIERZBOWSKI,A.,: The Janusfjellet Formation (Jurassic-Lower Creiaceous) at Myklegardfjellet, east Spitsbergen. Palaeont. Polonica, 43,107- 140. Fossiliferous marine strata of the Janusfjellet Formation (Jurassic-Lower Cretaceous) are describ- ed from Myklegardfjellet, Agardhbukta area, east Spitsbergen. The invertebrate fauna collected by the first author from these beds in 1977 has been determined by the second author (serpulids, bivalves, belemnites) and by the third author (ammonites). This assemblage allows to distinguish the Upper Callovian, the Kirnrneridgian (Lower and Upper) and the Lower Volgian stages in the lower part of the Janusfjellet Formation (Agardhfjellet Member). The upper part of the Janusfjellet Formation (Rurikfjellet Member) yielded poorly preserved fossils of little stratigraphic value. Key words: Mesozoic, stratigraphy, ammonites, bivalves, belemnites, serpulids, Spitsbergen. K. Birkenmajer, 1nstY~utNauk Geologicznych, Polska Akademia Nauk, 31-002 Krakow, Senacka 3; H. Pugaczewska, Zaklad Paleobiologii, Polska Akadernia Nauk, 02-089 Warszawa,irwirki i Wigury 93; A. Wierzbowski, -
Constraining Basin Parameters Using a Known Subsidence History
geosciences Article Constraining Basin Parameters Using a Known Subsidence History Mohit Tunwal 1,2,* , Kieran F. Mulchrone 2 and Patrick A. Meere 1 1 School of Biological, Earth and Environmental Sciences, University College Cork, Distillery Fields, North Mall, T23 TK30 Cork, Ireland; [email protected] 2 School of Mathematical Sciences, University College Cork, Western Gateway Building, Western Road, T12 XF62 Cork, Ireland; [email protected] * Correspondence: [email protected] or [email protected]; Tel.: +353-21-490-4580 Received: 5 June 2020; Accepted: 6 July 2020; Published: 9 July 2020 Abstract: Temperature history is one of the most important factors driving subsidence and the overall tectono-stratigraphic evolution of a sedimentary basin. The McKenzie model has been widely applied for subsidence modelling and stretching factor estimation for sedimentary basins formed in an extensional tectonic environment. Subsidence modelling requires values of physical parameters (e.g., crustal thickness, lithospheric thickness, stretching factor) that may not always be available. With a given subsidence history of a basin estimated using a stratigraphic backstripping method, these parameters can be estimated by quantitatively comparing the known subsidence curve with modelled subsidence curves. In this contribution, a method to compare known and modelled subsidence curves is presented, aiming to constrain valid combinations of the stretching factor, crustal thickness, and lithospheric thickness of a basin. Furthermore, a numerical model is presented that takes into account the effect of sedimentary cover on thermal history and subsidence modelling of a basin. The parameter fitting method presented here is first applied to synthetically generated subsidence curves. Next, a case study using a known subsidence curve from the Campos Basin, offshore Brazil, is considered. -
Dynamic Subsidence of Eastern Australia During the Cretaceous
Gondwana Research 19 (2011) 372–383 Contents lists available at ScienceDirect Gondwana Research journal homepage: www.elsevier.com/locate/gr Dynamic subsidence of Eastern Australia during the Cretaceous Kara J. Matthews a,⁎, Alina J. Hale a, Michael Gurnis b, R. Dietmar Müller a, Lydia DiCaprio a,c a EarthByte Group, School of Geosciences, The University of Sydney, NSW 2006, Australia b Seismological Laboratory, California Institute of Technology, Pasadena, CA 91125, USA c Now at: ExxonMobil Exploration Company, Houston, TX, USA article info abstract Article history: During the Early Cretaceous Australia's eastward passage over sinking subducted slabs induced widespread Received 16 February 2010 dynamic subsidence and formation of a large epeiric sea in the eastern interior. Despite evidence for Received in revised form 25 June 2010 convergence between Australia and the paleo-Pacific, the subduction zone location has been poorly Accepted 28 June 2010 constrained. Using coupled plate tectonic–mantle convection models, we test two end-member scenarios, Available online 13 July 2010 one with subduction directly east of Australia's reconstructed continental margin, and a second with subduction translated ~1000 km east, implying the existence of a back-arc basin. Our models incorporate a Keywords: Geodynamic modelling rheological model for the mantle and lithosphere, plate motions since 140 Ma and evolving plate boundaries. Subduction While mantle rheology affects the magnitude of surface vertical motions, timing of uplift and subsidence Australia depends on plate boundary geometries and kinematics. Computations with a proximal subduction zone Cretaceous result in accelerated basin subsidence occurring 20 Myr too early compared with tectonic subsidence Tectonic subsidence calculated from well data. -
First Record of Non-Mineralized Cephalopod Jaws and Arm Hooks
Klug et al. Swiss J Palaeontol (2020) 139:9 https://doi.org/10.1186/s13358-020-00210-y Swiss Journal of Palaeontology RESEARCH ARTICLE Open Access First record of non-mineralized cephalopod jaws and arm hooks from the latest Cretaceous of Eurytania, Greece Christian Klug1* , Donald Davesne2,3, Dirk Fuchs4 and Thodoris Argyriou5 Abstract Due to the lower fossilization potential of chitin, non-mineralized cephalopod jaws and arm hooks are much more rarely preserved as fossils than the calcitic lower jaws of ammonites or the calcitized jaw apparatuses of nautilids. Here, we report such non-mineralized fossil jaws and arm hooks from pelagic marly limestones of continental Greece. Two of the specimens lie on the same slab and are assigned to the Ammonitina; they represent upper jaws of the aptychus type, which is corroborated by fnds of aptychi. Additionally, one intermediate type and one anaptychus type are documented here. The morphology of all ammonite jaws suggest a desmoceratoid afnity. The other jaws are identifed as coleoid jaws. They share the overall U-shape and proportions of the outer and inner lamellae with Jurassic lower jaws of Trachyteuthis (Teudopseina). We also document the frst belemnoid arm hooks from the Tethyan Maastrichtian. The fossils described here document the presence of a typical Mesozoic cephalopod assemblage until the end of the Cretaceous in the eastern Tethys. Keywords: Cephalopoda, Ammonoidea, Desmoceratoidea, Coleoidea, Maastrichtian, Taphonomy Introduction as jaws, arm hooks, and radulae are occasionally found Fossil cephalopods are mainly known from preserved (Matern 1931; Mapes 1987; Fuchs 2006a; Landman et al. mineralized parts such as aragonitic phragmocones 2010; Kruta et al. -
Upper Cretaceous Deposits in the Northwest of Saratov Region, Part 2: Problems of Chronostratigraphy and Regional Geological History A
ISSN 0869-5938, Stratigraphy and Geological Correlation, 2008, Vol. 16, No. 3, pp. 267–294. © Pleiades Publishing, Ltd., 2008. Original Russian Text © A.G. Olfer’ev, V.N. Beniamovski, V.S. Vishnevskaya, A.V. Ivanov, L.F. Kopaevich, M.N. Ovechkina, E.M. Pervushov, V.B. Sel’tser, E.M. Tesakova, V.M. Kharitonov, E.A. Shcherbinina, 2008, published in Stratigrafiya. Geologicheskaya Korrelyatsiya, 2008, Vol. 16, No. 3, pp. 47–74. Upper Cretaceous Deposits in the Northwest of Saratov Region, Part 2: Problems of Chronostratigraphy and Regional Geological History A. G. Olfer’eva, V. N. Beniamovskib, V. S. Vishnevskayab, A. V. Ivanovc, L. F. Kopaevichd, M. N. Ovechkinaa, E. M. Pervushovc, V. B. Sel’tserc, E. M. Tesakovad, V. M. Kharitonovc, and E. A. Shcherbininab a Paleontological Institute, Russian Academy of Sciences, Profsoyuznaya ul. 123, Moscow, 117997 Russia b Geological Institute, Russian Academy of Sciences, Pyzhevskii per. 7, Moscow, 119017 Russia c Saratov State University, Astrakhanskaya ul., 83, Saratov, 410012 Russia d Moscow State University, Vorob’evy Gory, Moscow, 119991 Russia Received November 7, 2006; in final form, March 21, 2007 Abstract—Problems of geochronological correlation are considered for the formations established in the study region with due account for data on the Mezino-Lapshinovka, Lokh and Teplovka sections studied earlier on the northwest of the Saratov region. New paleontological data are used to define more precisely stratigraphic ranges of some stratigraphic subdivisions, to consider correlation between standard and local zones established for different groups of fossils, and to suggest how the Upper Cretaceous regional scale of the East European platform can be improved. -
Coupled Onshore Erosion and Offshore Sediment Loading As Causes of Lower Crust Flow on the Margins of South China Sea Peter D
Clift Geosci. Lett. (2015) 2:13 DOI 10.1186/s40562-015-0029-9 REVIEW Open Access Coupled onshore erosion and offshore sediment loading as causes of lower crust flow on the margins of South China Sea Peter D. Clift1,2* Abstract Hot, thick continental crust is susceptible to ductile flow within the middle and lower crust where quartz controls mechanical behavior. Reconstruction of subsidence in several sedimentary basins around the South China Sea, most notably the Baiyun Sag, suggests that accelerated phases of basement subsidence are associated with phases of fast erosion onshore and deposition of thick sediments offshore. Working together these two processes induce pressure gradients that drive flow of the ductile crust from offshore towards the continental interior after the end of active extension, partly reversing the flow that occurs during continental breakup. This has the effect of thinning the continental crust under super-deep basins along these continental margins after active extension has finished. This is a newly recognized form of climate-tectonic coupling, similar to that recognized in orogenic belts, especially the Himalaya. Climatically modulated surface processes, especially involving the monsoon in Southeast Asia, affects the crustal structure offshore passive margins, resulting in these “load-flow basins”. This further suggests that reorganiza- tion of continental drainage systems may also have a role in governing margin structure. If some crustal thinning occurs after the end of active extension this has implications for the thermal history of hydrocarbon-bearing basins throughout the area where application of classical models results in over predictions of heatflow based on observed accommodation space.